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HomeMy WebLinkAboutAPA128 Exh E Chp 2 figures Feb 1983iiiiiiiiii iiiiiiiiii 1> r 1> VI 7'. ~ ~Rl ~.Y~QELECTRIC PROJEC~Cll.ICENSE APPLICATION PROJECT NO.7114-000 As accenhtd bv f:~RC_.llllv ")7 1QA'l .... DATE DUE - -I = - - - - - - - -- - - - - - - - - - - - - - - - - - - - Demeo,Inc_38-293 -- ARLIS Atas\<.a Resources 1.ibraJ'Y &Infcnn~rion SefV 1ces,Ju1('",~8g~,A\fl'X~ AUG 2 3 198J BEFORE THE FEDERAL ENERGY REGULATORY COMMISSION APPLICATION FOR LICENSE FOR MAJOR PROJECT SUSITNA HYDROELECTRIC P,ROJECT VOLUME 5B EXHIBIT E Chapter 2 (Figures) FEBRUARY 1983 360 L-__ALASKA POWER AUTHORITY _ LOWER DRAINAGE BASIN ( '\JEKLUTNA LAKE STREAMFLOW GAGING AND WATEF NOTES: I.CONTINUOUS WATER QUALITY MONITOR INSTALLED. 2.DATA COLLECTION(JUL-SEP 1981 AND JUN-SEP 1982.) 3.THE LETTER BEFORE EACH STATION NAME IN THE TABLE IS USED ON THE MAP TO MARK THE APPROXIMATE LOCATION OF THE STATIONS. (!)w w a::(!)N Z W ::l a:(!) (!)(!)~<l::!: <l:<l:>-:I:...J (!)(!)t:a::u a.. ~w w en ::!E (!)W ...J a..i:i <l:9 i=!(!)<l:::!E en LL <l:::l W I- ::!E en (!)a I-z ~ww~<l:l-LL a::a::::!E gwenLLw w ::!Ea::w i=!t::r ti 0 0 I-a::w w :JSTATIONenuen~~en ID u (A)SUSITNA RIVER NEAR DENALI X X X X X (B)SUSITNA RIVER NEAR CANTWELL X X X X X (VEE CANYON) (C)SUSITNA RIVER NEAR WATANA DAMSITE X X Xl X X (D)SUSITNA RIVER NEAR DEVIL CANYON X X X (E)SUSITNA RIVER AT GOLD CREEK X X X X X (F)SUSITNA RIVER NEAR SUNSHINE X X X X (G)SUSITNA RIVER AT SUSITNA STATION X X X X (H)MACLAREN RIVER NEAR PAXSON X (I)CHULITNA RIVER NEAR TALKEETNA X X X X (J)TALKEETNA RIVER NEAR TALKEETNA X I~X X X (K)SKWENTNA RIVER NEAR SKWENTNA X X X X (L)YENTNA RIVER NEAR SUSITNA STATION X X X -......... ""\ \ I I I II c::? / I I -- <> ---/--/ ./ ./ ",/ MIDDLE \ \ \ \ '7 \ \ \ \ \ \ \ o J .".,..------~./ ./ ,/ / ./ ./ ,// // "-/' ........_--'" O~~~~IOiiiiiiiiiiiiiiiiiiiiiiiiiiii~20 MILESSCALE<=: I~QUALITY MONITORING STATIONS I FIGURE E.2.I SOURCE'R a 11II 1982 RIVER MILE 103.2 SINGLE CHANNEL: -STABLE -NON-ERODIBLE BANKS;CONTROLLED BY VALLEY WALLS,BEDROCK OR ARMOR LAYER CONSISTING OF GRAVEL/COBBLES. -CHANNEL MAY BE EITHER STRAIGHT OR MEANDERING;IN STRAIGHT CHANNELS, THALWEG OFTEN MEANDERS ACROSS CHANNEL. -OCCASIONAL FRAGMENTARY ALLUVIAL DEPOSITS IN FLOODPLAIN. SINGLE-CHANNEL RIVER PATTERN FIGURE E.2.2 SOURCE'RaM 1982 RIVER MI LE 124.4 SPLIT CHANNEL: -MAIN CHANNEL BEHAVES SIMILAR TO SINGLE CHANNEL AT LOW FLOW. -SIDE CHANNELS PROVIDE FLOOD RELIEF AT HIGH FLOWS (GREATER THAN 20,000 CFS). -ISLANDS WELL ESTABLISHED WITH VEGETATION. -GRAVEL/COBBLE BED MATERIAL. -MEAN ANNUAL FLOOD CORRELATES WITH BANKFULL FLOW. -CHANNELS ARE MODERATELY STABLE. SPLIT-CHANNEL RIVER PATTERN FIGURE E.2.3 SOURCE'RaM 1982 CHULITNA RIVER NEAR CONFLUENCE WITH SUSITNA RIVER BRAIDED CHANNEL: -FLOODPLAIN IS VERY WIDE AND SHALLOW EVEN AT FLOOO FLOW. -MULTIPLE AND INTERLACING CHANNELS IN UNVEGETATED GRAVEL FLOODPLAIN -MOVE LARGE QUANTITIES OF BED MATERIAL DURING FLOWS GREATER THAN BANKFULL -RESULTS FROM COMBINATION OF HIGH RATES OF BEDLOAD TRANSPORT,LOW CHANNEL STABILITY,HIGH SEDIMENT SUPPLY,HIGH GRADIENTS AND LOW UPSTREAM FLOW REGULATION. BRAIOEO-eHANNEL RIVER PATTERN FIGURE E.2.4 SOURCE'R 8 M 1982 DELTA ISLANDS MULTI-CHANNEL (DELTA ISLANDS): -VERY BROAD FLOODPLAIN WITH LITTLE LATERAL CONTROL. -MULTIPLE CHANNELS CONSIST OF A MIX OF BRAIDED,S~IT CHANNEL AND SINGtE CHANNELS WITHIN FLOODPLAIN. -RELATIVELY UNSTABLE.SUBJECT TO MAJOR LOCAL CHANGES DURING SINGLE FLOOD EVENTS. -LARGE AMOUNT OF FINE SUSPENDED SEDIMENT HELPS STABILIZE BANKS; DENSE VEGETATION EFFECTIVE IN TRAPPING SEDIMENT. -BED MATERIAL CONSISTS OF GRAVEL/SAND WITH POCKETS OF SILT. MUL TI-CHANNEL RIVER PATTERN FIGURE £.2.!5 · 1400 ~ ~w W LL. ~ z 1350 0 i=~ W ....J ~w 1300 1550 1500 1450 _~WATER SURFACE V FORQ~8,100CI /WATANA""........,,;/ 1250 ~-----+-----,,-+~-,,----'."""""~=-----+-----------+-----+-------+-I ~ 1200 1150 160 162 164 166 168 170 172 SOURCE:R •M 1982 ....J :> 1LIo NOTES: I.WATER SURFACE PROFILES ON PRELIMINARY DATA. 2.URX ~UPPER RIVER CROSS SECTION (ABOVE DEVIL CANYON ). BASED SUSITNA RIVER THALWEG DEADMAN CREE I ~x 102 ~..~~ ~l"'''''~THALWEG PROF I LE E PROFILE :FS AT FIGURE E.2.6 lll: ~ ~a::u z« ~o« l<Jo 186 188184182180178176174 RIVER MILEI i I lAND WATER SURFACE PROFILES tK 10 DEVIL CREEK I I 950 900 850 800 WAl~ 100I-W W lL.. ~ Z 0 750i=<t>W WATER SURFACE PROFI LE FOR ~...J -W PROBABLE MAXIMLIM FLOOD "",r-IY',.,---./ '-"700 ~/V::'.............."~ v~~V //~~LRX 45 ~650 ~V~" //?/- -""~~~....."/7600~,~~L'X 35~--.........."'"~LRX 29 550 136 138126128130132134 Z O:.t:WZ za::NOTES:<t ...JW(!)O «wOW<t--:;.~(!)CI::(!)I-o-J.WATER SURFACE PROFILES BASED CI::u j5 za::WONPRELIMINARYDATA.:I:enen2.LRX =LOWER RIVER CROSS SECTION (BELOW DEVIL CANYON). SUSITNA RIVER THALWE~ DEVIL CA~ SOURCE:RaM 1982 I ! / ..... ,,'", /'~ ~:;;;f,,/ _./~LRX68,.. l,0/,..// ,,/V.,-/'~~TER SU RFACE :~/~2bYR,FLOOD V'".,-"-"LRX 59~/~V,/Y V "./.,- !'--THALWEG~",,'PROFILE '/\ WATER SURFACE PROFILE FOR Q=13,400 CFS AT GOLD CREEK i 140 142 144 146 148 150 152 15 ~RI VER MI LE :II::z W 0W>-0::ZU«u 4 ~AND WATER SURFACE PROFILES ~YON TO RM 126 w (,!)«t-o::o !I.. -l;;: wo FIGURE E.2.7 650 600 550 I-500 LLl LLl ~ zo ~>LLl u1 450 400 350 LRX 3 WATER SURFACE PROFILE FOR PROBABLE MAXIMUM FLOOD 300 98 100 102 104 106 108 110 SOURCE:RaM 198Z ctLLlzuI-z :::::iLLl :::l:::l :I:...Ju~,z «0 ZU !=en :::len NOTES: I.WATER SURFACE PROFILES BASE D ON PRELIMINARY DATA. 2.LRX::LOWER RIVER CROSS SECTION (BELOW DEVI L CANYON l. LLlen ct :I: U SUSITNA RIVER THALWEG RM 126 l ,.~,.,.-_"V WATER SURFACE PROFILE .~..~~".- -~ FOR IQOYR.FLOOD \_~......,~-;;;-__ \._J·_·:::--~/Y iE PROFILE jCFS AT 112 RIVER'MILE 114 116 118 120 >-cr cr ;:) u 122 124 126 lAND WATER SURFACE'PROFILES Iro TALKEETNA f- I I I FIGURE E.2.8 1 ~·······l 1 )------1 1 PARKS HIGHWAY BRIDGE (SUNSHINE) ~ V KASHWITNA CREEK r CONFLUENCE /S\)S SUSITNA -YENTNA RIVER /"CONFLUENCE ------~ ~COOK ----INL: ~-~ 500 400 ~w W l!.. Z o 300 ~>W ...J W 200 100 o o 10 20 30 40 50 60 70 RIVER MILE 80 90 100 110 120 SOURCE'RaM 1982 SUSITNA RIVER THALWEG PROFILE SUNSHINE TO COOK INLET FIGURE E.2.9 1 1 1 1 1 1 1 J 5000400020003000 DISTANCE (FEET) 1000·o l- I- l- I- f- e- l- f- l- f- e- l- I- f- e- e-.~-- -'"-- - --- -~0:52000 -I ·0:34500 - -1J'r,A Q:23400 -1\0:17.000 -Q:13,400-\"- -U '\.Q:9700 c-o:6000Cell- I-- l- I- l- f- l- f- l- I- h II1I1111 I I I I I II II .I I " " I I I I I I I I I I I I I I I II I II I II I I I I I I I I I I I I I I I I 620 590 -1000 630 B 600 I- :Ja.. ~o (,) z 0 ~oct>W ..J W W (,) ~610 a:: :J Cf) a::w ~ ~ I- W W LL. NOTES: Q -=FLOW (CFS) (e)-::ESTIMATED SOURCE'RaM 1962 CROSS -SECTION NUMBER 32 NEAR SHERMAN (RIVER MILE 129.7) FIGURE E.2.10 1 1 1 --1 sus/rNA RIVER SUSITNA RIVER PLAN INDEX MAP J E.2.12 ,. DEVIL CANYON -~-J FIGURE E.2.11 LEGEND: +RIVER MILE ~LRX CROSS SECTION 100 YEAR FLOOD PLAIN BOUNDARY •@9 THERMALLY INDUCED OPEN LEAD DURING WINTER BERM STAFF GAGE SITE SUSITNA RM 152 IVER PLAN o RM 145 FIGURE E.2.12 NOTE FOR LEGEND SEE FIGURE E.2.12 SUSITNA RM 145 • RIVER PLAN TO RM 139 FIGURE E.2.13 NOTE:FOR LEGEND SEE FIGURE E.2.12. SUSITNA RM 138 RIVER PLAN TO RM 132 FIGURE E.2.14 NOTE.FOR LEGEND SEE FIGURE E212. SUSITNA RM 131 RIVER PLAN TO RM 125 FIGURE E.2.15 NOTE;FOR LEGEND SEE FIGURE E.2.12. SUSIT~ RM I~ RIVER PLAN TO RM 118 FIGURE E.2.16 ,... ,... NOTE FOR LEGEND SEE FIGURE E.2.12.SUSITNJ RM Iii ~RIVER PLAN TO RM "I FIGURE E.2.17 NOTE:FOR LEGEND SEE FIGURE E.2.IZ. SUSITN RM III RIVER PLAN TO RM 104 = FIGURE E.2.18 NOTE:FOR LEGEND SEE FIGURE E.2.12. SUSITNJ RM IO~ RIVER PLAN TO RM 101 FIGURE E.2.19 NOTE FOR LEGEND SEE FIGURE E.2.12. SUSITI RMI< A RIVER PLAN o TO RM 97 FIGURE E.2.20 55+00 HEAD OF SLOUGH AT STATION 62 fo 27 NOTE:WATER SURFACE PROFILE IS REPRESENTATIVE OF AUGUST 24,1982 CONDITIONS;MAIN STEM DISCHARGE AT GOLD CREEK 12,500 CFS,SLOUGH DISCHARGE 3 CFS. DISTANCE (FEET) SLOUGH 9 62t27 -----/--c 6 FT IMI GRAOIENT =5. N / o 610 605 ~w 600w lJ.. Z 0 i=ex>595w -lw 590 SLOUGH 9 THALWEG PROFILE SOURCE:TRIHEY 1982 FIGURE E.2.21 605 600 ~595ww lL. Z 0 i= ~ W ...J 590w LEFT '"BANK \kHT BANK ~J,-------,...-- L AUG.I WATER SURFACE ELEVATION (MAINSTEM DISCHARGE 26,400CFS ) NOTES: I.CROSS SECTION #128.853 APPROXIMATELY 2400 FEET UPSTREAM OF SLOUGH MOUTH. 2.CROSS SECTION REPRESENTS VIEW LOOKING DOWNSTREAM. 3.MAINSTREAM DISCHARGE MEASURED AT GOLD CREEK. 585 580 -30 o 30 60 90 DISTANCE (FEET) SLOUGH 9 CROSS SECTION 120 150 180 FIGURE E.2.22 50 40 30 20 (/) l.Lo ooo 6 4 ••••• •••....._- ~.--~•--------r------·WY1969 ---~ 2 1.01 1.25 2 5 10 20 RECURRENCE INTERVAL (YEARS) 50 100 500 1,000 10,000 LOW-FLOW FREQUENCY ANALYSIS OF MEAN ANNUAL FLOW AT GOLD CREEK FIGURE E.2.23 I I I r I r II I ,II I I II I I II I J -LEGEND: ~~......CANTWELL FLOW---WATANA FLOW~ GOLD CREEK FLOW ~ ~~ "l' ~I I r ', I ~I ,,~-I I \, ", I ::.l~ '--I ::\ l·\i ~,~.,..:II '"","t ':I', I ~:~., " ","..' V:: ~:,,'.\;..-I I I -~ · ·- ·: ".. - I I I "-''T'I I 88 80 72 64 56 II) u..u o 48o Q W <9a:« ~40 en o 32 24 16 8 o JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1964 NA CANTWELL,WAt I, E MONTH JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER rURAL FLOWS ANA AND GOLD CREEK FIGURE E.2.24 88 ,.....---r,-"""-'-_'I"""-"T'",-"T",-"T"I-"'T"I-""T"--"ll"""-""T',--"I--",r--I-",-"""'T,-"""'T'_I-'''''''-'''''I .....LEGEND: ..........CANTWELL FLOW 80 I--- ---WATANA FLOW GOLD CREEK FLOW 721------------------------------------ 641------------------------------------- - 561------------------------------------ (i)u..u§48 w ~n:: ~401------------------------------------uen o - JANUARY FEBRUARY MARCH APRIL MAY NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1967 NA CANTW.ELL,WATj I I I I I I I I I I I I I I I I 'I I I I I I , , - - - - I II , I , I \ I I II I I II., I:::~,,: ::: i \Y':./:,::/. .\~;\..\~ .......'.".\ ......'." ..••.'", !••••" - - - - - - .......~.~.~:\.. -.-.....................'- I I I I I I I I I I I I I I I ··~··~~7;;;:··-:-::;l~..·~~,:::::·.;:::.'::;'I-?"'=-="~'r:-:'~:=f'·r--I -I --.- ~JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEr.eER !MONTH I ~TURAL FLOWS i rANA AND GOLD CREEK I AIJASKA:RF~OTW~~T'm1'-A..'R'tl us.DE'''r (',; FIGURE E.2.25 88 J I 'I I I I I I II I I II I I I I I r I-LEGEND:......'".......CANTWELL FLOW----WATANA FLOW 80 ~ GOLD FLOW I- 72 I- 64 ~ 56 ~lo- U) 1L. U 0 48 0 Q-w ~ CJa::«40:r:uen 0 ~ 32 I- 24 I--A I~\J\16 .\ J\V;/\"',Y \..IV '-- 1 \r ~\,):\-"\ :.\I.•..:~\.I'J.,..,J ...........~i'·,:"......:~ 8 :....:...........-J!.....•... l- I I .1 I I I I I0 JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE; TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1970 Nt( CANTWELL,WAT I I I I I I I I I I I I I I I I I I I I I I I I I - - - - - - - :/1 !...:;.\(-'i....'..::vv..,.J ~I ·~:....•.•..•.. \.'.~.'"1}\j:'.\............i ..\IA . ":'.''\v'-"...."".. \'/'.1 A - - - MONTH JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER : ,rURAL FLOWS rANA AND GOLD CREEK FIGURE E.2.26 1 1 1 --1 1 J ~ ./' ./'~~ /.",~./ ~~I~~ ~A./~--~~~......-- ..-~ ~~..-----~~ ~~ .~V l"""" 200 50050100201025 RECURRENCE INTERVAL (YEARS) ANNUAL FLOOD FREQUENCY CURVE SUSITNA RIVER NEAR CANTWELL 1.251.05 LEGEND A OBSERVED DATA o ESTIMATED DATA •95%CONFIDENCE LIMITS 10 1.005 THREE PARAMETER LOG NORMAL DISTRIBUTION WITH 95%CONFIDENCE LIMITS PARAMETERS ESTIMATED BY MAXIMUM LIKELIHOOD 100 90 80 70 60 50 rn l.L 0 40 0 0 0- LLI C)300::« :J: 0rn c 20 SOURCE:R e.M 1981 FIGURE E.2.28 1 1 ...)~-I ..} ../' ./ / /"V //'/ ///~ ~~ ~~....-A.-------.-A --~..~....__-e-............~ 30 40 20 THREE PARAMETER LOG NORMAL DISTRIBUTION WITH 95 %CONFIDENCE LIMITS PARAMETERS ESTIMATED BY MAXIMUM LIKELIHOOD 100 ~8 l8 50 ffu ooo=-10w C,!)9 0::8~7uen6 B 5 4 3 2 LEGEND: •OBSERVED DATA o ESTIMATED DATA •95%CONFIDENCE LIMITS 1.005 1.05 J.25 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 100 200 500 ANNUAL FLOOD FREQUENCY CURVE MACLAREN RIVER NEAR PAXSON SOURCE'RaM 1981 FIGURE E.2.30 1 1 )-j ----1 1 J -'J 1 1 1 ---J --1 1 )-) -- ......!l/' ~V :/V -"/ ~~..,...- ~-'---' ~•~ ~......-----~----_.--4..-- V--~~~,.-----....- .---"~ ~.~~-- •[J" 50020010050201025 RECURRENCE INTERVAL (YEARS) "1.251.05 LEGEND: •OBSERVED DATA o ESTIMATED DATA •95%CONFIDENCE LIMITS 10 1.005 THREE PARAMETER LOG NORMAL DISTRIBUTION WITH 95 %CONFIDENCE LIMITS PARAMETERS ESTIMATED BY MAXIMUM LIKELIHOOD 1000 90g80 700 600 500 400 300 en 200 lL. U 8 0 ~ UJ 100 C) II::90«~8::J:u (f) 0 60 50 40 30 20 ANNUAL FLOOD FREQUENCY CURVE TALKEETNA RIVER NEAR TALKEETNA SOURCE:RaM 1981 FIGURE E.2.32 "j 1 1 J 1 1 J 1 ]1 )]--J J I I I NOTES: //I.THE MEAN ANNUAL INSTANTANEOUS FLOOD PEAK IS DETERMINED BY THE FOLLOWING FORMULA /-- Q:7.06 (D.A.)-46.3 (L)+697.14 (GH·200.15 (MAP)-49.55(MAS)-2594.00 / WHERE:V/Q:MEAN ANNUAL INSTANTANEOUS PEAK FLOW (CFS) ~D.A.=DRAINAGE AREA (SQ.MI.)./L=STREAM LENGTH (MI.)~ G=PERCENT OF DRAINAGE AREA COVERED BY GLACIERS V./MAp:MEAN ANNUAL PRECIPITATION (IN.)/~FLOOD MAS:MEAN ANNUAL SNOWFALL (IN.)/',,/ PEAK ESTIMATE 2.THE FLOOD PEAK FOR A GIVEN RETURN PERIOD IS ///'--DETERMINED BY MULTIPLYING THE MEAN ANNUAL .VPEAKBYTHEDIMENSIONLESSCURVERATIOFOR/'--.--~-........THE RETURN PERIOD OF INTEREST.~...-'\COMPOSITE 95 %.,....,.."CONFIDENCE '>~",...,'"\ INTERVAL "\.,....,......-::~~.......\~....--- ~'....-~', -f--~...........--"..--,..,..."-....--.-.-------,..,...'.,....,.. .,....,../ .,....,.. ..... 7.0 6.0 5.0 4,0 3.0 0 I-2.0<l: 0::: (f) (f) lJ.J ...J Z Q (f) Z lJ.J :::!:1.0 Cl 0.9 0.8 0.7 0.6 0.5 0.4 0.3 1.005 1.05 1.25 2 5 10 20 RECURRENCE INTERVAL (YEARS) 50 100 200 500 10POO SOURCE'RaM 1981 DESIGN DIMENSIONLESS REGIONAL FREQUENCY CURVE ANNUAL INSTANTANEOUS FLOOD PEAKS FIGURE E.2 34 - ......180 165-, 150 f"""135 120 (I)u. 0 105 0 0,....52 90 lIJ (J) c::«75:I: 0 (I) Q 60 45 ~30 15 r- 0 j /v /v 1//IJ ~V "7 )J ANNUAL----<~/ /~v v v /~SUMMER ~ 1.005 2 5 10 20 50 100 1,000 10,000 RECURRENCE INTERVAL (YEARS) WATANA NATURAL FLOOD FREQUENCY CURVE FIGURE E.2.35 - "... ,-180 165 150-135 120-I en LJ..u 105 0 0 Q 90w C) a::: <r 75:I: ~Uen 0 60 45 -30 I 15-0 J / / J /v i/ J / Jv 1/ / 1.005 2 5 10 20 50 100 ~OOO 10,000 - - RECURRENCE INTERVAL (YEARS) DEVIL CANYON NATURAL FLOOD FREQUENCY CURVE FIGURE E.2.36 200 t------+-------+-----t-------/-----___I_----___1 \ \ I \ I \I , /"/, ./".//-,40 t-="---,=;;;;;o--='--+---------::;;;..-"'9------t-------+---------"o,....-:--f------::-;.,;.----=......l-- en ~120 t------+-------+--+----j'--t-~.___\_-_+_----___I_----___1 ooo 160 t------+-------+-------iL-t---\-----_+_----___I_----___1 LJJ (!) 0:::«G 80 ~c -5 PEAK TIME (DAYS) 5 10 15 LEGEND FLOOD VOLUME (FT 3) PEAK DISCHARGE (CFS) 100 YR.122.3 X 10 9 500YR.178.2 X 10 9 ---10,000 YR.269.2 X 109 104,550 131,870 171,200 SUSITNA RIVER AT GOLD CREEK FLOOD HYDROGRAPHS MAY -JULY SOURCE'R 8 M 1981 FIGURE E.2.37 , ,.... I 200t------+------+-----t------+------+--------l r- 160 ,..... (/J u. 0 0120 0 Q ~w (!) a: <l: ~ 0 (/J 0 BO 40 - ----- '\ "\ ""\ " PEAK TIME (DAYS) 5 10 15 LEGEND: FLOOD VOLUME (FT3) 100YR 53.8 X 10 9 500YR 78.8 X 10 9 10,000 YR 119.5 X 109 PEAK DISCHARGE (CFS) 90,140 119,430 163,.960 SU SITNA RIVER AT GOLD CREEK FLOOD HYDROGRAPHS AUG -OCT SOURCE:RaM 198\FIGURE E.2.38 10 5 ~!§~~~~§~~§!§§81= 6J----+--+----+--+----+--+---+--+--+---I 41----+-+---+..,..-+---+-+--+-+--+---1 10 5 8 6 4 2 10 4-8en6lL ~4 LLJ C) 0=: ~2 ...... 0 ........r---en --is 10 3 ......... 8 6 4 ----2 10 2 0 10 203C %OF TIME DISCI 10 5 8 6 4 \.\""-----2 \"'--, 10 4 '----8en6lL ~4 LLJ C) 0=:«2x 0en is 10 3 8 6 4 2 21----+-+---+-+---+-+---+-+--+---1 2 ,____, ..------'\ 10 4 ......-......." 8 ~~E§~-Ei~E 6 I---+-+--+-+--+-+--+-+-~~...---I,' 4 I---+--+--+-+---+-+--+---+--+~' 21---+-+---+-+---+-+----+--1---+---1 10:E~3EI§~I3~E~~E3 41---+-+--+-+--+-+--+-+--+--1 4 I---+--I---+--+---+--+---+-+--"+-"-=-~----":"""---2 1---+-----,--I__-t--+__-F-.......~....-_-+-+--+----1 2 FE BR~A~Y ....-........... 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10:§~~~!~~~~~~~~~~ 61---+--+---+--1---+-+---+-+--+----1 4 ~,~I---+--+---+--+---+-+--+--+---1 ......""...... 21---+-+--+-+--+-+--+-+--+--1 LLJ C) 0=:«xoen is 10:~~~Ei3~~3~E3~~3 61---+-+---+-+---+-+---+-+--+---1 41---+-+---+-+---+-+----+-+--+---1 en lLo- 21----+-+---+--+---+-+---+-+---+--1 21----+-+---+-+--+--+--+-+--+---1 ._-"'-2 J----+--+----+--+----+---l----=""""h...,,--+----+-----I ,2 J~N~A~Y ................~ 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10:~~~~~3~E~3E~~3 61----+-+--+-+---+-+--+--+--+----1 4J----+--+----+--+----+--+----+--+----+-----I 10 5 8 6 \. 4 '\"."',............-...............------~2 '-,--"-----:'\..-10 4 .............--.en 8 lL 6 --~-...... '"LLJ 4 Kw "~«2z 0en is 10 3 8 6 4 en lLo- 2I__--+------j..,..---+--I----+--I__--+--I__-+-----t '"21---+--+__-+--+---+--+---+--+---+----:.tt , 10 2 0'10 20 30 %OF TIME DISCI 10:§!§~~ 6 1----+---+-4-4 4 \, 2',""-~'""".'10:Ei,2:E~ 6 1__--+---lIr,,-+-1 4 1---+---+-\.:>,-+-1, 2 I---I---+-H en lLo LLJ C) 0=: ~2 1__--+---+-+-1 oen is 10 38aH 6 1----+---+-+-1 4 1----+---+-+-1 --- -..-......- "-'-"- ------f--___--__........ ..........-.... .JU1LY 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10:~!~~!~~!~~~~~E~ 41---+--+---+--+---+-+---+-+--+---1 2 10 4-8en lL 6 0--4 LLJ C) 0=: ~2 0en is 10 3 8 6 4 2 JUINE 102 L-.....l...-.J_....J....---l._...L....---l._....L....,.....l._..L..-......o 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10:§!§~f§~~~~~~~§~ 61---+---If------+--f----+--f----+--f-----+---1 41__-t------j---+--I---t--I----+--I---t-----t --10 4 ~aaaaaaaaaen8~~61---I--+----+--+---+--+--+--+---+----1 '\.UJ 4 ......_ ~--.....-----z 2 f------+--=-1 __-+-_-f------+--f-------P........,+--f----l ~---.................., is -..._" 10:~~~~E§~gg~§~~~~ 6 1----+--1-""""'..-J,,;;;-....=--I----+--I----+--I---t--'~. 4 I---+---I--+--f------+-----f=-.....-........~+---+------1-......... 2 N~VE~BfR 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 D~CE~BfR 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 3C %OF TIME DISC lOS lOS 8 8 6 6 4 4 \. "~~.............2 2 ..................~,"- 10 4 10 4 '..."- en 8 -..8 \........"6 m 6 '"IL.IL.'""I"-~0 \"""'"4r\. .....4 r. U.I U.I ........--""(!)"'-(!)....'I'1\a::a::~..c(2 ~c(2 " ::J:1\,---r--::J:1'..'....\0 0 -I"--m -... r-----m ~\,r--r-...2i 10 3 ..-.I"---2i 10 3---..8 ...........8 '""--"6 '\.......6 -.....---.--.......... 4 "4 .......... ..........,~--1"-._-..\-2 2-'-"'........-.""",IMA~CHI·..........AP~IL .""",M~Y 10 2 .....10 2 i30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 ~CHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED I lOS lOS 8 8 6 6 4 4 1\-r----'"r--.2 "..........-.....-2 '-----r-......--"i r-_r-.......1'\"',--r--10 4 .-.10 4 en 8 .......-..8 1""00..-...........I"-m '"r-...IL.6 IL.6,\................'\."--100-. "\~...................,~"""--~"',U.I 4 ............1'....4 -...1"--...........U.I \(!)\(!)..-I"-........"a::--I-.a::"',"'........c(c( ::J:2 ..::J:2 .............., 0 0(/) "I' m 1""'00-..~"\2i 10 3 2i 10 3 -.ro- 8 8 6 6 -...... 4 4 "I i 2 2 ,UG,UST 10 2 SE1PTI ~M~ER 10'2 O\CT4 )8~R o 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED I·NOTES;i LEGEND: \I.FLOW DURATION CURVES BASED ON MEAN GOLD CREEK DAI LY FLOWS.----CANTWELL '\2.PERIODS OF RECORD:DENALI-----\DENALI:MAY 1957-SEPI966,"\.1\\.NOV 1968 -SEP 1981,CANTWELL:MAY 1961-SEP 1972 1\\""-MAY 1980-SEP 1981 GOLD CREEK:AUG 1949-SEP 1981"1','"r--........~"-r-......... "-.....MONTHLY AND ANNUAL I ....FLOW DURATION CURVES!.'"......'"1""...SUSITNA RIVER NEAR DENALII1'0 ..SUSITNA RIVER NEAR CANTWELLI...... !" [~N~UA~'"SUSITNA RIVER AT GOLD CREEK o 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED FIGURE E.2.39 - ~~~ ~ "----I'-- 4 2 lOS en 8 IL 6 0 4 IIJ C) 0:::ct 2:J: 0en 5 10 4 8 6 4 2 10 3 0 10 203( %OF TIME DISC 2 1---+----+----+ 10:~E~~ 6 1---+--+--1 4 1---+--+--+ 2 I---+--__+___+_ 310 0L....-...I.10-2.....0---l.3( %-OF TIME DISC 10 3 0 10 20 3( %OF TIME DISC 10 6 8 6 w (!) It: j!2 1---+----+--+ oen C 10:~~~~ 6 1---+----+--+ 4 1---+----+--+ 10 6 8 6 4 2 10 5 8en6ILe4w C) 0::: ct 2:J: 0en 5 10 4 8 6 4 2 10:E:=E=t==t ~6 1---1-_+_---+ o 4 1---+----+----+ 80 90 100 OR EXCEEDED I'..~...........---- D~CEIMB~R I\.. -,...."""-... F~8R~A~Y , ~r------.....- dUllY 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 10 3 0 10 20 30 40 50 60 70 %OF TIME DISCHARGE EQUALLED 10 6 8 6 4 2 10 5 en 8 IL 6 0 4 IIJ (!) It: ct 2:x 0en C 10 4 8 6 4 2 106 8 6 4 2 lOS 8en6IL ~4I.LI C) It:ct 2~ 0en 0 10 4 8 6 4 2 2 10 5 en 8 IL 60 w 4 C) It: ct 2~ 0en C 104 8 6 4 2 ~ '\. ~-~~~r--.......... ....... *1VE~B~R .........r--~-~ ....... dU1NE I---I-----'- I'--..~ -- d~N~A~Y 10 3 0 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 I.LI ~ ~2 ~o 10 4 8 6 4 2 3 10 0 10 20 30 40 50 60 10 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EOUALLED OR EXCEEDED 10 6 8 6 4 2 10 5 en 8 IL 6~ IIJ 4 C) 0: ct 2% 0 U) 0 10 4 8 6 4 2 __lOS U)8 ~6 4 10 6 8 6 4 2 lOS en 8 IL 60 w 4 C) 0:ct 2% 0en 0 10 4 8 6 4 2 - ~....--"",..... "\ 1'\ '\ MAY I ..... ~ .....~---10-.....--.""1\ II 0ICT?8~R 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 3 o 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 106 8 6 4 2 lOS 8 C/) 6LL U 4au (!)a::«2:I: U C/) i5 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 C/) LL 6 ~ 4au (!)a:: ~2u C/) i5 10 4 8 6 4 2 ""'"- ~-.... AP~IL. ~--i"""ooo... ........... "' SEIPT~M~ER MONTHLY AND ANNUAL FLOW DURATION CU RVES SUSITNA RIVER AT SUSITNA STATION 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 10 5 en 8 LL 6~ au 4 (!)a::«2:I: U C/) i5 10 4 8 6 4 2 10 6 8 6 4 2 lOS en 8 LL 6u 4au (!)a::«2:I: U C/) i5 10 4 8 6 4 2 NOTES: I.FLOW DURATION CURVES BASED ON MEAN DAllY FLOWS. 2.PERIOD OF RECORD:OCTOBER 1974 -SEPTEMBER 1981. o ED 00 ED I I i .......--i i IIMA~CHI )()40 50 60 70 80 90 10 CHARGE EQUALLED OR EXCEED -------'" ,UG1UST ~O 40 50 60 70 80 90 I CHARGE EQUALLED OR EXCEED , """-\.,\ ,~ --...r"ooo.. '" ~N~UA~ !O 40 50 60 70 80 90 100 HARGE EQUALLED OR EXCEEDED FIGURE E.2.40 10 4 10 4 10 4 8 8·8 6 6 6 4 4 4 2 2 2 10 3 10 3 10 3 en 8 .-.8 .-.8 &a.6 (I)6 (I)60&a.&a.-~~ 1&.1 4 4 41&.1 1&.1 (!)(!)(!)a::a::a:: c[2 c[2 ~2~"~ 0 0 0 (I)..........(I)~(t) C 10 2 r---is 10 2 ..........is 10 2 ~~ 8 --8 --8 6 ......6 ....6......"' 4 ...........4 ...........4 2 2 2 10 1 d~N~A~Y 10 1 F~BR~A~Y 10' 0 10 20 30 40 50 60 70 80 90 100 ·0 10 20 30 40 50 60 70 80 90 100 0 10 20 3( %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISC 10 4 10 4 10 4 8 8 8 6 6 ......6.............. 4 .........4 .........4 "--......---......."""'--"~...........---............ ......................2 ............ 2 .........2 10 3 "-10 3 10 3 .-. (I)8 en 8 .-.8 &a.(I) ~6 &a.6 &a.60~4 -41&.1 41&.1 lU (!)(!)(!)a::a::a:: c[2 c[2 c[2~~~ 0 0 ~(t)(I) is 10 2 is 10 2 is 10 2 8 8 8 6 6 6 4 4 4 2 2 2 10 1 dU1NE 10 1 dUllY I 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 10 O·10 20 3C cv.·OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCI 10 4 10 4 10 4 8 8 8 6 6 6 4 4 4 ", 2 2 2 "'\N .-.10 3 10 3 10 3 (I)8 .-.8 en 8 &a.(I) ~6 IL.6 IL.6 0 ~4 -4 4 1&.1 "'-lU 1&.1 (!)...........(!)(!)a::...........-a::~a::c[2 ~2 c[2~-..........."""'--~ 0 .............0 ----0 (I)(I)--(t) C 10 2 ............2i 10 2 -.................C 10 2 8 8 8.....--. 6 6 6....... 4 4 4 2 2 2 10 1 N~VE~BfR I D~CEIMBfR I 0 10 20 30 40 50 60 70 80 90 100 10 0 10 20 30 40 50 60 70 80 90 100 10 0 10 20 3C %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TI ME DISC !\ ""'""""'".............................. ........ "'\ \ \. '\ '\ M~Y ..... "-........-I'--.----"""'--.........~"- " OCT~)BER I I II 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 1 o 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 4 8 6 4 10 4 8 6 4 2 10 3 8en6IL 0 4 1aJ fi~2 ~ C 10 2 8 6 4 2 2 10 3 en 8 IL 6 ~ 1aJ 4 (!)a::: c(2~ 0en C 10 2 8 6 4 2 MONTHLY AND ANNUAL FLOW DURATION CURVES MACLAREN RIVER AT PAXSON ..........i'--..........-"""""'-.......... r--. AP~IL I".. "-~I ~ -...... ........... ~ "\ I I SE1PTI~M~ER NOTES: I.FLOW DURATION CURVES BASED ON MEAN DAILY FLOWS. 2.PERIOD OF RECORD:JUNE 1958 -SEPTEMBER 1981. I 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 4 8 6 r 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 4 2 10 3 en 8 IL 6~ 1aJ 4 (!)a::: c(2~ 0en C 10 2 8 6 4 2 10 4 8 6 4 2 10 3 en 8 IL 6 0 41aJ (!)a::: c(2~ 0en C 10 2 8 6 4 2 o ED 00 ED -...--t'o... IMA~CHI 30 40 50 60 70 eo 90 10 CHARGE EQUALLED OR EXCEED I : r-r-.--.......,,~ \ I I I i i ,u8 1 usT ~O 40 50 60 70 80 90 I CHARGE EQUALLED OR EXCEED r\ I " I "-i \ r \ I , I\. "'-.... !"'-" ~N~UA~ ~o 40 50 60 70 80 90 100 ICHARGE EQUALLED OR EXCEEDED FIGURE E.2.41 I' I\."-\\~~ "., \,, I\."",,- \......1""'---1- " '...._- ....................r--...--. 10 2 0 10 20 30 %OF TI ME DISCI 10 2 0 10 20 30 %OF TIME DISCI 105 8 6 4 10 2 0 ,1020 30 %OF TIME DISC. 105 8 6 4 2 10 4 8U)6&L ~4 kI (!) 0::«2:z:u f/) 0 10 3 8 6 4 2 2 10 4 8en6&Le 4 kI (!) 0::«2:z:u (/) C 10 3 8 6 4 2 105 8 6 4 2 10 4 8 (/)6&L ~4 kI (!) 0:: ~2 (,) f/) C 10 3 8 6 4 2 .........-..........I--...........---......... ---..... ~CE~B~R \. """--"-I--I--r--10-...-, .........".....-........... dUlLY ,---------10---- F~8R~A~Y 2 2 105 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 105 8 6 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 105 8 6 4 2 10 4 (i)8 &L 6u 4kI (!) 0::«2:z:u f/) is 10 3 8 6 4 2 4 2 10 4 f/)8 &L 6(,) 4 kI (!) 0::«2:z:u f/) 0 10 3 8 6 4 2 "'"........!"'o.... 1',...........~~ "-....................--..........-""'---I .... "'" JUINE f""'..,--"""-~........ .........-----""-----.......----1--....... ~VE~I~R "----r--I--r------ "-- I'"'- __I- -....-.. "~N~A~Y 10 2 0 10 20 30 40 SO 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED i0 2 0 10 20 30 40 50 60 7080 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED lOS 8 6 4 10 2 o 10 20 30 40 eo 60 70 80 90 100 '".OF TIME DISCHARGE EQUALLED OR EXCEEDED 105 8 6 4 2 10 4 f/)8 &L 6~ 4kI (!) 0::«2:z: (,) U) 0 10 3 8 6 4 2 2 ~10 4 f/)8 &L 6~ 4 kI (!) 0::«2:z:u U) 0 10 3 8 6 4 2 lOS 8 6 4 2 104 (i)8 &L 6u 4kI (!) Q:«2:z:u f/) 0 103 8 6 4 2 1"-""-~,"'.r--..... .... "......... "..................-,"-...."-'.. "'-"..i"'..... .. M~Y '"--. "-..-... "'----.. I'.....-...............---~.......-.....~........................ro..... °ICT~)B~R 2 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 8en6IL 0 4 ~ (!) 0:~2::I: 0 C/) 0 10 3 8 6 4 2 10 5 8 6 4 2 104 8en IL 6 ~ 4~ (!) 0: ~2::I: 0 C/) 0 10 3 8 6 4 2 ~ \'--.roo----\roo----....---....... 1"'---..1--- APr LL .. ",""roo--,--,-............-............_-....... -'-'"".....""'" '", SEIPTI~M~ER 10 5 8 6 4 2 10 4 en 8 IL 6~ ~4 (!) 0: ~2::I: 0en 0 10 3 8 6 4 2 10 5 8 6 4 2 10 4 en 8 IL 6 0 4~ (!) 0:~2::I: 0en 0 10 3 8 6 4 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED o ED 00 rCHARGE EQUALLED OR EXCEEDED : - -......---..10_ :-... IMA~CHI' 30 40 50 60 70 eo 90 10 ~CHARGE EQUALLED OR EXC EED r---....-~ 1-t\---" ""'"... --"I :\ !\ ,U8IUST 30 40 50 60 70 80 90 I CHULITNA RIVER - ---TALKEETNA RIVER LEGEND: FIGURE E.2.42 MONTHLY AND ANNUAL FLOW DURATION CURVES CHU LITNA RIVER NEAR TALKEETNA TALKEETNA RIVER NEAR TALKEETNA NOTES: I.FLOW DURATION CURVES BASED ON MEAN DAILY FLOWS. 2.PERIODS OF RECORD: CHULITNA RIVER NEAR TALKEETNA: FEBRUARY 1958 -SEPTEMBER 1972 MAY 1980 -SEPTEM BER 1981 TALKEETNA RIVER NEAR TALKEETNA: JUNE 1964 -SEPTEMBER 1981 00 ED - ...... ""I "1\,I .. '"""-.......... .......----'- ~N~UA~ o 40 50 60 70 80 90 I CHARGE EQUALLED OR EXCEED Ul II.. 0 0 0 Q I ~0.9(!)a:0.8~....:J: 0 0.7(/) Q 0.6 .....0.5 0.4- 0.3 ~ - - 4 3 2 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 ..... """ NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES JANUARY FIGURE E.2.43 - 4 -3 / / ~ 2 .- ! (/) LL. 0 I""'"0 1,3,7 AND 15-DAY HIGH FLOW 0 0 I 0.9~ (,!)0.8.-.It: <l: :I:0.7 0 (/) 0 0.6 t- 0.5 0.4 0.3 "'"' 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 .....NOTE;PERIOD OF RECORD WY 1950 -WY 1981. - SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES FEBRUARY FIGURE E.2.44 - 4 ...., 2 1,3,7 AND 15 -DAY HIGH FLOW 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 19BI. - GOLD CREEK CURVES AT FREQUENCY MARCH SUSITNA RIVER HIGH-FLOW - FIGURE E.2.45 - I""" 4 f"""3 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 1981 - CREEK CURVES AT GOLD FREQUENCY APRIL SUSITNA RIVER HIGH-FLOW -FIGURE E.2.46 100 r I 1-DAY -~~ 50 HIGH FLOW......I -~~ 40 3-DAY ~- HIGH FLOW en ~~~ 1L 30u 0 0-0 w ~20a::« ,,-~ uen 15Ci ,- 10 9r- RECURRENCE .INTERVAL (YEARS)- 5 1.05 1.1 2 5 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 1981. - SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES MAY FIGURE E.2.47 100 "... 1-DAY HIGH FLOW .... 50 r-3-DAY If)HIGH FLOWl.L.40u 0 ~0 0-30~ w (!) 0:: <C,-::cu If) 0 20 15 10 1.05 1.1 2 5 RECURRENCE INTERVAL(YEARS) 10 20 50 - - NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES JUNE FIGURE E.2.48 r-.70 60 I-DAY HIGH FLOW r-50 3-DAY 40 HIGH FLOW-)' 30 .,-. 7-DAY 20 HIGH FLOW ......15-DAY HIGH FLOW JULY-en IJ.. () 0 10 0 0- w (!) 0:::«100 J:90() ~ 0 80 70 I-DAY 60 HIGH FLOW 50 F'" 40 30 ,.... I 20-AUGUST 10 1.02 1.05 2 5 20 50 - RECURRENCE INTERVAL (YEARS) NOTE:PERIOD OF RECORD WY 1950 -WY 1981 -SUSITNA RIVER AT GOLD CREEK HIGH-FLON FREQUENCY CURVES JULY AND AUGUST FIGURE E.2.49 50201.25 2 5 RECURRENCE INTERVAL (YEARS) 40 30 SEPTEMBER en 1.J..20u 0 0 Q 1LI (,l) a:::« :I:u 10en [5 9 8 7 6 5 1.02 - 20 ,I""'"OCTOBER"" _... enr-1.J.. I U 0 10 0 952 8 1LI 7(,l)a:::«6:I: r-uen [5 5 r 4 3 r 1.03 1.1 2 5 10 20 50 RECURRENCE INTERVAL (YEARS) NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES SEPTEMBER AND OCTOBER FIGURE E.2.50 7-6 5 4 --3 7-DAY HIGH FLOW 2 (I'J l.L U 0 0 Q w (!)a:I« ::I:0.9u ~O.B0 0.7 0.6r 0.5 r 0.4 0.3,...., 0.2 I.05 I.I 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE~PERIOD OF RECORD WY 1950 -WY 19BI. GOLD CREEK CURVES SUSITNA RIVER AT HIGH -FLOW FREQUENCY NOVEMBER FIGURE E.2.51 -. 5 I -.4, ,....3 2 r-en lL.u 0 0 0 Iw ~0.9 ~0.8u ~07o. 0.6 0.5 0.4 0.3 0.2 ./"011---1,3,7 AND 15-DAY HIGH FLOW 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE: PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK HIGH-FLOW FREQUENCY CURVES DECEMBER FIGURE E.2.52 I~ 4 3 2 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES JANUARY FIGURE E.2.53 r I 4r----.-----,----------,r------,---.---,-----, 3 2 - - (J) IL. U ooo 1 ~09w. fio;8 ~ ~0.7 (J) o 0.6 0.5 0.4 0.3 0.2 1,3,7 AND J4-DAY LOW FLOW 1.05 1.1 - 2 5 RECURRENCE INTERVAL (YEARS) NOTE:PERIOD OF RECORD WY 1950 -WY 1981. 10 20 50 SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES FEBRUARY FIGURE E.2.54 - 4 3 ".,.. 2 ",.. (f) l.L. U I,3,7 AND 14-DAY LOW FLOW-.0 0 2 I 0.9 l.LI (!)0.8a:::« I 0.7u (f) 0 0.6,- 0.5 0.4 0.3 I""'" 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE·PERIOD OF RECORD WY 1950 -WY 1981. -, ..- SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES MARCH FIGURE E.2.55 - F I 4.-------.,.--...----------.-----------,------.---...------, 3 2 f~ (f)u. () 0 ~0 0 I- ~0.9w (!)0.8a:: c:l::r:0.7 --() (f) Cl 0.6 0.5 0.4 0.3- 0.2 L..--.....l..--L...-..J....---I.__.....l..__L...-_.....J 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES APRIL FIGURE E.2.56 20 r-------r--.-------------.---------,---,---.---------, - 10 9 8 en 7 u. u 6 ooQ 5 w (!) a::4« :I:uen C 3 2 3-DAY LOW FLOW 1.05 1.1 7-DAY LOW FLOW 2 5 RECURRENCE INTERVAL .(YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES MAY FIGURE E.2.57 50201025 RECURRENCE INTERVAL (YEARS) 50 40 30 (/lu.u 0 20 0 0 IJJ CDa::<:I: U (/l 0 10 9 8 7 6 5 1.05 1.1 NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES JUNE FIGURE E.2.58 - 40 ~ 30 -- 20 15 50201025 RECURRENCE INTERVAL (YEARS) 10 9 8 7 6 5 ~~1.05 1.I NOTE:PERIOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES JULY AND AUGUST FIGURE E.2.59 502010 SEPTEMBER 2 5 RECURRENCE INTERVAL (YEARS) 1.05 1.1 NOTE:PERIOD OF RECORD WY 1950-WY 1981 2 15 20 10 9 8 7 6 5 ~4(I) LL. U 0 0 0 IJJ (!) a:7<t :I: U 6(I) 0 OCTOBER 5 4 3 SUS ITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES SEPTEMBER AND OCTOBER FIGURE E.2.60 .... .... 4 3 2 .... en LYLOW LL. u,...0 0 FLOWQI 0.9 1LI ~ C!)0.8a:: <t:c 0.7uen c 0.6 ~ 0.5 ....0.4 0.3,.. 0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 r I ..... NOTE:PERfOD OF RECORD WY 1950 -WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES NOVEMBER FIGURE E.2.6 I ..... 4r----.---,r--------r-----....----,.....--....-----, 3 2 (/) LL U o8 1 =.0.9 ~.0.8 a:: ~0.7u (/) Ci 0.6 0.5 0.4 0.3 I,3,7 AND 14-DAY LrNI FLOW .....0.2 1.05 1.1 2 5 RECURRENCE INTERVAL (YEARS) 10 20 50 NOTE:PERIOD OF RECORD WY 1950-WY 1981. SUSITNA RIVER AT GOLD CREEK LOW-FLOW FREQUENCY CURVES DECEMBER FIGURE E.2.62 18.00 17.00 16.00 15.00 14.00 13.00 12.00 I-w W LL 11 ..00 I I-a..w 10.000 0:: W ~9.00~ 8.00 7.00 6.00 5.00 4.00 3.00 • n • .6- D /:).• .6- b..0 •.6- • 0•b..o·I•.6-•0 b..•.6-0 I h .6-•n -••.6-/:)..6- ~0 06.1:::. u .. b..6.•.6-D •.6-0 .6-6.0 •/:). .6- 6..6-•0 •6. •0 .6-0 6. 6.0 .6- .6-.6- 1\ D.--f--- 0 6. /:). .6-- \ 6. 2.00 126 128 130 132 134 136 138 LEGEND: GOLD CREEK FLOW; •23 ,'400 CFS o 17,000 CFS .6-13 ,400 CFS 6.9,700 CFS z« :!: 0:: W Ien NOTE: WATER DEPTHS COMPUTED BY U.S.ARMY CORPS OF ENGINEERS H EC n COMPUTER PROGRAM. MAINSTEM DEVIL CAN 4 •WATER DEPTHS AT RIVE R MILE 150.2: -•24.13 FEET- 0 22.88 FEET 0 •21.95 FEET 0 D..20.68 FEET • • D.. •••~-- 0 •D 0 D ••••--•• 0 0 • II ~0 ~~D.....•D..••0 0 0 •• ....~.L::>.•• •0 0 n •~•~f:!" •0 u £::,L..>. ~•• ~~ , I 38 140 142 144 146 148 150 152 15 zo:::RIVER MILE ::ll::Z<rw w 0->w ,..c_o:::zzo::()« () w (!)...J«:>I- 0:::W 0 Cl a.. WATER DEPTHS NYON TO RM 126 I 1--F_IG_l_JRE E020631 18.00 17.00 16.00 15.00 14.00 13.00 12.00 I- LaJ LaJ LL.11.00 ::I: I- D.. LaJ 0 10.00 a:: LaJ !i 9.00~ 8.00 7.00 6.00 5.00 4.00 3.00 2.00 • ! I •0 0 ... ... L:::.•L:::. • 0 •0...... •0 c..L:::. ...•[] ...• ••L:::. h L:::.-~..... 0 0~......- L:::. L:::. L:::. NOTE: WATER DEPTHS COMPUTED BY U.S.ARMY CORPS OF ENGINEERS H EC -.IT COMPUTER PROGRAM.MA'INSTEM RM 126 1 <x:z I- W W ~ ...J i:! 98 100 LEGEND: GOLD CREEK FLOW: •23,400 CFS o 17,000 CFS ...13 ,400 CFS L:::.9,700 CFS 102 104 106 108 LaJ (f) <x:::I: () 110 • 0 .& ••/::;. 0 0 .& /::;.•J;. • /::;.0-•- J;. ..... 0 0 J;.•••J;./::;.J;.A •r ••/::;./::;...0 0• 0 J;.1:J00J;. 0 •J;. J;.!J. J;. !J.J;. 6.•!J.•A 0 0 J;.....0 J;. /::;./::;. D. 0 112 114 116 118 120 122 124 12 RIVER MILE >- 0:: 0:: ::::::>u II WATER DEPTHS ~TO TALKEETNA 6 FIGURE E .2.64 1 1 ~l 1 --~l "')1 J J WSEL=592.1 SLOUGH FLOW =3 CFS WSEL=592.15 MAINSTEM =22,500 CFS WSEL=59t.25 2.0 *MAINSTEM =18,000 CFS -------~---------------------_../~-".;;.~:~.:" '\...-WSEL=590.85 ..;::.~:~:,;:. \.0 MAINSTEM=16000CFS .:-:.... ,••'0·*: WSEL AUG 241 1982=590.00 .~.>~~./>~o MAINSTEM =12,500 CFS :'.;..~:..~:. SLOUGH =3 CFS .}.:::"Ct f.::,..... .''.:'.;.:~::<:;:~~.,'.-:";~':>"i.:~.;;~':''::.:;,:.:;",?~:...::/':,'.",:'lf~~~~~~'~~~t~~j~hf .".;-',.'.'I..~~~~~G~ WSEL=594.1 1"MAINSTEM =32,500 CFS 4.0 --- ADF8G STAFF GAGE >::'.<>/;~};;~:"/" ...;.:..;,";'PASSAGE I".1 REACH A 594 593 592 ~ ~591u.-z Q 590 ~>~589 UJ 588 587 -5+00 0+00 (MOUTH) 5+00 10+00 NOTES: \.MOUTH OF SLOUGH AT STATION 0+00. 2.SELECT MAINSTEM DISCHARGES MEASURE,D AT GOLD CREEK. DISTANCE (FEET) BACKWATER PROFILES AT THE MOUTH OF SLOUGH 9 SOURCE:TRIHEY 1982 FIGURE E.2.65 401520253035 MAINSTEM DISCHARGE AT GOLD CREEK (1000 CFS) -/ l-V f-/, l-V ) l-I f-V J -/ -V .J f-I ~I I I / 590.0 589.5 10 594.0 I-w W IL. en 593.0 :::r: C,!) ~ 9en u..o :::r:.... ~o ~ w:::r:592.0.... !;i z Q.... ~w ~w w () ~591.0a:: ~en a::w ~~ OBSERVED WATER SURFACE ELEVATIONS AT MOUTH OF SLOUGH 9 FOR ASSOCIATED MAINSTEM DI,SCHARGES AT GOLD CREEK DATA SOURCE:ADF a G 1982 FIGURE E.2.66 1 1 -,1 LEGEND: -..-DAILY AVERAGE AT DENALI ~DAILY AVERAGE AT VEE CANYON A DAILY AVERAGE AT SUSITNA STATION (S.ELECTED DATES) OCT. .. .. SEP. .. .. AUGUST .. JULY .. ,f( \ ~~ I I'\ I M \ I I "~.'~'"f~It 1 I If'~II " ,1 I I I"\'l..I '''','"~,",I r \I"I 1 I l',l,II '-I .,I I r ,,'""-"-'",,,,"~'"-'\jlt.J Ii ,,',I " I 'I +1~" Ii I"\,,,I I \"~·10 \:\'\ ~I ,f \'I " I ,I 11 \ ,I J' I I'll •I f \'1" I j ,I \•I \,. I r 'l...l ~.'I ,;It I I W ~JIIIII~J \ oJ ~ 14 13 12 II 10 -9u 0-8 w ~..f ~0:f I=>7 I I l-I I <{, a::6 I W , a.T4 ~5 ,i, W I l-I 4 •I 3+~IfII "III"II 2+/~J f I I J I 0 MAY JUNE SUSITNA RIVER WATER TEMPERATURES SUMMER 1980 DATA SOURCE:USGS FIGURE E.2.67 'I J LEGEND: --e--DAILY AVERAGE AT DENALI ............DAILY AVERAGE AT WATANA T II ~r ~..fIlt'I ~1\II , I r II,+\'...t I ~ (I : I ~I ~~I ~~!I I~~~ II,1\il Ill..I 'I I ,f ~r~I,',~f ~~I ~1 f I 'NJ~I\lilt I,~M \I I'\""~I I M I ~\I I fU I I 'I \,,,~.;;;\I ¥~,~I I I I I I "\,1 II I I 1 Il'W '.f I~,~I ~!~~'~/~\ ,T f,'l{\I"I"'~/,'11M~II ~I 'tr I ,I \'~¥\I\~I II ~ ,~\;\"~~I ,.~\,~~I I I ...~~\ ,I U \ I ~ \, ~, I \ I ~, \ \..: 14 13 12 II 10 9-u 0 8-LLJ 0::: ::J 7....ex 0:::w 6 a.. ::IEw 5.... 4 3 2 MAY JUNE JULY AUG.SEP. SUSITNA RIVER WATER TEMPERATURES SUMMER 1981 DATA SOURCE:USGS AND R8 M FIGURE E.2.68 J J ~]OJ ~l J 1 121 I I I I I 101 I I I I --4 LEGEND: •WEEKLY AVERAGE TEMPERATURE 81 ~liii~~i~~fiI::l!J ENVELOPE OF WEEKLYo'::::::::::::,::::::::MAXIMA AND MINIMA o I&Ja::~61 l'r---t----+---l--cr I a:: I&J Q. 2 I&J~41 1 I I I U 21 I I I I I 01 I AUG.SEP.JUL.JUN.FEB.JAN.DEC.OCT.NOV. ,,I I ,,,,!,,,,,, o 4 8 12 16 20 24 28 32 36 40 44 48 52 WEEK MAR.APR.MAY MONTH SUSITNA RIVER AT WATANA WEEKLY AVERAGE WATER TEMPERATURE 1981 WATER YEAR FIGURE E.2.6 9 15 15 (.) o =:------------........................... ............... =:------- OL...--==------"""":":!'=----...-o::'-:-:---"":"":!~26 137 224 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE)-6/1/80 o.....-:2:-1:6~-----1:-=3:"i:7:------"":"":!~--~ SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE)-6/IS/80 ---------~~-~,... ',~,..."........ ", "" -------- 0 ............L...l..-....L...~ 26 137 224 291 SUSITNA GOLD CK.VEE CYN.DENALI LOCATION (RIVER MILE)-7/15/80 15 (.) o----------------~------------....,--~ ......................-....; OL...-~-----~.I.......---~~--.......,j~26 137 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE)-7/1/80 15 15 r---,....------or-------~--___,~ISr--~-------r--...........----r----"'I""'I (.) o a.: ~ 1IJ I- ----~---~ ----------~--.....'..................., '...,...., ..... (.) o a.: ::!:w I- OL...-......."'--...r....-__---'~ 26 137 224 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE)-8/1/80 OL...-~-----~----..I----.I-I26137 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE)-8/15/80 15 15 (.) o a.: ~ W I- O __~-----~==----__:~--""""="~26 137 224 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE )-9/1/80 (.) o a.: ::!:w I- O.....~~----~-=----~~--""""="~26 137 SUSITNA GOLD CK.VEE CYN. LOCATION (RIVER MILE )-9/15/80 LEGEND ----MAXIMUM ----MEAN -------MINIMUM NOTES I.)ALL TEMPERATURES WERE RECORDED BY THE USGS WITH SINGLE THERMOGRAPHS AT EACH SITE. 2.)GOLD CREEK'S TEMPERATURES WE RE INFLUENCED BY TRIBUTARY INFLOW AT THE SITE AND THEREFORE WERE NOT INCLUDED. 3.)DAILY MEAN TEMPERATURES COMPUTED AS AVERAGE OF MINIMUM AND MAXIMUM FOR THE DAY. SUSITNA RIVER -WATER TEMPERATURE GRADIENT SOURCE:USGS FIGURE E.2.70 MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION •MAXIMUM I I / I \ I-~••....•.. .. --.. I ...... u ....- 49 49 054 21 65 9 25 3 5 17 5 27 3 22 6 4 10 2 12 I 7 -- D V G C T 8 85 D V G C T 8 88 0 V G C T 8 88 -- I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I u ~ wa::: ::l ~a:::w 'l.5.0 2:w..... 0.0 10.0 I.A.~13.0 I .A.-----'15.0 SUMMER WINTER t3REAKUP 2.MAXIMUM VALUES OF f2°C AT DENALI ON JUNE 4 AND 5 1 1980; 15.0 OC AT GOLD CREEK ON JULY 3 AND 4,1979;AND 16.5 °c AT SUSITNA STATION ON JULY 9,1976 HAVE BEEN RECORDED BY USGS CONTINUOUS RECORDINGEQUIPMENT1 HOWEVER THESE WERE NOT INCLUDED IN THE ABOVE COMPILATION. ONLY DISCRETE OBSERVATIONS WERE UTILIZED SINCE CONTINUOUS RECORDERS ARE NOT PRESENT AT EACH STATION THROUGHOUT THE BASIN. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA 8-SUNSHINE S8-8USITNA STATION NOTES: I.A.CRITERIA:SHALL NOT EXCEED 20°C AT ANY TIME.THE FO'LLOWING MAXIMUM TEMPERATURE SHALL NOT BE EXCEEDED WHERE APPLICABLE:MIGRATION ROUTES AND REARING AREAS--150C,SPAWNING AREAS AND EGG AND FRY INCUBATION--13°C (ADEC,1979). I.B.o ESTABLISHED TO PROTECT SENSITIVE IMPORTANT FISH SPECIESl.JAND FOR THE SUCCESSFUL MIGRATION..l SPAWNING,L EGG-INC BATIONJ.FRY-REARING,.J AND OTHER REI"'ROOUCTIVt. FUNCTIONS OF IMPORTANT SPt.CIES. SOURCE:USGS DATA SUM MARY -TEMPERATURE FIGURE E.2.71 \7.o.o. SLOUGH 21 • • 0o. NOTE:RM =RIVER MILE ---"-----L...L~M..;.;.;.ATCHLINE YSI SURFACE - -\l .YSI INTERGRAVEL -• h,RECT,ONtOFFLOW .4 DEVIL CANYON: /~10 RIVER MILES INSTRUMENT LEGEND: RYAN SURFACE - - -0 RYAN INTERGRAVEL--. DATAPOD SURFACE - -0 DATAPOD INTERGRAVEL-. SLOUGH 8A \7 • •SLOUGH 9 o. '0. SHERMAN CREEK MATCH L1NE-~- FOURTH OF JULY CREEK DIRECTION OF FLOW RM 130 LOCATION MAP FOR 1982 MIDWINTER TEMPERATURE STUDY SITES SOURCE:TRIHEY 1982 FIGURE E.2.72 SLOUGH 21 (RM 142) SUSITNA RIVER AT PORTAGE CREEK (RM 149) 1000 1600 2200 TIME AUG 31-SEP 6 400 I I I I I I I I ~--.......... t-- f-- I I r I I I I4 10 08 ~ 0.: ~w 6 I- 1000 1600 2200 TIME AUG 31-SEP 6 400 o 8 1----+-----+-----+---+__----1 ~ 0.: ~w 6 I-----+----t-----,,...----'-/------'"Iild---t ~ 8 <.>o ~6 ~w ~ 4 I I I I I I I I ,.... /~- _V ""'-....- """- I I I I I I I I 8 <.>o ~6 ~w ~ 4 ,I I I I I I I-r-----.--- .-- I I I I I I I I 400 1000 1600 2200 TIME SEP 7 -13 400 1000 1600 2200 TIME SEP 7-13 8 ~ 0.:6 ~w ~ 4 I I J I I 1 I I """"- / -./,"'-I'--- I I I I I I 1 I 8 ~ ~6 ~w I- 4 I I I I I I I I -- -- I I I I I I I I 400 1000 1600 2200 TIME SEP 14-20 400 1000 1600 2200 TIME SEP 14-20 1000 1600 2200 TIME SEP 21-27 400 I I ,I I 1 I I r-- --_... ....- 1 1 I I I I I I2 <.>6 ~ a.: ~4 I- 8 1000 1600 2200 TIME SEP 21-27 400 <.>6 t----+----'----'-/-----+---+-----I~ cL ~ ~4 r-+-lIIIIiiiii;;;;;;;;;;;;....~-----t-----F=--__1 FIGURE E.2.73 COMPARISON OF WEEKLY DIEL SURFACE WATER TEMPERATURE VARIATIONS IN SLOUGH 21 AND THE MAINSTREAM SUSITNA RIVER AT PORTAGE CREEK 1981 SOURCE:ADAPTED FROM ADF a G 1981 OJ 1 1 SUSITNA RIVER DAILY AVERAGE TEMPERATURE,RM 126.1 (BASED ON PRELIMINARY DATA FROM ADF8G) INDIAN RIVER DAILY AVERAGE TEMPERATURE NEAR MOUTH (BASED ON PRELIMINARY DATA FROM ADF a G) - ---PORTAGE CREEK DAILY AVERAGE TEMPERATURE NEAR MOUTH (BASED ON PRELIMINARY DATA FROM ADF a G ) LEGEND: ,"\ \ )\.v~\ . L j 1\\~ f -V : \/.""-J!I \,.r r................\F\1~.1 """'v ~~.\,./•I \I \ 1,; '"\1 , .I \ ",...,~"I \ .~~V"I \",\\I1/'i'I Y"\\I ,--'/',,\I \oJ 1 \1 ,I J \'\'/'~-'\I 'I 15 14 13 12 II 10 9 ta w Il:: ~7 c:r Il:: W £1.6~wr- 5 4 3 2 301020 SEPTEMBER 311020 AUGUST 31 JULY 10 20301020 JUNE o 'I I ,,I ,I I ,!I ! I SUSITNA RIVER,PORTAGE CREEK AND INDIAN RIVER WATER TEMPERATURES SUMMER 1982 FIGURE E.2.74 15 13 '.\\., \ 1 I SUSITN BELOW (.) ~ L&J 9a::\I!, ::),..-\.«I .,~VI , a::,NOL&J I ('0 I ---a...\:,--~•\I ,----L&J "'--"-..-,'.. V 7 "-...... "-"-...... ...... 5 :3 I 8 16 JUNE 24 2 10 JULY 18 SOURCE:ADF 6G 1982 NOTES: I)TIME SCALE IS IN INCREMENTS OF 8 DAYS. 2)CHULITNA DATA FOR JULY PROVIDED BY USGS FROM -CHULITNA GAGE 18 MILES UPSTREAM OF CONFLUENCE. COMPARISON OF 19E AND SUSITNA RIVE SUSITNA RIVER ABOVE CONFW~NCE --- CHULITNA RI ER ABOVE CONF UENCE DATA 26 3 II 19 AUGUST 27 4 12 SEPTEMBER 20 MONTH 82 TALKEETNA,CHULITNA, ER WATER TEMPERATURES LEGEND: _.-SUSITNA RIVER ABOVE CONFLUECE (RM.103.0) ----SUSITNA RIVER BELOW CONFLUENCE (RM.83.9) -••..!...TALKEETNA RIVER IMMEDIATELY ABOVE CONFLUENCE CHULITNA RIVER IMMEDIATELY ABOVE CONFLUENCE ----NO DATA FIGURE E.2.75 - 20 18 16 i="w W lL.. (!)w 3: ...J«::r:14~ w ~ ([)« z 0 ~>12w ...J W ...J W >W ...J 0::: W ~«103: / ~ I /// / /V /1/v / /, V/ rf / 0 )(4 I 0 0 - 8 6 o 10 20 30 DISCHARGE (1000 CFS) 40 50 LEGEND: X FIELD MEASUREMENT OCT.7,1980 (RaM 1982d>' o FIELD MEASUREMENTS ADF8G 1982. -HEC -2 COMPUTED RATING CURVE. FIELD MEASUREMENT DEC.3,1980 EJ DURING ICE COVER PROGRESSION (R8M (982d). HYPOTHETICAL ICE COVER RATING CURVE - - -WITH FREEZEUPAT DEC.1980 DISCHARGE. NOTE:ICE COVER RATING CURVE IS AN ILLUSTRATtON ONLY AND IS NOT INTENDED TO REFl-ECT ACTUAL CONDITIONS. ICE AND OPEN WATER STAGE- DISCHARGE RELATIONSHIP,LRX-9,RM 103.2 FIGURE E.2.76 J 1 1 FINE GRAVEL MEDIUM GRAVEL VERY FINE COARSE GRAVEL GRAVEL 60 VERY COARSE GRAVEL SMALL COBBLES LARGE COBBLES 0/6 050 084 ~(MM)(MM) 25 54 113 19 43 100 13 31 68 32 59 110 33 64 122 1 I 28 49 84 19 43 100 LRX~29LRX-31 CROSS-SECTION LRX-26 LRX-27 LRX-28 LRX-29 20 I I }/I :I I ILRX-30 LRX-31 LRX-32 50 1 I I }'I I 7 L I /I I I I 40 1 I } I ,L'I7"7 I I I I en LL U § ::.301 w (!) ~1~I~I~ICl I I 10 I QLf I v-'I I I I I I I I 0'I ,!!!, o 20 40 60 80 100 120 140 160 180 MEDIAN DIAMETER OF BED MATERIAL MOVED (MM) SOURCE:RaM 1182 BED MATERIAL MOVEMENT CURVES LRX-28.29.31.35 FIGURE E.2.77 1 1 -1 -, o 6000 , D ~4000 en ~zw 2owen c ~2000z tAl Q.en=>en ...Jg ~ ) , u , 4 .,. t -.-~t "'I n _II..~n It 4t ••~n •••...........0 ~•~~ , 45 46 72 20 54 5 21 2 !5 16 6 24 2 19 8 :3 15 3 12 1 5 1->- D V G C T S S:;D V G C T S SS 0 V G C T S SS r-r- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTE: I.A.CRITERION:NO MEASURABLE I NCREASE ABOVE NATURAL CONDITIONS (ADEC 1979). I.B.ESTABLISHED TO PREVENT DELETERIOUS EFFECTS ON AQUATIC ANI MAL AND PLANT LIFE,THEIR REPRODUCTION AND HABITAT. 2.AT GOLD CREEK,2 WINTER OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 1.0 mg./I. DATA SUMMARY-TOTAL SUSPENDED SEDIMENTS SOURCE:USGS AND RaM FIGURE E.2.78 ~)1 ~.~..J )1 J 50 40 30 20 enLL 10(.) 0 9 0 80-7-w (!)6a:::<r :J:5uen a 4 3 2 .-"V ~ V v ".,.. ~~ ~~~~ ",.-"'~...... ./-V~~...1'.......V ....... l---"",.. SUSITNA RIVER AT ,........,..."""""""~".,..~",..~SUSITNA RIVERGOLDCREEK~.....-",..NEAR DENALIV~",.. .",-.......~~;' ..io"" ~~f'-SUSITNA RIVER V VV V NEAR CANTWELL ",. ,/~(VEE CANYON),/..... V V !"""""~..... V V ~/1-'"...1000"..... .L...~"~.-""""V"......./',,'~- L ....-L'~MACLAREN RIVER~--""NEAR PAXSON,...,.....~V'",.,... ./ V V V /'/""/V ~V V- ~ ~ I IPOO SOURCE.R 8 M 1982 2 3 4 5 6 7 8 9 10,000 2 3 4 5 6 7 8 9 100,000 SUSPENDED SEDIMENT DISCHARGE (TONS /DAY) SUSPENDED SEDIMENT RATING CURVES MIDDLE AND UPPER SUSITNA RIVER BASINS 2 3 4567891 FIGURE E.2.79 )1 -1 -J 1 ,.,I~ V LEGEND: ,~V §-----SUSITNA NEAR DENALI ,,~ ------SUSITNA NEAR CANTWELL ~V ~V SUSITNA AT GOLD CREEK ~.~ ------MACLAREN NEAR PAXSON /,1#V ~!-,~~'lr1 l/V ,ioo"""....oC1 L..,..oo Io~...1-0 ~r;::~... -C...._:. ~to;;....-::..l ~-.. --~ L..c ~~~~.... ~-e:-,..- ~~a..::to"".,----~... E~..._...... 10--- 99.5 99 99.9 99.8 98 95 90w Nu; c 80w 5 70 5 60~ z 50<X J: I-40 a::: ~30 ii: I-20zwua:::w 10a.. 5 2 I 0.5 0.2 0.1 0.001 0.01 0.1 PARTICLE SIZE (MILLIMETERS) 1.0 SUSPENDED SEDIMENT SIZE ANALYSIS SUSITNA RIVER SOURCE:ALASKA DISTRICT CORPS OF ENGINEERS 1975 FIGURE E.2.80 1 -1 1 1 1 ])1 J 1500 S 1000 t-z..... >-I- 0 m D:: ~500 I- o ,~'I ~~b -- 4~ •••.,. •.... ~~t 0 ~O·•- -_1.--_.. 0 18 27 13 15 21 18 0 4 !5 0 0 3 13 0 I 3 0 0 0 5 1--...... D V G C T 5 55 D V G C T S 5S D V G C T S 55 r-r- I I I J I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 55 -SU51TNA STATION NOTES: I.A.CRITERION :SHALL NOT EXCEED 25 NTU ABOVE NATURAL CONDITIONS (ADEC 1979 ).' I.B.ESTABLISHED TO PREVENT THE REDUCTION OF THE COMPENSATION POINT FOR PHOTOSYNTHETIC ACTIVITY, WHICH MAY HAVE ADVERSE EFFECTS ON AQUATIC LIFE. DATA SUMMARY -TURBIDITY SOURCE:USGS AND R8 M FIGURE E.2.81 200~----...,...---.....,.....---r--...,...----,-----,.-......,....-------r---r---.,....----,-...,....-~----t - NOTES: T =0.185 (SC )0.998 r 2 =0.92 T=TURBIDITY SC =SUSPENDED SEDIMENT CONCENTRATION A/ 150 1-------+----+----+--+----+---+-----I------+----+-----I--+-0='".-+~_.-A-7If------4 /~100~-----+----+----+---+---+----+---+--------:;0....--t---H~~--+-~/'---t--t----4 /~80 t------_+_---+--__+_-_+___+-___+-__+_------t---t----+-r-----t--t-----+-----f A/0 60 I------_+_---+----+--+---+-----+---+--------+---h£---+-----tr----t-----+-~ / v 40t------_+_---+--__+_-+---+-----+--+-----=A=-----+-7iC-----+----+---+---+--t-----I/ /~ 30 t------+----+----+-------+-----+-----+----+--~J""_x__+-------l---+--__+__--+--____f_____I/8 -20 I--------+------+----+---+----+-----+---+-+-------+---+---+------Ir----+------I---I~~( ~.~~ ~10 I--------+----t-----+--.;-;IA-"'/L-t-----+---+--------t &/V' 8 t------+-----t-----+-/+--+----+---+---+--------+---I---+-----+--+-----+------I 6 I------+-------+--:.I'/"----------I---+-----+-----+-----+-------+---~-+---__+__f---_+_____I// 41-------+-/-.I'----+----+--+---+----+---+-------+-----+-----Ir-----+--l---+----1 3 / 2 !---7'/t...-----+-----t-----+--+----+---+-__+_LEG END: V &-SUSITNA RIVER NEAR CANTWELL G -SUSITNA·RIVER NEAR CHASE X -SUSITNA RIVER AT GOLD CREEK I ~---L..--..L------L.....----L...--....L----l------l_-L...-I------l.....1------I---1---L-I.....l.....--..----J.I \0 20 30 40 50 60 80 100 200 300 400 500 600 800 SUSPENDED SEDIMENT CONCENTRATION (mg/1) TURBIDITY VS. SUSPENDED SEDIMENT CONCENTRATION SOURCE;PERATROVICH.NOTTINGHAM AND DRAGE 1982 FIGURE E.2.8 2 ') MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION 15.8 .~ )u t -~ •••n .~ .~ I ~-". -.... 4 U I t· I -. 0 7 19 0 29 5 13 0 4 8 0 15 3 14 0 I 3 0 4 0 4 1-1- 0 V G C T 5 55 0 V G C T S 55 0 V-G C T 5 55 1-1- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I 8.0 10.0 12.0 14.0 zw (!) >-xo Clw ~o CJ) CJ) Cl .......... Ct E I.A.-----. SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S -SUNSHINE S5 -SU51TNA STATION NOTES: I.A.CRITERIA:GREATER THAN 7mg./1.,BUT IN NO CASE SHALL DISSOLVED OXYGEN EXCEED 17mg./I.(ADEC 1979). I.B.ESTABLISHED FOR THE PROTECTION OF ANADROMOUS AND RESIDENT FISH. DATA SUMMARY-DISSOLVED OXYGEN SOURC E:USGS AND RaM FIGURE E.2.8 3 1 )1 1 MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION -t H ~ -l- I";.. -I--,U l U I -I-l~ -~ t n • - -~--~- a 7 15 a 8 2 9 a 4 8 a 6 3 7 0 I 3 a I a 2 1-- 0 V G C T 5 55 D V G C T 5 SS 0 V G C T S SS t-t- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I 80 100 120 zw (!) >-xo cw ~o 60enen o zo ~ 0:: ::::> ~en ~o I.A. SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 55 -SUSITNA STATION NOTES: I.A.CRITERION:THE CONCENTRATION OF TOTAL DISSOLVED GAS SHALL NOT EXCEED 110 %SATURATION AT ANY POINT.lADEC,1979). I.B.ESTABLISHED FOR THE PROTECTION OF ANADROMOUS AND RESIDENT FISH. DATA SUMMARY -DISSOLVED OXYGEN %SATURATION SOURCE:USGS AND R Ii M FIGURE E.2.84 -10 CO (\J W •W 0: :::) (!) i:i: r- 0ro- •--w w •(!)(!) 0:a::«0:r:8 «(,) F"'"(J):::c 0 u--(/) in "!0 0 10 +(\J (/)co .0 > 0 •••-II ZIIl'l"""i='«0 (J)~':l!.~a:: ::::>-tien....(/)u 0 0 I-0•o~Z (\Jw W (!)U0:«a:::r: (,)W~a..0 •-en« •(!) •cw •~•0 ~••en ••~(/) •-•0 ••....J •~•• •••0 ••••l-••••••• Q Q (NOlol\f~nol\fS olN3~~3d)SV9 03AlOSSIO 'VolOol 10o 1 j )J J 1 J - ":- 01 E-n:- (J) :Ja::oza.. ~za.. ...J ~ ~ I.A. 1.1 I • U • 4. 4. !..~ .....nu..lr 4'~4 .1-.r 0 ••~I~"U ~ 0 10 23 0 23 6 23 0 4 II 0 17 4 20 0 I 3 0 6 0 7 1-1- 0 V G C T 5 S::i D V G C T S 55 0 V G C T 5 55 1-1- I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I rl~TJ I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP 4.AT SUNSHINE)2 WINTER OBSERVATIONS WERE LESS THAN 0.01 mg./1. 5.AT SUSITNA STATION)2 WINTER OBSERVATIONS WERE LESS THAN O.Olmg./l. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES: I.A.CRITERION:LESS THAN 0.01 mg./1.FOR ELEMENTAL PHOSPHORUS (EPA 1976). LB.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 2.AT VEE CANYON ,4 SUMMER OBSERVATIONS,2 WINTER OBSERVATIONS, AND THE I BREAKUP OBSERVATION WERE LESS THAN 0.05 mg./1. 3.At GOLD CREEK)6 SUMMER OBSERVATIONS,3 WINTER OBSERVATIONS) AND I BREAKUP OBSERVATION WERE LESS THAN 0.05 mg./I. S-SUNSHINE 55 -SUSITNA STATION DATA SUMMARY -TOTAL PHOSPHORUS SOURCE:USGS AND RaM FIGURE E.2.86 J J 1 0.6 .. ........ 0 E-a- (J)0.4 <t LLJ tixa.. (J) 0 ~a- 0 0.2 x I- 0::: 0 0.0 :1 til ~,"'J~••....U "!Ito I ." ~ 0 9 27 0 II 3 I 0 4 8 0 4 I 2 0 I 3 0 0 0 I 1-1- D V G C T S S5 D V G C T 5 SS 0 V G C T S 55 1-1- I I I I I J I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP 3.AT GOLD CREEK,13 SUMMER 'OBSERVATIONS WERE LESS THAN 0.02 mg./1. 2 WINTER OBSERVATLONS AND 2 BREAKUP OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 0.01 mg./I. 4.AT SUSITNA STATION,THE 2 WINTER OBSERVATIONS WERE LESS THAN 0.02 mg./I. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES; I.NO CRITERION ESTABLISHED. 2.AT VEE CANYON,7 SUMMER OBSERVATIONS WERE LESS THAN 0.05 mg./1. 2 WINTER OBSERVATIONS AND THE I BREAKUP OBSERVATION WERE LESS THAN THE DETECTION LIMIT OF 0.01 mg./I. S-SUNSHINE ss -SU51TNA STATION SOURCE:USGS AND R8 M. DATA SUM MARY-ORTHOPHOSPHATE FIGURE E.2.87 1 -)·-~l I J MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION ) ) , II U U •-I-.~.n ..~..~H ..oil-~,Il' I OiJo •<I1i1o •...U •~ '----- II 19 71 6 31 0 I 3 4 30 4 II 0 I I 2 9 0 10 0 0 1-1- 0 V G C T S SS 0 V G C T S SS 0 V G C T S SS 1-1- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I 2.0 3.0 1.0 0.0 z en <C Z IJJ CDoa: ~ z IJJ ~ <Ca: ~ z .......... o E SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 5S -SUSITNA STATION NOTES: loA.CRITERION:LESS THAN 10mg./I.(EPA 1976). LB.ESTABLISHED TO PROTECT WATER SUPPLIES. 2.AT VEE CANYON,5 SUMMER OBSERVATIONS,3 WINTER OBSERVATIONS, AND I BREAKUP OBSERVATION WERE LESS THAN THE DETECTION LIMIT OF 0.10 mg'/I: 3.AT GOLD CREEK,6 SUMMER OBSERVATIONS,2 WINTER OBSERVATIONS AND 2 BREAKUP OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 0.10 mg./1. DATA SUMMARY -NITRATE NITROGEN SOURCE:USGS AND RaM FIGURE E.2.88 1 300 - ~ Ct .§. en 0 200:J 0en 0 UJ>...J 0enen 0 100 ...J ~ 0 ~ o It .... -l-•It -.., ~r-..•,....~ .~".-~... .!n - 0 \0 59''6 39 8 24 0 4 23 0 19 4 20 0 I 8 0 10 0 7 -- 0 V G C T S SS 0 V G C T S S8 0 V G C T S SS -- I I I I I I IJ I I I I I J I I I I I I I I I I I I I I I I I I I I I I J I J I I I I I I I I I J J I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.A.CRITERION:1,500 mg./1.(ADEC 1979). I.B.ESTABLISHED TO PROTECT NATURAL CONDITIONS OF FRESHWATER ECOSYSTEMS (500 mg./1.IS THE CRITERION FOR WATER SUPPLIES). DATA SUMMARY -TOTAL DISSOLVED SOLlDS SOURCE:USGS AND RaM FIGURE E.2.89 1 1 "1 1 » 400 uo 10 C\J ~300 E ~ IIIo.s:::. E :::J->- t:200~ I- U ::::> Clzou 100 467 • •~. 0 ••••.. .~, I.-~ U I.~4 •~..,.,4~.--I-t ..,"•t• .~411- ~•.. • 32 18 29 81 14 73 9 27 3 5 37 5 31 3 22 I 3 9 2 18 0 7 -- D V G C T 5 55 D V G C T 5 55 0 V G C T S 55 -- I I I I I I I J I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.NO CRITERION ESTABLISHED. DATA SUMMARY -CONDUCTIVITY SOURCE:USGS AND R6 M FIGURE E.2.90 )J )1 1 60 40.. ........ 0 E- I.LJ I- ft ~20:::>en o ., n ~~ •I •-..."'"o!~......-n It .~ I-••U •0 ,.,.... ••••,, ~ II 19 78 6 62 9 25 3 4 33 4 29 4 21 I 2 9 0 16 0 7 f-r- 0 V G C T 5 5S 0 V G C T S SS 0 V G C T 5 S5 f-r- I J I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.A.CRITERION:SHALL NOT EXCEED 200mg./1.(ADEC 1979). \.B.ESTABLISHED TO PROTECT WATER SUPPLIES. 2.AT GOLD CREEK,I SUMMER OBSERVATION AND I BREAKUP OBSERVATION WERE LESS THAN 5.0 mg./I. 3.AT TALKEETNA)I SUMMER OBSERVATION WAS LESS THAN 1.0 mg./1. DATA SUMMARY-SULFATE SOURCE:USGS AND R6 M FIGURE E.2.91 30 20 ....... C. E-10LLJ 0 a::: 0 ..J :::I: U 0 I._-\ -ll". l·~ •l'l r-.~I-I-I ... I·,.l'j'4'1"1"'".j l 4t ..~ I ~,I olio I1·,- -III19746629243433429421 I 2 9 0 16 0 7 r-r- 0 V G C T S S5 0 V G C T S SS 0 V G C T S S5 r-r- I I I I I I I I I II I I I I I I I I ~iLJ I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.A.CRITERION-.LESS THAN 200 mg /I (ADEC 1979). I.B_ESTABLISHED TO PROTECT WATER SUPPLIES. 2.AT VEE CANYON,3 SUMMER OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 1.0 mg/I 3.AT GOLD CREEK,2 SUMMER OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 1.0 mg II, DATA SUMMARY-CHLORIDE SOURCE:USGS AND R8 M FIGURE E.2.92 60 - '"400. E-Q LiJ>..J 0 f/) ~20Q.-"0-2 => 0..Jex 00 • t •U l I-~ n It t .~-It•.~ t -••1-"".~..n I l•....-~••It ~~n l U ..••... U n l n ~ II I~74 6 61 9 25 3 4 33 4 32 4 21 I 2 9 0 16 0 7 1-- 0 V G C T S Sti D V G C T S SS D V G C T S SS -- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.NO CRITERION ESTABLISHED. 2.(d)=DISSOLVED DATA SUMMARY -CALCIUM (d) SOURCE:USGS AND RaM FIGURE E.2.93 MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION ) .~ 4 •t •••I·~ l •, •..".~•4 .~4~•••••••..l 4 4 •U 4r ••• I •, .. II 19 74 6 61 9 25 1 3 4 33 4 32 4 21 I 2 9 0 16 0 1 1-1- D V G C T S SS,D V G C T S SS D V G C T S SS 1-1- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I 5.0 0.0 -= 15.0 a ~10.0 ...Jo C/) C/) a ........ 0. E at 2:-2 => Cii L&I Z (!) ~ ~ SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE SS -SUSITNA STATION NOTES: I.NO'CRITERION ESTABLISHED. 2.(d)-DISSOLVED. DATA SUMMARY-MAGNESIUM (d) SOURCE:USGS AND R8 M FIGURE E.2.94 30 - ~20aae-c lLl ~ 0 rJ) rJ) ~10a ~ ~ :2c 0 rJ) 0 !-l- ~.. -I- .1'- •.. -......io ••.,..,...~~~n ••U r'~H •I .r,,~,•- I I '--- II 19 ·64 6 61 9 25 3 4 27 4 29 4 21 I 2 7 0 16'0 7 1-- D V G C T 5 55 D V G C T 5 5S·e V G C T 5 55 f--- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I J I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA 5-5UNSHINE S5-SU5ITNA STATION NOTES: I.NO CRITERION ESTABLISHED. 2.(d)-DISSOLVED DATA SUMMARY-SODIUM (d) SOURCE:USGS AND R 8 M FIGURE E.2.95 MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION •MAXIMUM I I 4 ~.. I . ".., .~"","n u n n •'"'~.~•.~., "II I II 19 64 6 61 9 25 3 4 26 4 29 4 21 I 2 7 0 16 0 7 1-1- D V G C T S SS D V G C T S 55 D V G C T 5 55 f--f-- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I J I I I I I I I I I I I I I I I I I I I 0.0 2: :::> enen <I ba. 15.0 cw ~oenen C 'Q'5.0 ........oE 10.0 SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE SS -SUSITNA STATION NOTES: I.NO CRITERIoN ESTABLISHED. 2.AT VEE CANYON I I SUMMER OBSERVATION AND I WINTER OBSERVATION WERE LESS THAN THE DETECTION L1MrT OF 1.0 mg./I. 3.(d)=DISSOLVED DATA SUMMARY-POTASSIUM (d) SOURCE:USGS AND Ril M FIGURE E.2.96 170 ........o E- 'pi)120ou "u U) <I U) U) UJ Z o 70a: <I:x: 20 • ..~ .~•I •• n 4 4 4-.-It .~••U •4 ,.~-4'4'.~•.~,. 4 ":II ••• 4 4 -'--.. 19 9 73 6 62 9 25 4 0 33 4 29 4 21 2 I 9 0 16 0 7 1-1- D V G C T 5 5~D V G C T 5 55 0 V G C T 5 55 I-~ I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 5S -SUSITNA STATION NOTES: I.NO CRITERION ESTABLISHED. 2.SOME METALS HAVE VARIABLE SYNERGISTIC EFFECTS WITH HARDNESS,DEPENDENT ON THE PREVAILING HARDNESS IN THE WATER.THE CRITERIA FOR CADIUM J FOR EXAMPLE,ARE 0.0012 mg./1.IN HARD WATER AND 0.0004 mg./1.IN SOFT WATER. DATA SUMMARY -HARDNESS SOURCE:USGS AND RaM FI GURE E.2.97 9.0 8.0-Ien ~ ~IA. ::t:a.- :I:I 1.0a. 6.0 \ , . . II 19 74 6 65 7 2~3 4 34 4 29 3 20 I 2 9 0 16 0 1 -- D V G C T 5 55 0 V G C T 5 55 D V G C T 5 55 -- I I I I I I I I I II I II I I I I I I I I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE SS -SUSITNA STATION NOTES: r.A.CRITERIA:NOT LESS THAN 6.5 OR GREATER THAN 9.0 pH UN ITS.SHALL NOT VARY MORE THAN 0.5 pH UNITS FROM NATURAL CONDITION (ADEC 1979). I.B.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. DATA SUMMARY-pH SOURCE:USGS AND RaM FIGURE E.2.98 175 ...: ........ o 125E JOou ~ en« ~75 z :J« :lil:: ...J c( 25 1.A;-----"20 a , .n •• -"".. I-~• •n ~ •-u a n•0 .. I •• ......c- II 16 67 6 60 6 21 3 3 33 4 29 2 19 I I 7 0 14 0 6 1-1- D V G C T S SS 0 V G C T S SS 0 V G C T S SS 1-1- I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER t3REAKUP D-DENALI V-VEE CANYON G-GOLO CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.A.CRITERION:20 mg./1.OR MORE EXCEPT WHERE NATURAL CONDITIONS ARE LESS (EPA 1976). I.B.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. DATA SUMMARY -ALKALINITY SOURCE:USGS AND RaM FIGURE E.2.99 -"-1 30 ~ ........20 Cl E LaJ CI X 0 £5 z 0 10m 0:::<t (.) LaJ LaJ 0::: l.L. 0 • .~ .~...•,....U ...•It U ... -l-·10 •, 4 II •••~ It .-.. II 16 62 6 55 3 15 ·3 3 29 4 24 0 15 I I 6 0 14 0 5 1-...... D V G C T 5 Sti -0 V G C T 5 55 0 V G C T 8 88 I-f- I I I I I I I I I I I I II I-I I I I I I I I I I I I I I I I I I I I I I I I I I I III I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER ~REAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTE: I.NO CRITERION ESTABLISHED. DATA SUMMARY -FREE CARBON DIOXIDE SOURCE:USGS AND Ra M FIGURE E.2.100 "-a. E zom It:ct U (.) Z ct C) It:o -I ct b2... 30 20 10 • ••.~ u ..--I...U I ..io. ~...1-4~..•., 0 .~:..41·a 0 0 10 0 3 2 7 0 I 4 0 2 2 9 0 0 2 0 I 0 4 1-1- D V G C T 5 S~D V G C T 5 55 D V G C T S 58 1-1- I I I I I I I I I IIIII III I I I I I 1 1 •••••1 I I I II I I I I I I I I I 1 I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA 5-SUNSHINE 58 -SU8ITNA STATION NOTES: I.NO CRITERION ESTABLISHED. 2.WATERS CONTAI NI NG LESS THAN 3.0 mgJI.HAVE BEEN OBSERVED TO BE RELATIVELY CLEAN (McNEELY ,t 01.1979). DATA SUMMARY-TOTAL ORGANIC CARBON SOURCE:USGS AND RaM FIGURE E.2.101 60 ~ Cl .§.40 0z« ~ IJ.J 0 Z IJ.J (,!)>-x 200 ....J« ~ ~ IJ.J :I: U 0 • , ~, .~ 0 8 16 0 0 0 0 0 4 5 0 0 0 0 0 I 2 0 0 0 0 -- D V G C T S S~D V G C T S SS D V G C T S SS -- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP SOURCE:RaM D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.NO CRITERION ESTABLISHED. 2.AT GOLD CREEK t 2 SUMMER OBSERVATIONS WERE LESS THAN 1.0 mg./I. DATA SUMMARY-CHEMICAL OXYGEN DEMAND FIGURE E.2.102 150 MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION ~ I ., -to-,--~fo ~ ....-- 14 17 62 6 30 3 4 3 4 25 4 13 I 4 I 2 8 0 8 0 0 -- D V G C T S SS D V G C T 5 SS 0 V G C T 5 5S f--f--- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I o 100 a:: 9o (.) w ::>a:: I- -en t:z ::> ~ C( CDo (.) :E ::>z i=~I.A~50- SUMMER WINTER t3REAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA 5-5UN5HINE SS-5USITNA STATION NOTES: I.A.CRITERION:SHALL NOT EXCEED 50 UNITS (ADEC 1979). LB.ESTABLISHED TO PREVENT THE REDUCTION OF PHOTOSYNTHETIC ACTIVITY WHICH MAY HAVE DELETERIOUS EFFECTS ON AQUATIC LIFE. 2.AT DENALI t I SUMMER OBSERVATION WAS LESS THAN 5 UNITS.ONE SUMMER OBSERVATION WAS GREATER THAN 5 UN ITS. 3.ATSUSITNA STATION 12 SUMMER OBSERVATIONS AND 2 WINTER OBSERVATIONS WERE LESS THAN 5 UNITS. 4.AT TALKEETNA 1 I W1NTER OBSERVATION WAS LESS THAN 5 UNITS. SOURCE:USGS AND RaM DATA SUMMARY-TRUE COLOR FIGURE E.2.103 2.A 3.0 -"':-\ C' E 2.0 Clw ~ 0 (/) (/) £5 I~ ~ «1.0- ~ ~z ~=>..J <l t I...,.,~, 0.0 0 10 '6 0 0 0 0 0 3 3 0 0 0 0 0 I 2 0 0 0 0 I--f- 0 V G C T 5 55 0 V G C T 5 55 0 V G C T 5 55 1-1- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES; I.NO CRITERION ESTABLISHED.4. 2.A.A LIMIT OF 0.073 mg./I.HAS BEEN SUGGESTED BY EPA (SITTIG 1981). 2.8.THIS SUGGESTED LIMIT IS BASED ON THE EFFECTS OF ALUMINUM ON HUMAN HEALTH.5. 3.AT VEE CANYON,7 SUMMER OBSERVATIONS WERE LESS THAN 0.10 mg./I. TWO WINTER OBSERVATIONS AND THE ONE SUMMER OBSERVATION WERE LESS THAN THE DETECTION LIMIT OF 005 mg./I. S-SUNSHINE 55 -SUSITNA STATION AT GOLD CREEK,4 SUMMER OBSERVATIONS,2 WINTER OBSERVATIONS AND THE 2 BREAKUP OBSERVATIONS WERE LESS THAN THE DETECTION LIMIT OF 0.05 mg./I. (d)=DISSOLVED. SOURCE~R8 M DATA SUMMARY-ALUMINUM (d)FIGURE E.2.104 30 ......... dl E-UJ ...J II)«ffi 20 >oo UJ 0:: ...J ~ 12 ~10 2: ::::>z i :3<t 2A..,0 .. t - 0 0 "3 0 I 3 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 -- D V G C T S S~D V G C T S SS D V G C T S SS -- I I I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.NO CRITERION ESTABLlSHED. 2.A.A LIMIT OF 0.073 mg./1.HAS BEEN SUGGESTED BY EPA (SITTIG 1981). 2.B.THIS SUGGESTED LIMIT IS BASED ON THE EFFECTS OF ALUMINUM ON HUMAN HEALTH. 3.(t)=TOTAL RECOVERABLE. DATA SUMMARY -ALUMINUM (t) SOURCE:USGS FIGURE E.2.105 0.30 2.A·~0 ...,; "- Cl E o UJ :ioeneno m ::I: l-=> ~en m 0.20 0.10 . 0 10 7 0 0 0 0 0 3 3 0 0 0 0 0 I 2 0 0 0 0 .....- 0 V G C T 5 55 0 V G C T 5 55 0 V G C T 5 55 .....- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I II I I I I I •MAXIMUM -MEAN •MtNIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP 4.AT GOLD CREEK,6 SUMMER OBSERVATIONS,2 WINTER OBSERVATIONS, AND THE 2 BREAKUP OBSERVATIONS WERE LESS THAN 0.05 mg./I. 5.(d)=DISSOLVED. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES: I.NO CRITERION ESTABLISHED. 2A.EPA HAS SUGGESTED AN AMBIENT LIMIT OF 0.0035 mg'/I.{SITTIG 1981). 2.B.THIS SUGGESTED LIMIT FOR BISMUTH IS BASED ON HUMAN HEALTH EFFECTS. 3.AT VEE CANYON,9 SUMMER OBSERVATIONS,THE 3 WINTER OBSERVATIONS, AND THE I BREAKUP OBSERVATION WERE LESS THAN 0.05 mg./I. S-SUNSHINE SS -SUSITNA STATION SOURCE:R 8 M DATA SUMMARY-BISMUTH (d)FIGURE E.2.106 0.003 -"-~0.002 E ~ 0w ~ 0 (J) (J)o I.~ -:c 0.001 2 ~ ::::>-~1.---....0 <t u 2.--'" 0.000 0 ::>~ 0 ::>~ -_.- 0 0 3 0 4 3 13 0 0 I 0 5 I 9 0 0 0 0 2 0 6 1-;- D V G C T S SS D V G C T S SS D V G C T S SS r-r- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER .WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS -SUSITNA STATION NOTES: I.CRITERIA:0.0012 mg./1.IN HAR D WATER AND 0.0004 SOFT WATER (EPA 1976). 2.CRITERION:LESS THAN 0.0002 rng./1.(McNEELY et 01.1979). 3.THE ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT GOLD CREEK,I SUMMER OBSERVATION WAS LESS THAN 0.001 mg./I. THE I WINTER OBSERVATION WAS LESS THAN 0.003 mg./I. 5.AT TALKEETNA,2 SUMMER OBSERVATIONS AND 2 WINTER OBSERVATIONS WERE LESS THAN 0.001 mg.fL 6.AT SUNSHINE,2 SUMMER OBSERVATIONS AND THE I WINTER OBSERVATION WERE LESS THAN 0.001 mg./I. 7.AT SUSITNA STATION,12 SUMMER OBSERVATIONS WERE LESS THAN 0.002 mg.lJ.THE 9 WINTER OBSERVATIONS AND THE 6 BREAKUP OBSERVATIONS WERE LESS THAN 0.003 mg./I. 8.(d):DISSOLVED SOURCE:USGS DATA SUMMARY-CADMIUM(d)FIGURE E.2.107 -~-,1 MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION 0.0100.005._---.--"- ,0030 .0020 , :>.0010 ----JII" ,0000 ~~.. 0 0 6 0 10 6 13 0 0 I 0 5 I 9 0 0 0 0 3 0 6 f-I- 0 V G C T 5 55 0 V G C T 5 55 0 V G C T 5 SS ,...1- I I I I I I I I I I I I II I I I I I J I I I I I I I I I I I I I I I I I 1 I I I I I I I I I I I III I I I I I' o ...... 0- S ~0 CD<ta:::w>ou UJa::: ...J I. j:! ~ '0 ~ :E I. ~ :IE 2o <J 0 SUMMER WINTER BREAKUP D-DENALI V-VEE OANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES I.CRITERIA:0.0012 IN HARD WATER AND 0.0004 mg / I IN SOFT WATER (EPA 1976). 2.CRITERION:LESS THAN 0.0002 mg./1.(McNEELY et 01.1979). 3~ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT GOLD CREEK,3 SUMMER OBSERVATIONS WERE LESS THAN O.OIOmg/1.THE I WINTER OBSERVATION WAS LESS THAN 0.001 mg./I. 5.AT TALKEETNA,5 SUMMER OBSERVATIONS,I WINTER OBSERVATION AND 2 BREAKUP OBSERVATIONS WERE LESS THAN 0.010 mg./!. 6.AT SUNSHINE,4 SUMMER OBSERVATIONS WERE LESS THAN 0.010 mg./1. 7.AT SUSITNA STATION,7 SUMMER OBSERVATIONS,7 WINTER OBSERVATIONS AND 5 BREAK UP OBSERVATIONS WERE LESS THAN 0.020 mg./I. 8.(t)=TOTAL RECOVERABLE. DATA SUMMARY -CADMIUM (t) SOURCE:USGS FIGURE E.2.1 08 ~2.a.a.ou £:) UJ ~ ~~ ~0 '--j o ~ .......... ~O. :J U O. 030 020 .010 ~ 000 . ~ -- 0 0 '3 0 3 3 13 0 0 I 0 5 I 9 0 0 0 0 2 0 6 ......1- D V G C T S SS D V G C T S SS D V G C T S SS r-r- I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION i SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 5S -SUSITNA STATION NOTES: I.CRITERiON:0.01 OF THE 96-HOUR LC50 DETERMINED THROUGH BIOASSAY (EPA 1976). 2.CRITERION:0.005 mg/I (McNEELYet 01.1979 L 3.THE ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT TALKEETNA.THE 3 SUMMER OBSERVATIONS WERE LESS THAN 0.010 mg/1. 5.AT SUSITNA STATION,6 SUMMER OBSERVATIONS.2 WINTER OBSERVATIONS AND 2 BREAKUP OBSERVATIONS WERE LESS THAN 0.002 mg /1. 6.(d)=DISSOLVED. SOURCE:USGS DATA SUMMARY COPPER (d) FIGURE E.2.109 - ': Cl E-W -Jm« 0:::w>0 (.) W 0::: -J ~ 0 1---='(.) 0::: Wa..a.. 0 (.)2 0 0 !. D -. ... U -'"n 0 ~. - -'---'--~ 0 0 6 0 IL 6 13 0 0 I 0 5 I 9 0 0 0 0 :3 0 6 -- D V G C T 5 55 0 V G C T 5 55 0 V G C T 5 SS -"""" I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I J I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER 8REAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-5UN5HINE SS-5U5ITNA STATION NOTES: I.CRITERION:0.01 OF THE 96 -HOUR LCSO DETERMINED THROUGH BIOASSAY (EPA 1976). 2.CRITERION:0.005 mg./!.(McNEELY et 01.1979). 3.THE ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT GOLD CREEK 1 I SUMMER OBSERVATION WAS LESS THAN 0.010 mg./1. 5.AT SUSITNA STATION,I SUMMER OBSERVATION AND 2 WINTER OBSERVATIONS WERE LESS THAN 0.020 mg./I. 6.AT TALKEETNA,I BREAKUP OBSERVATION WAS LESS THAN 0.020 mQ./I. 7.(t)=TOTAL RECOVERABLE. SOURCE:USGS DATA SUMMARY-COPPER (t)FIGURE E.2.1I0 60 zo ~I.A·-'O -j ......... Cl E l.IJ ...Jm« D: W ~ (.) W D: ...J ~o..... -lU lL. 40 20 ~-~-1 ~ . •.I IJ~..._. .J.~ 0 0 6 0 13 6 13 0 0 I 0 5 I 10 0 0 0 0 4 0 6 '--r- D V G C T 5 5S D V G C T 5 55 D V G C T S 5S f--f-- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS -SUSITNA STATION NOTES: I.A.CRITERION:LESS THAN 1.0mg./1.(EPA 1976;SITTIG 1981). LB.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 2.(t)=TOTAL RECOVERABLE. DATA SUMMARY -IRON (t) SOURCE:USGS FIGURE E.2.III MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION •MAXIMUM \ I I ..", 0 .~ .~ .....~ 4 0 •I....."'.i~ ~ L.~.~-_. 0 0 6 0 10 6 13 0 0 I 0 5 I 9 0 0 0 0 2 0 6 f-r- 0 V G C T S SS 0 V G C T S SS 0 V G C T S SS f-r- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I 0.1 0.20 0.30 til E I.LJ ...Jm«a: I.LJ>o (,) I.LJa:: ...J ~o ~ :g 0.. -1.---'o« I.LJ 0.0...J " SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 5S -SUSITNA STATION NOTES: I.CRITERION:LESS THAN 0.03 mg./I.(McNEELY et 01.1979). 2.CRITERION:0.01 OF THE 96-HOUR LC50 DETERMINED BY BIOASSAY (EPA 1976). 3.ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT GOLD CREEK,3 SUMMER OBSERVATIONS WERE LESS THAN 0.100 mg./I. 5.AT TALKEETNA,6 SUMMER OBSERVATIONS AND I WINTER OBSERVATION WERE LESS THAN 0.100 mg./I. 6.AT SUNSHINE,2 SUMMER OBSERVATIONS WERE LESS THAN 0.100 mg./I. 7.~SUSITNA STATION r 5 SUMMER OBSERVATIONS,3 WINTER OBSERVATIONS, AND 2 BREAKUP OBSERVATIONS WERE LESS THAN 0.200mg./I. 8.(0 =TOTAL RECOVERABLE. SOURCE:USGS DATA SUMMARY-LEAD (t)FIGURE E.2.112 -. .........c;. E c lIJ ~eneno E: 2 lIJen lIJz I.A 4:( C)z 4:( 2 0.30 0.20 0.10 ~..-• 0.00 .,~"",..IL "1 0 0 '7 0 13 5 13 0 0 I 0 7 2 9 0 0 0 0 I 0 6 -- 0 V G C T 5 5~0 V G C T 5 55 0 V G C T S 55 -- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I tl I II II I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER aREAKUP D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T-TALKEETNA 5-SUNSHINE S5-SUSITNA STATION NOTES: I.A.CRITERION:LESS THAN 0.05 mg./I.(EPA 1976) I.B.ESTABLISHED TO PROTECT WATER SUPPLIES. 2.AT SUSITNA STATION.6 SUMMER OBSERVATIONS,I WINTER OBSERVATION AND 6 BR EAKUP OBSERVATIONS WERE LESS THAN 0.010 me;,./I. 3.(d)=DISSOLVED DATA SUMMARY-MANGANESE SOURCE:USGS (d) FIGURE E.2.113 W-lm ct 0::: W ~ frl 0::: -l ~0...... c ~-wenwz ct (!)I.Azct ~ 1.50 l.00 • 0.50 •I-iii • •••lit H 0.00 II 1.1 -l- 0 0 6 0 "12··6--13 0 0 I 0 5 I 9 0 0 0 0 4 0 6 I--f- 0 V G C T 5 5::t 0 V G C T S 55 0 V G C T S S5 f-f-- I I I I I I I I I I I I II I I I I I I I I I I II I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S -SUNSHINE 55 -SUSITNA STATION NOTES: I.A.CRITERION:LESS THAN 0.05 rng./I,(EPA 1976). LB.ESTABLISHED TO PROTECT WATER SUPPLIES. 2.AT SUSITNA STATION.I BREAKUP OBSERVATION WAS LESS THAN 0.01 rng./1. 3.(t)=TOTAL RECOVERABLE. DATA SUMMARY-MANGANESE (t) SOURCE:USGS FIGURE E.2.114 MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION 003 1002 001 .- JOOO ~ °0 "3 °3 3 13 0 °I 0 2 2 9 0 0 0 0 0 0 6 f--r-. D V G C T S SS D V G C T S SS 0 V G C T S SS r-r-; I I I I I I I I I I I I I I I I I J I I I I I I I I I I I I I I I I I I I I 111 I I I I I I I I I I I I I I I I O. 0. ';-O. Cl .E- ow ~o (I) (I)o -;;0.0 :z:->-a:: ~I.A a::w 2: SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA NOTES: I.A.CRITERION:LESS THAN 0.00005 mg./1.(EPA 1976). LB.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 2.AT GOLD CREEK,I SUMMER OBSERVATION AND THE I WINTER OBSERVATION WERE LESS THAN 0.001 mg./I. T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION 3.AT SUSITNA STATION,8 SUMMER OBSERVATtONS,7 WINTER OBSERVATIONS, AND THE 6 BREAKUP OBSERVATIONS WERE LESS THAN 0.0005 mg./I. 4.(d):DISSOLVED DATA SUMMARY -MERCURY (d) SOURCE'USGS FIGURE E.2.115 "'-CC---C-'-'l 0.0 "o E. wffi 0.00 «a::::w ~uwa:::: ....J«b 0.0 I- CI :I: >-a:::: ~u 0::: W :Ii I.A 0.0 -b.106b8 I I . - ----_~- 0 0 6 0 9 6 13 0 0 I 0 5 I 9 0 0 0 0 3 0 6 I-f- D V G'C T 5 55 D V G C T 5 S5 D V G C T S 55 I-f- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER I3REAKUP 4.AT GOLD CREEK I THE I WINTER OBSERVATION WAS LESS THAN 0.0005 mg./!. 5.(t)=TOTAL RECOVERABLE. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES: I.A.CRITERION:LESS THAN 0.00005mQ./1.(EPA 1976). LB.ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 2.AT TALKEETNA,I SUMMER OBSERVATION WAS LESS THAN 0.0005 mQ./1. 3.AT SUSITNA STATION,7 SUMMER OBSERVATIONS,7 WINTER OBSERVATIONS AND 4 BREAKUP OBSERVATIONS WERE LESS THAN 0.0005 mg./I. S-SUNSHINE 55 -SUSITNA STATION SOURCE:USGS DATA SUMMARY -MERCURY (t) FIGURE E.2.116 1 l z:1. w :lI::: U Z o. MEAN •MINIMUM •MAXIMUM NO.OF OBSERVATIONS LOCATION USO .100 050 --•n n .~ 000 ••('- 0 0 6 0 I 6 5 0 0 I 0 0 I 3 0 0 0 0 0 0 I I-~ D V G C T S SS D V G C T S SS 0 V G C T S SS r-r- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I o ......... t-wcfi 0 eXa::: W ~ Uwa::: ..J !et50 ~ SUMMER WINTER BREAKUP D-DENALI V-VEE CANYON 'G-GOLD CREEK C-CHULITNA T-TALKEETNA S-SUNSHINE SS-SUSITNA STATION NOTES: I.CRITERION:LESS THAN 0.025 mg./1.(McNEELY It 01.1979). 2.CRITERION:0.01 OF THE 96-HOUR LC50 DETERMINED THROUGH BIOASSAY (EPA 1976). 3.THE ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. 4.AT GOLD CREEK,2 SUMMER OBSERVATIONS WERE LESS THAN 0.05 mg./I. 5.AT TALKEETNA,THE I SUMMER OBSERVATION WAS LESS THAN 0.05 mg./I. 6.AT SUNSHINE,2 SUMMER OBSERVATIONS WERE LESS THAN 0.05 mg./I. 7.(t)=TOTAL RECOVERABLE. SOURCE:USGS DATA SUMMARY-NICKEL (t)FIGURE E.2.117 -"-cit .E- o UJ>..J 0 CJ) ~ 0 c N- (.) z N I. 0.30 0.20 0.10 .. . ..n ... 0.00 ..u t .~j loIII~•~ -.. 0 0 ;,0 3 3 13 0 0 I 0 5 I 9 0 0 0 0 2 0 6 -"'- D V G C T 5 55 D V G C T 5 55 0 V G C T 5 SS 1--1-- I I I I I I I I I I I I I I I I I I ,I I I I I I I I I I I I I I I I I I I I I I I I I I I II I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP O-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA S-SUNSHINE 55 -SU5ITNA STATION NOTES: I.CRITERION:LESS THAN 0.03 mg./I.(McNEELY et 01.1979). 2.CRITERION:0.01 OF THE 96 -HOUR LC 50 DETERMINED THROUGH BIOASSY (EPA 1976). 3.THE ABOVE CRITERIA BASED ON HUMAN HEALTH EFFECTS. 4.AT SUSITNA STATION,8 SUMMER OBSERVATIONS,8 WINTER OBSERVATIONS AND 4 BREAKUP OBSERVATIONS WERE LESS THAN 0.020 mg./I. 5.AT GOLD CREEK THE I WINTER OBSERVATION WAS LESS THAN 0.012 mg./1. 6.(d)=DISSOLVED SOURCE:USGS DATA SUMMARY -ZINC (d)FIGURE E.2.118 0.00 0.30 "Cl E -0.201.IJ ...Jm«a:: 1.IJ>o (.) 1.IJa:: ...J 010« . 5 I--c: N-(.)1.----" z N .. -II> .~-.. ~ 0 0 6 0 II 6 13 0 0 I 0 5 I 9 0 0 0 0 3 0 6 -- D V G C T S SS D V G C T 5 55 0 V G C T 5 55 -- I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I •MAXIMUM MEAN •MINIMUM NO.OF OBSERVATIONS LOCATION SUMMER WINTER BREAKUP 4.AT SUSITNA STATION,I SUMMER OBSERVATION AND 2 WINTER OBSERVATIONS WERE LESS THAN 0.020 mg./1. 5.(t)=TOTAL RECOVERABLE. D-DENALI V-VEE CANYON G-GOLD CREEK C-CHULITNA T -TALKEETNA NOTES: I.CRITERION:LESS THAN 0.03 mg./I.(McNEELY et 01.1979). 2.CRITERION:0.01 OF THE 96-HOUR LC50 DETERMINED THROUGH BIOASSAY (EPA 1976). 3.THE ABOVE CRITERIA ESTABLISHED TO PROTECT FRESHWATER AQUATIC ORGANISMS. S-SUNSHINE SS -SUSITNA STATION SOURCE:USGS DATA SUMMARY-ZINC (t) FIGURE E.2.119 SLOUGH SA GRO 8-3Ae a-4A e \ ~ ~ )UND WATER CONTOURS LEGEND: •GROUND WATER OBSERVATION WELL(ego 8-10.) NOTES: I)ELEVATIONS ON SEPTEMBER 3,1982 WITH DISCHARGE AT GOLD CREEK =14,600 CFS. 2)CONTOURS IN FEET ABOVE MEAN SEA LEVEL. FIGURE E.2.120 ---"--- 9-12~ SLOUGH 9 GROU 9-10. I" roO\ /&01- / 9-3. 9-2. FLOW Q 9-IA. ALASKA RAILROAD LEGEND: •GROUND WATER OBSERVATION WELL (eg.9-15.) NOTES: I.ELEVATIONS ON SEPTEMBER 6,1982 WITH DISCHARGE AT GOLD CREEK:12,200 CFS. 2.CONTOURS IN FEET ABOVE MEAN SEA LEVEL. ~D WATER CONTOURS FIGURE E.2.121 "-./V '"/' '/ ~ '"/ "'-/VOLUME I "/') /\ /\ \ /\ /\ /SURFAT AREA-.\ \ /I \ \J /"- "\ /'\ \ /\ I \ \ \ \ - - ,.,.. """' - -I 26 24 22 20 I- IJJ ~18 ::Eo I-16....o CD ::IEo 14a:: IL z ~12....- ~w ~10 8 6 4 2 70 60 2 AREA (ACRES) 50 40 30 3 4 5 VOLUME (ACRE-FEET x 100) 20 6 10 7 o 8 -SALLY LAKE AREA-CAPACITY CURVES FIGURE E.2.122 LJ ) ~'",',~IA":~ .DELUSION'...••.6\d ".~~~,j~.-aoo~~jj;rk.-----+/1:.~AS X ';:F!?IDeadmanCree~,"i;..'.'.<:...10 ..: LEGEND: NORMAL MAXIMUM --....--~~-OPERATI'lIG LEVEL EL.218S CONTOURS ARE IN-----2300-----FEET ABOVE MSL ----SLOUGH --'.-TRI BUTARY WATER BODIES TO BE INU 2 MILES ! ( ! .../21 ~./- i 3 V kKosinaCree WATANA RESERVOIR Portage Creek .J7 0\v= LEGEND: ,-------NORMAL MAXIMUM OPERATING LEVEL El.1455 --2000 CONTOlJRSIN FEET ABOVE MSL -'-- - - -SLOUGH •.-..-TRIBUTARY WATER BODIES TO BE INUNDATE o I rDBY DEVIL CANYON RESERVOIR I I t SUSITNA RIVER WalanaDam o SCALE ~..~~~2_MILES /-............. / I / / / I / SUSITNA RIVER // DRAINAGE BASIN 'v / /" /" ,,/ ./®..-..-"-//' .,.----.,.- ,// ,,/ /' /" /' / / I / I / / / I / / / I / / I I I \ \ \--\/, /""-"/""/"-,/'""---_/"'- "- " TOWNSH IP GRIDS I RIGHTS IN THE SOURCE:DWIGHT 1981 -- LEGEND: TOWNSHIPS I.SUSITNA 2.FISH CREEK 3.WILLOW CREEK 4.LITTLE WILLOW CREEK 5.KASHWITNA 6.SHEEP CREEK 7.MONTANA CREE K 8.TALKEETNA 9.CHULINA (CHUNILNA) 10.SUSITNA RESERVOIR II.CHULITNA 12.TOKOSITNA 13.KROTO -TRAPPER CREEK 14.KAHILTNA 15.YENTNA 16.SKWE NTNA 17.HAPPY 18.ALEXANDER CREEK t? o 10 20 MILES SCALE ~~~~iiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiiil o I '-•CANTWELL _,/~~,/----,/--~",/, ,./",/\,~/,--- I J I /0> / / / ( \ \ \ 6&V \ \ \ ~\ Q \ \ I I ./.....------- /' /' /' //'/' ......,// """,--..,..." INVESTIGATED FOR WATER !SUSITNA RIVER BASIN FIGURE E.2.125 1 )]')))l SELECT LOCATIONS OF COOK INLET SALINITY ESTIMATES ~ LEGEND: ~SALINITY ESTIMATE LOCATIONS ~ .~... ~ ~ ANCHORAGE KENAI PENINSULA BLrlNG SOUND o 20 40 FIGURE E.2.126 30,000 25,000 20,000 ~15,000 z ::::i <l:en 10,000 5,000 o ~ ~. ~~~~~~.......-........ ,.....~.......,........ ""~......... ~10--""-/./'/.. 1-0-•.......:./ /~./.' /..~ ?,,/ .' :?~,t'.~~ OCT NOV DEC JAN FEB SOURCE;RMA 1983 NOTES: I.CURVES PLOTTED USING END OF THE MONTH SALINITIES FOR NODE 27. 2.I PPT=1000 mg/I. TEMPORAL 51 COOK INLET NEAR ~~.----~.. ~_....~.~-'".1.-.-',, .""..,'.,","~~, \',~.~.,\,,~ ~'...,~".,'".:\."':-~:- _..... '"".....................~~"":".:::--'~-......' - ;,...-"'" MONTHS APR MAY JUN JUL AUG SEP ALINITY ESTIMATES FOR :THE SUSITNA RIVER MOUTH LEGEND: PRE -PROJECT ---WATANA FILLING (WY 1992) _.-.WATANA OPERATION (WY 1995) FIGURE E.2.127 ~~i--'" ">/ /' VOLUME 1/'\SURFACE AREA /1\ V \/\ /\ I \ \ ..... - - r'" I - 2600 2500 2400 2300 2200 2100 l- I.LJ I.LJ IL. Z eooo0 ~>I.LJ ~ I.LJ 1900 1800 1700 1600 1500 1400a 6 2 SURFACE AREA (ACRES x 10 4 ) 5 4 :5 2 4 6 8 ~ VOLUME (ACRE-FEET x 10 6 ) 12 o 14 ..... WATANA RESERVOIR VOLUME AND SURFACE AREA FIGURE E.2.I 28 I I~1 / / l ~/ V !VOLUME / /~/f-SURFACE AREA V 1\/ V \ 1\ /1 1\ /I \ I \ I 1 I - ..... 1500 1400 1300 r --.....ww,....l4. Z Q !c( l~:>1200w !-J ILl .~ 1100 1000 900 o 12 2 SURFACE AREA (ACRES x 103 ) 10 8 6 4 4 6 8 10 VOLUME (ACRE-FEET x 10 5 ) 2 12 o 14 DEVIL CANYON RESERVOIR VOLUME AND SURFACE AREA FIGURE E.2.129 20 18 16 14 -;;;12 LLo ooo ~10 uJ C) a::« :I:rn o 8 ~------+----_----.Jf----------j----------jl---~-----f----- 6 ALL CASES 4 2 o I OCT NOV DEC JAN FEB MAl OPERATIC ALTERNATIV NOTES: I)LETTERS DESIGNATE THE VARIOUS SCENARIOS CONSIDERED (ie.A=CASEA). 2)FLOW REPRESENTS GOLD CREEK FLOWS. 3)Three additional flow regimes were investigated with respect to project economics.These regimes are discussed in Exhibit B,pages B-2-l23 thru B-2-128 . &are identified as cases E,F,&G.MINI MUM FOR D - C2--~- CI - C A2 \ AI C,e,e,D A AI A2 I I \ A ,- i - , APR MAY JUN JUL AUG SEP ~L TARGET FLOW iFLOW SC ENARIOS FIGURE E.2.130 : POTENTIAL Wj , ".LOCATION MAP o 4 8 MILES SCALE ~i~~5iiiiiiiiiiiiiiiiiiiii! TANA BORROW SITES LEGEND E~~:=J BORROW I QUARRY SITE LIMITS o 2 MILES SCALE ;! FIGURE E.2.131 I - - - 1700 1600 SUSITNA RIVER FLOW - ( N 3 228 000 "'-1 / N 3 228 500 REFERENCE:BASE MAP FROM COE,1978 "'~200'WATANA TOPOGRAPHY SHEETS 8 B 9 OF 26,COORDINATES IN FEET,ALASKA STATE PLANE (ZONE 4) WATANIJ QUARRY 51 APPROXIMATE QUARRY SITE LIMIT QUARRY SITE L ~ TE L LEGEND ___BORROW SITE LIMIT l.ENTIRE QUARRY SITE LIES WITHIN PROPOSED WATANA RESERVOIR LIMITS 2.MATERIAL LIMITS INFERRED FROM PRELIMINARY MAPPING AND ARE SUBJECT TO REFINEMENT AND VERIFICATION IN OESIGN LEVEL INVESTIGATION. 3.SURFACE ELEVATIONS FROM I"~200'TOPOGRAPHY -COE,1978, TRACED AT 25'CONTOUR INTERVAL. 4.PHOTO TAKEN AUGUST,1981. 0~~~~~2~0;ii0iiiiiiiiiiiiiiiiiiii400iiil FEETSCALE~, FIGURE E.2.132 N ~O 000 - BORROW SITE 0 ( . I -I .-4 , L t -, -----~~._-----------_.-------,---'---..;--------'--------- REFERENCE:BASE MAP FROM 1978,COE -I".200'OAMSITE TOPOGRAPHY, SHEETS 13-15,18-20 OF 26 r L r i------ l'i I I // / / " "/ " , / "/ ) / "/ / / LEGEND ---BORROW SITE LIMIT NOTES MOST OF BORROW SITE LIES OUTSIDE OF PROPOSED WATANA RESERVOIR LIMITS. 2.BORROW MATERIAL IS COMPRISED OF UP TO 600 FEET OF GLACIAL TILL,OUTWASH,AND ALLUVIUM. 3.CONTOUR INTERVAL 25 FEET,REDUCED AND TRACED FROM REFERENCED BASE MAPS. 4.PHOTO TAKEN AUGUST,1981. ~0~~~4~00iiiiiiiiiiiiiiii8iiil?0 FEETSCALEi:, WATANAIBORROWSITE D FIGURE E.2.133 ·~ -...-- •• o ClO --_/ 1&. REFERENCES:BASE MAP FROM COE ,1978 -I"•200'WATANA TOPOGRAPHY,SHEET 6 a II OF 26 R aM,1981-1".400'DEVIL CANYON RESERVOIR MAPPING,FLIGHT 5 (6-8),MANUSCRIPT 2 COORDINATES IN FEET,ALASKA STATE PLANE (ZONE 4) /' LEGEND -----BORROW SITE LIMIT NOTES PORTIONS OF BORROW SITE LIE WITHIN THE PROPOSED DEVIL CANYON RESERVOIR LIMITS. WATANA BORROW SITE E 2.MATERIAL LIMITS BASED ON FIELD EXPLORATION,MAPPING AND AIR PHOTO INTERPRETATION.FINAL LIMITS OF BORROW MATERIALS SUBJECT TO RESULTS OF DESIGN INVESTIGATIONS. 3.CONTOUR INTERVAL 25',TRACED AND/OR REDUCED FROM REFERENCED BASE MAPS. 4.PHOTO TAKEN AUG UST,1981. o 400 800 FEET SCALE ~i~~~iiiiiiiiiiii~! FIGURE E.2.134 -i REFERENCE:BASE MAP FROM R8M,1981-1"'2000'RESERVOIR MAPPING, COORDINATES IN FEET,ALASKA STATE PLANE (ZONE 4 l. /----.~---. /~. /' /'/----"j'!..----- // I I ( I') ,I ,.'/ J I ,(' // /'f'I~ 1/i I ,I ,J ,.'I J~j r!",I) ,//1,'1 (~) I , I.I./,/.~NATURAL FLOW RESTRICTION ),~WEIR /11 1./ !'(~-)r:') ,-_~Ii / I r~ L~~' ..l.,.,000 LEGEND ---BORROW SITE LIMIT NOTES ENTIRE BORROW SITE AS ORAWN LIES WITHIN PROPOSEO OEVIL CANYON RESERVOIR LIMITS.LOCAL DEPOSITS ARE INFERRED TO CONTINUE UP SLOPE BEYOND LIMITS SHOWN. BORROW SITE I WATANA BORROW SITE I 2.MATERIAL LIMITS BASED ON FIELO MAPPING AND AIR PHOTO INTERPRETATION.FINAL MAPPEO LIMITS OF BORROW SITE SUBJECT TO RESULTS OF DESIGN INVESTIGATIONS. 3.CONTOUR INTERVAL 100',TRACED FROM 1"'1000'ENLARGEMENT OF REFERENCED BASE MAP 4.PHOTO TAKEN AUGUST,I9B1. 0~~~'~OOO~iiiiiiiiiii20~PO FEETSCALEl:, FIGURE E.2.135 13 12 " 10 9 CJ)u...8(.) 8 Q ~ w 7 <.!) a:: <l: :I: (.) CJ)6 15 5 4 3 2 I I I I I I I I I I I I I f-- f-- f-- f-- f-- r-- f-....,-r,I _____________-.J L ___.... -- -- ..NATURAL.:• I I I I I I I I I I I I I LEGEND: MINIMUM FLOW REQUIREMENT DURING FILLING OF WATANA ---MINIMUM FLOW REQUIREMENTS DURING OPERATION OF WATANA AND WATANA/DEVIL CANYON. OCT NOV DEC JAN FEB MAR APR MAY JUN TIME OF YEAR JUL AUG SEP OCT NOV MINIMUM FLOW REQUIREMENTS AT GOLD CREEK FIGURE E.2.136 100 9 8 7 6 5 4 3 en I!.. U o 2oo UJ (!) a:«:x:uen o 10 ~9 ~8 a:7« ~6 UJ ~5 :x:..... 4 -----ii'""--P--...... ~~..-.-.-•----• 2 I I 2 5 10 20 50 80 90 95 98 99 PROBABILITY OF EXCEEDANCE NOTE:PERIOD OF RECORD IS WY 1950 -WY 1981. THREE -YEAR MEAN DISCHARGE AT GOLD CREEK FIGURE E.2.137 2200 WATANA DAM CREST ELEVATION 2000 I-w W I.L zo ~> lLJ -I lLJ 1800 1600 1400 40 J ~------ /~ .,- ---_/~- 30 CJ) LL () 0 0 0- w 20· C) ll::c:r :I: () ~ I::) 10 a LEGEND: 10 %EXCEEDENCE 50%EXCEEDENCE 90 %EXCEE DENCE M J J 1990 PROBABIL ITY PROBABILITY PROBABILITY WATANA WATER LE' GOLD CREEK FLOWS DURING I - --tIO %-...'---- -~/~..,./,,:::::--'------------~~.::--~-------\---50% // ;','{/90% ~ 'I ~ WATANA WATER LEVELS M A D ~M I ~ELS AND ~ESERVOIR FILLING I I GOLD CREEK· FLOWS o NOTES: I.NATURAL STREAM FLOWS UNTIL MAY 1991 WHEN FILLING BEGINS. 2.AVERAGE MONTHLY VALUES PLOTTED IN MIDDLE OF MONTH. FIGURE E.2.138 50 40 ---CD Cf)'\ LL \(,.)30 0 0 \0 LaJ (,!) D:: <t ::I: (,)20Cf)c ® 10 o 5 10 15 20 25 30 LEGEND: AUGUST NOTES: AUGUST 1958 FLOWS FILLING SEQUENCE II AUGUST 1958 FLOWS -WATANA MINIMUM STORAGE CRITERIA VIOLATED FILLING SEQUENCE 2,AUGUST 1958 FLOWS -WATANA CAPABLE OF ABSORBING HYDROGRAPH I.WATANA FLOW ASSUMED TO BE 84 %OF GOLD CREEK FLOW. ?RESERVOIR FILLING CRITERIA EXCEEDED WITH SEQUENCEQ) 3.NEGLIGIBLE CHANGE .IN DAM HEIGHT DURING FLOOD EVENT 4.MAXIMUM RELEASE AT WATANA 31,000 CFS (COMBINED POWERHOUSE AND OUTLET FACILITY DISCHARGE). FLOW VARIABILITY AT GOLD CREEK DURING WATANA FILLING FIGURE E.2.139 1 1 1 1 NOTE:THE ELEVATIONS AND DISTANCES PRESENTED IN THIS SCHEMATIC ARE NOT INTENDED TO PROVIDE QUANTIFICATION OF PROJECT EFFECTS. CD PERCHED TRIBUTARY BED (UNAFFECTED BY LOWERED LEVEL OF SUSITNA RIVER) COBBLE ~ ~......... I BACKWATER AREA (PRE-PROJECT CONDITIONS I--------J.~.~GRAVEL DEPOSITED BY TRIBUTARY -~''W\fUi8iiiiilt ""-"""WATER LEVEL ........(POST-PROJECT CONDITIONS) ~~------- ..................7 <SUSITNA RIVER WATER LEVEL (PRE-PROJECT CONDITIONS) TRIBUTARY WATER LEVEL TRIBUTARY THALWEG ®DEGRADATION OF TRIBUTARY BED (UPSTREAM PROGRESSION OVER TIME) o 12 4 2 10 14 i= w ~8-zo i= ~~6 IJ..I o 20 40 60 80 100 DISTANCE (FEET) 120 140 160 180 SCHEMATIC OF THE POTENTIAL EFFECTS OF THE SUSITNA RIVER ON A TYPICAL TRIBUTARY MOUTH FIGURE E.2.140 4.0 3.5 3.0 2.5 0 0 w r0:: ::) !:i: 0::2.0w Q. ~ W I- 1.5 1.0 0.5 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: I.MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY NATURAL FLOWS. 2.GOLD CREEK DISCHARGE (CFS): OCT 4280 NOV 2560 DEC 1790 JAN 1460 WATANA FILLING:DOWNSTREt 49.00 155.00 161.00 167.00 173.00 179.00 185.00 ~M TEMPERATURES -OCT TO JAN FIGURE E.2.141 4.0 3.5 3.0 2.5 ------------~ APR30 ~ (.) o wa:: ::::> !;:( ffi 2.0 ll... :::!:w I-- 1.5 1.0 0.5 APR 15 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: I.MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY NATURAL FLOWS. 2.GOLD CREEK DISCHARGE (CFS); JAN 1460 FEB 1240 MARI120 APR 1240 WATANA FILLING:DOWNSTREA~ 49.00 155.00 161.00 167.00 173.00 179.00 185.00 ~TEMPERATURES -JAN TO APR FIGURE E.2.142 4.0 3.S 3.0 2.S u 0 wa:: :J ~2.0a::wa.. :::!:w I- I.S 1.0 os 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: I.MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND LOW FLOW DISCHARGE. 2.GOLD CREEK DISCHARGE (CFS): OCT 2020 NOV 1460 DEC 1320 JAN 1260 WATANA FILLING:DOWNSTREA LOW WIN '9.00 155.00 161.00 167.00 173.00 179.00 185.00 ~TEMPERATURES -OCT TO JAN 1rER FLOWS FIGURE E.2.143 4.0 3.5 3.0 --~APR 30 _-----....~-------------- -- 1.0 05 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: I MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND LOW FLOW DISCHARGES. 2.GOLD CREEK DISCHARGE ( CF S); JAN 1260 FEB 1220 MAR 1120 APR 1240 WATANA FILLING DOWNSTREA~ LOW WIN~ 49,00 155.00 161.00 167.00 173.00 179.00 185.00 TEMPERATURES-JAN TO APR "ER FLOWS FIGURE E.2.144 9.0 8.5 8.0 7.5 7.0 u 0 w 6.50:: ::::> t:c 0:: Wa. ::!Ew I-6.0 5.5 --.. ______SEP 15 ---.___AUG 15.-.-.........--.......-.-.-....-._.-.............-.--.""'-._._..--.......4.5 5.0 ------------- 4.0 SEP 30 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143 NOTES: I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA AND MEDIAN FILLING FLOWS. 2.GOLD CREEK DISCHARGE (CFS): JUN 6000 AUG 12000 JUL 6700 SEP 9000 RIVER MILES WATANA:SECOND YEAR OF F ...---.:-.------..--.0-0-0-0-°-0_0-0- .00 149.00 155.00 161.00 167.00 173.00 179.00 185.00 ILUNG DOWNSTREAM TEMPERATURES -SUMMER FIGURE E.2.145 9.0 8.5 8.0 7.5 7.0 u ~ w 6.50:: ::j f-- <[ 0:: Wa.. :::!:w I-6.0 5.5 5.0 -.....AUG 15--.-'-.-.--.----."""'-.---._........... .----."""'-.--'--._........... .----.........- -----...._-------.. _____ SEP 15---------------------- 4.5 4.0 SEP 30 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143 NOTES: I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA AND MEDIAN FILLING FLOWS WITH AUGUST FLOW REDUCED TO 6,000 CFS 2.GOLD CREEK DISCHARGE (CFS), JUN 6000 AUG 6000 JUL 6700 SEP 9100 RIVER MILE WATANA:SECOND YEAR OF FILL 6,000 C· -0-0_.---..-...,.-.....'--.-..., o~.-......-......----.---=:.:::4..........._._. 1.00 149.00 155.00 161.00 167.00 173.00 179.00 185.00 .ING DOWNSTREAM TEMPERATURES-SUMMER FS IN AUGUST FIGURE E.2.146 J 1 ]]] a 2 CJ) D:: W ~ ~ ~:3 0- Wo 4 5 ~..~/~~..~-'~/~.-,v'I/r VP'''::r·d ..ff l/IT",..,..".."....,..,.V.~'"..~~-.,.................., ~/lJ'V,J V~~/~/~~v ./V~;:f /' ....I/""/./~ ~',//'~:r</-/~',/ .,..~v~./I/V~,~V ~V ........~,~~'//~~~V~~'~V/-~~,../ ,:/~/ ,.I'///V/""/ ~~~.~ / ~/ / /' /',,,' \f' .2 .3 .4 .5 .6 .7.8 .9 I 2 3 4 5 I 6 7 8 9 10 2 3 4 5 6 7 8 9 100 MICRO EINSTEINS PER SQUARE CENTIMETER PER SECOND 2 3 4 5 6 7 8 9 1000 LEGEND: DATA --a--- -0- ---0--------fr-a--- DATA SOURCE:RaM 1982 STATION STA.II STA.II STA.II STA.II DATE JULY 15,1982 JULY 28,1982 SEPT.la,1982 AUG.10,1982 EKLUTNA LAKE LIGHT EXTINCTION IN SITU MEASUREMENTS FIGURE E.2.147 17,060 01 SCHARGE ( C FS) 9,500 13,3005100 86 t----fl----ff---_t_----+--------I-------+------+----II 74 t---t-----_+_------I------_+_-------I--------I---1 90 t------t-'--1f--+-~l---_t____\:li~--+--------I------_+_---....>r-_+____I1 78 t---+------+-------I-------+------+--------I---1 1,500 2,000 94 --+-r-----....,------...,....-----....,.-----------I~- ~o >-u ~82 r-_t_-----+-----+-------+------+-------+------I <3 ~ lL. W 70 L.....-.....L-.....I........l...-....L...-......L...""""'--....J 100 300 500 700 PLANT OUTPUT (MW) 900 1,100 WATANA-UNIT EFFICIENCY AND DISCHARGE OPERATING RANGE (AT RATED HEAD) FI.GURE E.2.148 / / MAX.YEAR (WY 1956) """,/--- ,I"/ \/ \I \I, \I,/"/,I ,I ,I"/ \f"4--MI N.YEAR \/(WY 1970) \/ \/,/,,//,/'.,/ 2190 2180 2170 2160 i="w W LL 2150 -.Jw>W -.J 2140a:: 0>a::wen 2130wa:: e::{ z e::{2120l- e::{ ~ 2110 2100 2090 2080- 2070 --.........--L..-...-.........-_L..-..._.........._----ll....-_........._----ll....-_.........._----ll....-_.........._.....-I OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP WATANA RESERVOIR WATER LEVELS (WATANA OPERATION) FIGURE E .2.149 '"l0- U r---r---r---r---r---T---- 140f-----'----f-----f-----f-----f-----f-----t----,--- I I 30 f-------j----o-I--t-----j---j----+---+ I, i " I~19!!1 LEGEND' ~=JINFLOW OUTFLOoV 19!!Z 19!13 19!!4 19M 19!!6 19S7 19!!8 19!!9 1960 1961 196Z 1963 ZZOO ,-----.---.----,------.-----r---,---r-------r-----,------r-----r-----r-----r-- i ~2100 ~ ..J III 2000 '-----1-~----l--1-9!!-1-1--1-9-52-'-----1-9-!!3-'------19!l4----'--1-9M----'--1-9!!-6-'-----~-7---19-!l8--'----19ll-9---'---196-0---'--19-6-1----'-19-6-Z----'--I96-3 !!O 1----1----+---I---+--+--+---t- ~ 'I!I40f---t---t---t---t---t---t---t----t----t---+---+---+---+,7- 1 +-- "II GOLD CR 196Z 19631961196019!!919!!719!16 'I , n , ":':'1 ~ I, "'I .,II I "'I 'I 'I 'I " I 'I II r.I--~I " II,,I " -}-i,'--4-1--+-, I I~ :I I l II'"I'I lI, I , I,,,I,, I ,!"I I I,,f--t-\--~"t -4 ~,I ,,1 ~l ' ' I I',,,,,I I I,,), I ,1 1 ,I rJ r I I I JUL ,I : I ~,l Jl,~~~/I rl :Br~r f!.n.:n~'in)\"\~U ~1\1i 1'+~V.·c '""'i'i •I i ~l\J • !\j ~'".\J .~u '-' 19!!!!19!!419!1319!!2 G 30 I----+---+--¥II+--+--+--,.,I:-I---j-H---!"t"+--+---+i+---I----;:;-j-----t'-t-~ I''L liT ~[1 :~ II ,I ,',I n I I "1',1 ,II':~:~:U:ZO f----;t',-I--t-it-I--:-i-I--i-"7I--j-=+I--f-'-I--t-tI--r-'t--+-It--t r I ' : I ~:" :I I I I I:rJ I , I I : I I l':' '"l0- U § III.. II::..o '"o WATANA SIML ~ 11 --,--_~~-+_--f___-_+--+ + I "~l _.0 II II I II 1 IIII)~II II lUI ~Lj 1 1 1 11:1 I I IU I 1964 1965 1966 WATER YEAR 1961 1968 1969 1910 1911 191Z 1913 1914 1915 1916 1911 1978 1919 Ino 1981 WATANA INFLOW AND OUTFLOW 1964 1965 1966 WATER YEAR 1967 1968 1969 1971 197Z 1973 1914 1915 1916 1911 1918 1919 1911O 1981 WATANA RESERVOIR ELEVATION n ! L -r.---+---+---+----+-- I .\J.U l)LJ U U tJ \J "J.U U LJ U \.J \..'lo \J 'l 1964 1965 1966 1961 1968 1969 1910 1911 197Z 1913 1914 1915 1916 1911 1918 1919 1980 1981 WATER YEAR EEK PRE-AND POST-PROJECT FLOW LATED RESERVOIR OPERATION FIGURE E.2.150 LEGEND: -----PRE-PROJECT - - -WATANA OPERATION 1=:;1 ELEVATION CHANGE ••••.•.EXTRAPOLATED v V ./···.. .. ··· : : . VCHANN'L BOTTOM - 10,000 20,000 30,000 LRX 57 RATING CURVE(2) GOLD CREEK DISCHARGE (CFS) o 756 748 754 746 MAY JUN JUL AUG SEP MINIMUM FLOWS MAY JUN JUL AUG SEP MEAN FLOWS WATANA OPERATION:MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER M ILEI42.3 MAY JUN JUL AUG SEP MAXIMUM FLOWS 756 754 746 748 752 752 ~ f-f- W W W W lJ..lJ.. ~ ~ z z ~750 0 f- i=750 «« >> w W ...J ...J W W NOTES: I.WATER SURFACE ELEVATION ABOVE RATING CURVE. 2.RATING CURVE BASED ON GOLD CREEK DISCHARGE AND OBSERVED 1982 WATER LEVELS (ADF6G 1982). FIGURE E.2.151 LEGEND: PRE -PROJECT ---WATANA OPERATION (:::::::::1 ELEVATION CHANGE •••••••EXTRAPOLATED 618 ......~:-~.....618 ~ t-t- W W W Wu..u.. ~~ z zo616o 6i6 i=t-;=;;=;w W--J --JWw 614 614 / / / / .I···: : ···. :CHANNFl BOTTOM AT -:El.60P-5 I -.. o 10,000 20,000 30,000 lRX 35 RATING CURVE(2) GOLD CREEK DISCHARGE (CFS) 612 620 622 MAY JUN JUL AUG SEP MINIMUM FLOWS MAY JUN ,IUl AUG SEP MEAN FLOWS WATANA OPERATION:MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER MILE 130.9 MAY JUN JUL AUG SEP MAXIMUM FLOWS 612 620 622 NOTES: I.WATER SURFACE ELEVATION ABOVE RATING CURVE 2.RATING CURVE 8ASED ON GOLD CREEK DiSCHARGE AND OBSERVED 1982 WATER LEVELS (ADF8 G 1982). FIGURE E.2.152 LEGEND: PRE-PROJECT ---WATANA OPERATION Imtl ELEVATION CHANGE •••••••EXTRAPOLATED WATANA OPERATION:MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER MILE 124.4 10,000 20,000 30,000 LRX 28 RATING CURV~2) GOLD CREEK DISCHARGE (C FS ) ........ V / V .I ~ :. f .' VCHANNE BOTTOM ~548 o 550 554 556 5563 .....w W lJ... zo f=552 ~w ...J W MAY JUN JUL AUG SEP MINIMUM FLOWS MAY JUN JUL AUG SEP MEAN FLOWS 548 MAY JUN JUL AUG SEP MAXIMUM FLOWS 550 554 55'8'_ . 556 zoi=552 ~w ...J W .....w W lI.. NOTES: I WATER SURFACE ELEVATION ABOVE RATING CURVE. 2.RATING CURVE BASED ON GOLD CREEK DISCHARGE AND OBSERVED 1982 WATER LEVELS (ADF 8G 1982). FIGURE E.2.153 5oo ~J20 I---_+_- U ooo 100 I~-_+_- 160 I---_+_- 180--......-- w ~80 I----+-- « :I:u ~601-------"!IIJlo 1401----+-- 353010152025 TIME (DAYS) 1:50 YEAR FLOOD (SUMMER) 5 1\ I \ ~INFLOW \ II .~l ____l~U!~LOW ~'N ~\ L OUTLET FACILITIES AT FULL CAPA- CITY (ASSUMED POWERHOUSE FLOW I 7000 CFS) 1--"\POWERHOUSE AND OUTLET FACILITIES OPERATING (MATCHING INFLOW) 20 10 70 90 00 80 w ~40« I U ~30 ~60 u o 8 50 \MAX WSEL =2193.0 \ I/"~ I \ \ OUTLET ~/\FACILITIES ~AT FULL CAPACITY r/1 1 71...I VPOWERHOUSE AND OUTLET FACILITIES OPERATING (MATCHING,INFLOW) 2202 2200 -2198I-w W l.L -2196z 0 ~~2194 ~ILl ..J ILl Q;;2192 0>0::: ILl ~2190 0::: 2188 2186 2184 o 5 10 15 20 25 30 TIME (DAYS) I:50 Y EAR FLOOD (SUMMER) 35 2202--..,.-- 22001---+-- ~~198 1----4---w W I.L i 2196 1----4--- o ~~2194 I---_+_- ..J ILl 6 2192 1----+-- >0::: ILlf3 2190 1---+--1- 0::: 2188 1---+-1-- 2186 I------".~- 2184 ......._...r....._ o FLOOD DISCHA SURFAC 360 ,.....--~--r------;'--,..---.,.....-.....,--......, 35 --+---+----.-(\--..........pr--=OUTFLOW +---1 IJ I /"-'OUTFLOW"...JII MATCH ING ~- 'i INFLOW I .......MAIN SPILLWAY4"'"OPERATING -+----+--1•r-'POWERHOUSE AND OUTLET !FACILITIES AT FULL CAPACITY ~RHOUSE AND OUTLET FACILITIES ATING (MATCHiNG FLOW) I I I I I 10 15 20 25 30 35 TIME (DAYS) I:10,000 YEAR FLOOD 320 I---+---+---At--..---+----+--t----Ir-'j.~/OUTFLOW2801---+--~-f---t,...."------.______-_,_-__+_---1 INFLOW __~r~240 I-----,----~rl--t__\_\__\_--+_-__+_-__l~.:\'A-g 200 I----+-----"lf---*II--+--V~_+I-'t__+_-__+_-__lI'\,w ,.EMERGENCY ~\~160 1--+--/1---:'-/1---SPILLWAY --+-\"I<or-"--+----1 ~"OPERATING " ~120 I----+--+-f!--I---+----+---+-~~--Ir___-.--.-- o i ' !80 1----+--Jr~-+-__=_=_=_::_::_:_.I.::-=-~-:-'-:-:-_:_:__-+-___1I--___II:MAIN SPILLWAY II/OPERATING 40 !M"POWERHOUSE AND OUTLET -IJ--~,//FACILITIES AT FULL CAPACITY WI6--0UTLET FACILITIES OPERATINGo o 5 10 15 20 25 30 TIME (DAYS) PROBABLE MAXIMUM FLOOD 2202 r----r---"""T""-~--~-....,....-~--_, 353025 2200 I-------I__+l-If'-/_--+-~___=""..,.........,.-__+---+-_____t~'EMERGENCY~~ ~2198 I---+---ft--SPILLWAY _-+1-+-'_+--_---1~I OPERATING \ 5 2196 1---+----If-+----I---f---+-\--\-+-----1 6 , ->'lJ.J 2194 1---+---+-+----+---t---+---------+-----1 ....J I \w , 0::2192 1---+---+--+----+---t---+--------:-'---+-----1~~\ ~0 ~,~219 1---+-f--~\-M-A-IN2...-SP-IL-L-Wl-A-Y-,O-U...l-T-L-ET----I...I----1 FACILITIES AND POWERHOUSE 2188 I--_+---I_--+--_O_P_ER-,-A_T_I_N_Gr----,-------,------I 1 I 2186 I---t-+j+-~OUTLET FACILITIES AT --+------1 ~FULL CAPACITY 2184 10....-----'-_......11_---:....1 __.l.....-I----L.._----L...._.-J, o 5 10 15 ,20 TIME (DAYS) PROBABLE MAXIMUM FLOOD fERHOUSE AND OUTLET FACILITIES iRATING (MATCHING INFLOW) 10 15 20 25 30 35 TIME (PAYS) I:10,000 YEAR FLOOD /~II~NFLOW EXCEEDING _ /\ OUTFLOW CAPACITY MAIN SPILLWAY OPERATING (MATCHING INFLOW) r MAX WSEL 2193.3 WATANA ~RGES AND RESERVOIR CE ELEVATIONS FIGURE E.2.154 J )1 -1 ]--1 1 ).1 .1 ))J ~-l --J 100 90 80 70 60 ..50en lL.uo 40 oo ~30 a: <t :I: Uen 15 20 - r / // ~""'" 10 1.02 1.11 1.25 2 5 10 20 50 100 RECURRENCE INTERVAL (YEARS) NOTE:BASED ON WEEKLY RESERVOIR SIMULATIONS. GOLD CREEK ANNUAL FLOOD FREQUENCY CURVE WATANA OPERATION FIGURE E.2.155 I I II I I II I I II I I II I I II I I r-LEGEND: GOLD CREEK PRE -PROJECT FLOW........WATANA OUTFLOWf------GOLD CREEK POST-PROJECT FLOW r- r-~ r- r- -~ - -1 1\ 1\•\~\-I \~ \ J \1\1\ ~J ""'-I \ ~"~\-,":-,.'T":""'.-r"l1\ \I L..w-..~.--r-r ,..--.~~................, 'r"r.~~.--r"?..........,.....~....." _....-,.,...r"'P .........._'\...~~:-:-:::-!\ -..... I I I I III I I 88 80 72 64 56 In LLu 048oo UJ (!) 0::« ~40en r:::l 32 24 16 8 o JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1964 WATANA AND SIMULATION U . ..............: DECEMBER r'~ ~."",-.JI---, ~.., NOVEMBEROCTOBERAUGUST r",,.""..,....../\/ ,..."'"'..,'V,..."."."...'...'".'"...'" JULY MONTH I GOLD CREEK FLOW SING 1995 DEMAND FIGURE E.2.156 I I 'I I I I I I JI I I II I I I I I I -LEGEND: GOLD CREEK PRE-PROJECT FLOW--.......•WATANA OUTFLOW----GOLD CREEK POST-PROJECT FLOW - - - - - ~i- '"I-rJ\A ~ ~ r- ~A, II..I' ::-:.":\i V I \/\.1\j'v'\,"1 '::-.-::.,:,:.~\I\" I-\/"'.••..~J I'::.:-:.,:,:.~.':":.-:'.:":.':"),f.....•••••·••••••••••..•........1'::.";".~~~.-:-.~':":~.-:-:~~--!J i"OO\_.oJ i-......... I I IIIIIIIIIIIII I I 88 80 72 64 56 32 24 16 8 o JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1967 WATANA AN SIMULATION U~ II ,I I I I I I I I I r I I I ,I I ,I I I r I - - - - - - ~- ~\i u~,,\~1 - ..... W \J i\~iJ'J '-.jE -J'I ! ~J ~,,_-..J i j\"Jr·..·: J'r ..~I \I ..p.'::.~ I \~",,/"\./ .;~r::----------_..J{......J ..................................- '"I \.,J I ".~.....I1\J \i ..--It'\I .........~......_--..,yvy \.....,1 ~.......~..........~;:~ ............_....-............:- I I I I I I I I I I I I I I I I I I I I I 1 I I I MONTH JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER 10 GOLD CREEK FLOW 31NG 1995 DEMAND FIGURE E.2.157 ..... 88 80 72 64 56 (Jl "-U o 48 oo w (!) 0: <CG 40 lI) a 32 24 16 8 o I ,,)I ,r I I II I ,I)I 1 I I 1 I -LEGEND: GOLD CREEK PRE-PROJECT FLOW ...........WATANA OUTFLOW ~- - -GOLD CREEK POST-PROJECT FLOW ~ f-- f-- - ~ - r- - -A~I V .....,•\,.JV - A ~.I\A......f\/\...,...j------7,'~---------~--.....,.....-------.-----~-----.....,-..................-.....................-. I I .1 I I I II r~ JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE·. TIME SCALE IS IN I NCREMENTS OF 10 DAYS. 1970 WATANA ANC SIMULATION W ~!... .......................... MONTH GOLD CREEK FLOW liNG 1995 DEMAND SEPTEMBER OCTOBER NOVEMBER DECEMBER FIGURE E.2.158 ~ ""~~'... ................. ~,r-- "- j -- ............""""'- 10 2 0 10 20 30 ~ 0/0 OF TIME DISCHA 10 2 0 10 20 30 ~ %OF TIME DlSCHAI 10 5 8 6 4 10 2 0 10 20 30 oli %OF TIME DISCHAI 10 5 8 6 4 2 10 4 (/)8 aa.6 ~4 I&J ~ It:«2:::t: 0(/) C 10 3 8 6 4 2 2 10 4 8 (/) 6aa. ~4I&J ~ It:«2:::t: 0 (/) 25 10 3 8 6 4 2 -----~.--I-- .....----r----r---.r-.... D~CEr'B~R -----------r---... ~~......-----r--- .JU1LY 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED F~BR~AI~Y 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 2 10 4 U;8 aa.6~ 4I&J ~ It:«2:::t: 0 (/) 25 10 3 8 6 4 2 10 5 10 5 8 8 6 6 4 4 2 2 10 4 10 4 8 -....8 (/)6 -(/)6aa.aa. ~4 ~4 l&J l&J ~~It:It: c(2 ~2:::t: 0 0 (/)~(/) C 10 3 ---.....C 10 3 8 8 6 6 4 4 2 2 4 2 10 4 (/)8 aa.6,0 4 I&J ~ It:«2:::t: 0 (/) C 10 3 8 6 4 2 --- ~ ~~-r-...---r-............ N~VE~B~R "'-.---~"r---...r-.........,r-......... '..-- .IU 1 NE """"'-.--------......... "~N~A~Y 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 l&J ~It: ~2 ~ C 10 3 8 6 4 2 10 4 (/)8u..6~ l&J 4 ~ It: c(2:::t: 0 (/) C 10 3 8 6 4 2 lOS 8 6 4 2 104 U;8 aa.60 l&J 4 ~ It: c(2:::r: 0 (/) C 103 8 6 4 2 ~r--.Ir--_ -. ""-r---'\ \ ..~y -1'00....--.-1--- ~--r--. """"" OCTOBE R I I PRE-PROJECT FLOWS WATANA OPERATION FLOWS 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 8en6~ 0 4 LLI <!la:: c(2~ 0en 0 10 3 8 6 4 2 10 5 8 6 4 2 104 8en6~ ~ LLI 4 <!la:: c(2~ 0en 0 10 3 8 6 4 2 LEGEND: , '--..--~ .......... '" SEPTI~"BER I I I ----- '--I--"--I--- ....... ~ AP~I~ MONTHLY AND ANNUAL FLOW DURATION CURVES SUSITNA RIVER AT WATANA 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 en 8 ~6~ LLI 4 <!la:: c(2~ 0en 0 10 3 8 6 4 2 10 5 8 6 4 2 10 4 en 8 ~6 ~4LLI <!la:: c(2~ 0en 0 10 3 8 6 4 2 NOTE: I.CURVES BASED UPON AVERAGE MONTHLY FLOWS FOR 32 YEARS OF SYNTHESIZED RECORDS DERIVED FROM HISTORICAL AND FILLED DATA. 00 ED o DED '- r-_ r---. ~A~CHI 40 50 60 70 80 90 10 ARGE EQUALLED OR EXCEE I I -r---, r-....~ "' ,UI1Usr 40 50 60 70 80 90 I ARGE EQUALLED OR EXCEED -!--\.-.\'-\ i\. "\~I""-- "\. tN~UA~ 40 50 60 70 80 90 100 ARGE EQUALLED OR EXCEEDED FIGURE E.2.159 \ \.',- \.,".....-- ............ '... .........i'-- '. 1', ~.... - "-"-~ 10 2 0 10 20 ~ %OF TIME DIS' 10 5 8 6 4 10 2 0 10 20~ %OF TIME DIS 10 2 0 ,10 20 ~ %OF TIME DISI 10 5 8 6 4 2 10 4 U)8 IL 6 ~4 IIJ (!) D:: ~2:I: 0en 0 10 3 8 6 4 2 2 10 4 8en6IL ~4IIJ (!) D:: ~2:I: 0en 0 10 3 8 6 4 2 10 5 8 6 4 2 10 4 8en6IL ~4 IIJ (!) D:: ~2 0en 0 10 3 8 6 4 2 -----_.---.. ""----~---...... .............. D~CE~8'R ~i'oo..... ~r--1"---1- --.,"'.....- dUllY I-- "'"........."-100-.------ F~8R~A'Y 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TI ME DISCHARGE EQUALLED OR EXCEEDED 2 10 5 8 6 4 2 10 4 U)8 IL 60 4IIJ (!) D:: ~2 0en 0 103 8 6 4 2 en IL 3 IIJ (!) D:: ~2oeno 10 3 8 6 4 2 10 4 en 8 IL 6 0 4 IIJ (!) D:: ~2 0en 0 10 3 8 6 4 2 "-..........100-. "r--r--~-~-1\'....------- JUINE ~--- .........'-----r--r--.................... "" N~VE~8'R ~--....-- ......... "---r--~ ...... J~N~A~Y 2 2 10 2 0 10 20 30 40 50 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 eo 60 70 80 90 100 '"·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 5 8 6 4 2 104 en 8 IL 63 IIJ 4 (!) D::~2:I: 0 U) 0 10 3 8 6 4 2 10e 8 6 4 2 104 U)8 IL 60 IIJ 4 (!) D:: ~2:I: 0en 0 103 8 6 4 2 IIJ ~ 1 2 ~o 103 8 6 4 ........ "'-~---.~---------- '\. " I MfY ----....--------....-....i"'--... OCTC )BER I I PRE-PROJECT FLOWS WATANA OPERATION FLOWS 2 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 .-8en6IL 0 4 ILl (!)a: c(2~ 0en i5 10 3 8 6 4 2 10 5 8 6 4 2 10 4 en 8 IL 6~ ILl 4 (!)a: c(2~ 0en i5 10 3 8 6 4 2 LEGEND: ------- "'--~--~r--r------- AP~IL ~-....I'-.... 1'_t--r--..-....,., r-.. ", I I SEIPTI~M8ER I I MONTHLY AND ANNUAL FLOW DURATION CURVES SUSITNA RIVER AT GOLD CREEK 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 en 8 IL 6~ 1LI 4 (!)a: c(2~ 0en i5 10 3 8 6 4 2 10 5 8 6 4 2 104 en 8 IL 6 0 41LI (!)a: c(2~ 0en i5 10 3 8 6 4 2 NOTE: l.CURVES BASED UPON AVERAGE MONTHLY FLOWS FOR 32 YEARS OF SYNTHESIZED RECORDS DERIVED FROM HISTORICAL DATA. 00 ED 00 ED --- -I---1--...-- IMA~CHI 30 40 50 60 70 80 90 I SCHARGE EQUALLED OR EXCEED ....1-, -~ '...--1-0 _ ~ ,UGjUST 30 40 50 60 70 80 90 I ~CHARGE EQUALLED OR EXCEED "l\. -1---'\. '\. ~ "-"-r---...i'-... I ~N~UA~ 30 40 50 60 70 80 90 100 ~CHARGE EQUALLED OR EXCEEDED [FIGURE E.2.160 1""-...- ~......r-- ~ '.................I".. 1'-'.... ~-... 10 3 0 10 20 ~ %OF TIME DISI 10 6 8 6 4 3 10 0 10 20 3 %OF TIME DISI 3 10 -0 10 20 3 %OF TIME DIS( 10 6 8 6 4 2 10 5 en 8 &L 6 ~4 IIJ C) It:4(2::E: 0 U) 0 10 4 8 6 4 2 2 10 ~ 8 U) 6&L ~4 IIJ C) It:«2::E: 0 U) is 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 U)6&L ~4 IIJ C) It:~2 0 U) is 10 4 8 6 4 2 --.1'--1'-...1"--I-- "'"'" """-......................-lo000o.... D~CEIMB~R .......~-100---- .........~-~i'oo.. F~BR~A~Y ---~..-r-_"'"- dUllY 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 2 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED U) &L ~ IIJ C) It:~2o U) is 10 4 8 6 4 2 10 6 8 6 4 2 10 5 en 8 LL 6~ 4IIJ C) It:«2::E: 0 U) is 10 4 8 6 4 2 4 2 10 5 U)8 &L 6 0 4 IIJ C)a::«2::E: 0 U) is 10 . 8 6 4 2 -~...-.....-I""-...i""""o-o.-....: JU1NE ~I-•--~-~------ --....-.....~--................. JANUARY I i I ~,.....---------~-............ N~VE~B~R 2 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 IIJ C) It: ~2 ~o 10 4 8 6 4 10 6 8 6 4 2 10 5 U)8 LL 6~ IIJ 4 C) It: 4(2::E: 0 U) 0 10 4 8 6 4 2 10 6 8 I 4 2 lOS en 8 &L 60 IIJ 4 C) It: 4(2::E: 0 U) 0 10 4 . 8 6 4 2 10 6 10 6 8 8 6 6 4 4 2 2 10 5 10 5 en 8 .....8 6 U)6II..II.. 0 0 """.....4 .....4I&J I&J .............. (!)(!)--~a::a::~-~«2 «2:::t::::t:~0 0U)U)~2i 10 4 ~...1'--2i 10 4---88 6 6 I 4 "'-4!r--.I-- r-----..... 2 ...........2 IMA~CHI 10 3 AP~IL 10 3 M~Y 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 SCHARGE EQUALLED OR EXCEEDED lifo OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 10 6 8 8 6 6 4 4 2 2 10 5 10 5.....8 .....8 r--.en U) II..6 ...........II..6--I"'---ii_---.£~........."'-£-...I&J 4 -r--:----...4I&J(!)-r--=r:::::(!)a::~--.a::««:::t:2 ~:::t:2 --..:F::....:::0 0 ~--en U)10._-2i 2i ----10 4 10 4 -8 8 6 6 4 4 2 2 ,U8IUST SE1PTI ~M~ER OCTC)B~R 10 3 10 3 I I _ 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 $CHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED NOTES LEGEND I.CURVES BASED UPON AVERAGE MONTHLY PRE -PROJECT FLOWS FLOWS FOR 32 YEARS OF SYNTHESIZED ---WATANA OPERATION FLOWSRECORDSDERIVEDFROMHISTORICAL AND FILED DATA. '~ 1\'."....""-- """- '"MONTHLY AND ANNUAL"'""'---FLOW DURATION CURVES ~N~UA~SUSITNA RIVER AT SUNSHINE 0405060708090 100 ~CHARGE EQUALLED OR EXCEEDED FIGURE E.2.161 ~~ .... --1--- :::::--~t:-o 3 10 0 10 20 ': 0/0 OF TIME DIS 10 3 0 10 20 ~ %OF TIME DIS 3 10 ··0'10 20 ~ %OF TIME DIS' 10 6 8 6 4 2 10 5 en 8 I&-6 ~4 UJ C) II: c(2~ 0 (I) C 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 (I) 6u.. ~4LLI C) II: c(2~ 0 (I) C 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 (I)6I&- ~4 UJ C) II: ~2 0 (I) C 10 4 8 6 4 2 .......~---....-......--"1----~....~ -""- D~CEIMB'R -.....0 -.-.1---'--I-----::::r--:::::e:-...... dUlLY ----~-----'"-- -- F~BR~A~Y 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 2 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 10 5 en 8 I&-60 UJ 4 C) II: c(2~ 0en C 10 4 8 6 4 2 (I) I&- ~ UJ C) II: ~2o (I) C 10 4 8 6 4 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 5 en 8 I&-6 ·0 4 LLI C) II: c(2~ 0 (I) C 10 4 8 6 4 2 ~.-..~..- ...........--..-I--1---r---....r----......--- ~VE~8'R ~:::-:::-::t:::r:-r--- ~~ dU1NE 1'-......----r-1--.1---~--..........i'ooo..--- d~N~A~Y 3 10 0 10 20 30 40 50 60 70 80 90 100 '"OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 3 10 0 10 20 30 40 !SO 60 70 80 90 100 '".OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 2 LLI C) II: ~2 ~ C 10 4 8 6 4 2 10 5 (I)8 I&-6~ UJ 4 C) II: c(2~ 0 (I) C 10 4 8 6 4 2 .....10 5 (I)8e6 4 10 6 8 6 4 2 10 5 en 8 I&-60 UJ 4 C) II: c(2~ 0 (I) C 10 4 8 6 4 2 10 6 10 6 8 8 6 6 4 4 2 2 10 5 10 5 en 8 ....8 -6 U'J 6 -LL LL -.........~0 ~-r'\....4 ~4 "\IA.I IA.I (!)(!)0:::0:::c(2 c(2 r1 ;%:%: ~--0 --..0---en ~-r-l------en I---2i 1--.-2i---10 4 1'00...~10 4 8 -8 6 6r--_-I--. 4 4 2 2 IMA~CHI 10 3 AP~IL . 10 3 M~Y 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 SCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 10 6 8 8 6 6 4 ..4 2 2 1'-1---10 5 r--.-_10 5 en 8 ....8r-_.enLL6-1""00...LL 6 ......~---I'....~.......~ IA.I 4 -4 --..;;::~IA.I .._- (!)(!)-I""-•0:::0:::---..---..1"-....c(c("'---%:2 %:2 ---~0 0enen 2i 10 4 is 10 4 8 8 6 6 4 4 2 2 ,U8 t UST 10 3 SE1PTI t"~ER 10 3 °ICT«)B~R 130 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100~CHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED - NOTES:LEGEND:i I.CURVES BASED UPON AVERAGE MONTHLY PRE -PROJECT FLOWS FLOWS FOR 32 YEARS OF SYNTHESIZED ---WATANA OPERATION FLOWSRECORDSDERIVEDFROMHISTORICAL AND FILED DATA. ;1'. "-'..:'- i"\..."1\'......... i ......--MONTHLY AND ANNUAL ."-FLOW DURATION CURVES....... SUSITNA RIVER AT SUSITNA STATION 'N~UA~ o 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED FIGURE E.2.162 100102030405060708090 PERCENT OF TIME DISCHARGE EQUALLED OR EXCEEDED \ "'"• '"\, '.....~........-\,1""'---- \-............----"""""-,-i'--............~""""""-........ \--~, \ \ '"~~ \ \ \06 0.4o 40 2 80 0.8 10 20 60 ~u 8 ooo :::6 lLl (!)a::<t ~ ~4 Ci f'i""l I - LEGEND: -PRE -PROJ ECT ----WATANA OPERATION -1995 DEMAND NOTE:FLOW DURATION CURVES ARE BASED ON MEAN WEEKLY DISCHARGE. ANNUAL FLOW DURATION CURVE SUSITNA RIVER AT GOLD CREEK PRE -PROJECT AND WATANA OPERATION FIGURE E.2.163 10846 WATER TEMPERATURE (OC) 2 ,~V- 12/12/80 9/29/80 /131/80 J \\'/, \\V4/30/8~ ~:-----\r-- 60 80 o 20 o (f)a:: LLJ... LLJ ~ -40 :I:...a.. LLJo .- - WATER TEMPERATURE PROFILES BRADLEY LAKE,ALASKA SOURCE:CORPS OF ENGINEERS 1982 FIGURE E.2.164 1 -I 1 1 i UJ ~ :a~ i UJ ~ CDc:r ~ % (!) LLi % 60 :~ 50 •,x .J ----~-_..---c?J ~.-x X l\:------,."._..--C:J,..x ----""0 0 /""",0r:x .;0,X "",""'"0(0x/ 0 ~ 40 ~'11:'\r x p (X 0 / •1:o " I "",. 0 "/' 30'/ !' X e::/ X ) I X 0/ X I 20·)(0f X I X 0 1 ):;I LEGEND:~ )0 I ---JUNE I -PREDICTED 10 I X JUNE 18 -MEASURED ~I -0 JUNE 18-PREDICTED •X I 0 JULY 14-MEASURED I X I - - - J ULY 14-PREDICTED I 1982 DATA I~I I0 4 5 6 7 8 9 TEMPERATURE (Oe) 10 II 12 13 14 EKLUTNA LAKE OBSERVED AND PREDICTED TEMPERATURE PROFILES JUNE-JULY FIGURE E.2.165 ~~~']J ._)) 141312II109 TEMPERATURE (Oc) 8765 <:1 x I V 1 X fD x ..J ~x I x ~-I10X1''''' ",.,.....-- I ~ I ~-,/~ l.:)~vL"J:._-1-~ I ~/~-~B I .X,~8/ , V l":'1 I J j .~~' ~/I ~I r-1 -I......\:J I I LEGEND: El I 8 AUGUST II -MEASURED •I ---AUGUST 11-PREDICTED8rJ0IXSEPTEMBER9 -MEASURED)~:I SEPTEMBER 9 -PREDICTED, 0 SEPTEMBER 21 -MEASUREDI- - -SEPTEMBER 21 -PREDICTED 8<0 I 1982 DATA."---J I. m /- )~ I ' 0x1 • I :I 50 0 4 10 20 60 ~ Ui I- Ui !40 ~o I- .~ I.Ll>g <t 30 l- X (!) W:r: EKLUTNA LAKE OBSERVED AND PREDICTED TEMPERATURE PROFILES AUG -SEP FIGURE E.2.166 1 1 10 - 98 GJ GJ fa GJ GJ 7 I 6 X 5 TEMPERATURE (OC) 43 o 200 601--_.__~__~+.I <::.p -----X' o ~--~I o ~I x · I I 50 1 I I,...I • -I I I I I o I en 0 1 X I'~0 I w 0 I ·~40 G I I I~01 X I 5 ~I~~. >Io~~30 i I~I x •1°I~I I~I . :I:I · !x I 201 I I 1 I ",I .LEGEND' I )G OCTOBERI4-MEASURED I X,GJ ---OCTOBER 14-PREDICTED 10 I I I I I /'X NOVEMBER 4 -MEASURED I I I (NOVEMBER 4-PREDICTED I I'0 JANUARY 31-MEASURED I X GJ - - -DECEMBER 31-PREDICTED I i 1982 DATA L ___~~~~l EKLUTNA LAKE OBSERVED AND PREDICTED TEMPERATURE PROFILES OCT -DEC FIGURE E.2.167 SOURCE:BC HYDRO 1982 UNPUBLISHED DATA 4 FIGURE E.2 .168 32 TEMPERATURE (0 C) o ""\'...,,...~, '\ \~ "t~, ~PRILI4 ?\~:\,\ \\~\\ ~..\ '~\APRIL 15 \\'\ \\.,,"\\\ """'r-,\\\ \" \"\\\ \"'"\\\ \\,.\APRIL 14 \ \ \\,, \\,, \\ \\ "\\\, \'.\\ \ \\\ \ LEGEND: -~SITE I FOREBAY --SITE 2 UPSTREAM OF FOREBAY ------SITE 3 FINDLAY FORKS(APPROXIMATELY 60 MILES UPSTREAM) LAKE WILLISTON TEMPERATURE PROFILES APRIL 14-15,1982 150 160 140 130 120 110 100 90 t- W W ~ I..L ~80 t-o.. W 0 70 60 50 40 30 20 10 0 NORMAL MAXIMUM OPERATING RESERVOIR LEVEL (EL.2185FT.) EL.2151 FT. El.2114 FT.--- El.2077 FT....;..._ MINIMUM OPERATING RESERVOIR lEVEL {EL.2065FT.) EL.2040 FT.--- 20 FT.(TYPICAL) WATANA MULTILEVEL INTAKE FIGURE E.2.169 14 12 4 10 u 0 ilJ 80:: ::l If0- e:(I0::~ilJ D...":::!:,... ilJ (f0- G 2 a II 21 II 21 JUNE JULY NOTES: I)TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2)BASED ON 1982 DATA EKL RESERVOIR TEM JU '\I 1 ~ ""~~lJ'vv ,fvJ r"jJV 11/:\'1 t\0rt', 1\~J L~--..~"\.------r...._I \--I --...._1 \.__~ \I--J -.---L-...1-,--SIMULATED OUTFLOW-SIMULATION RESTARTED --TEMPERATURE , I I I 31 MONTH 9 AUGUST 19 29 8 18 SEPTEMBER 28 8 JTNA LAKE )ERATURE SIMULATION N TO SEP FIGURE E.2.170 14 12 10 u ~8 wa: ::> I- <[ a:w 0- ::Ii:w I-6 4 2 o /""RECORDED OUTFLOW TEMPERATURE 1-..--./ 1---,~.............. '~V,\ ',-vv'"" ~........"'.. SIMULATED- OUTFLOW TEMPERATUI I 8 18 OCTOBER 28 7 NO NOTES: I)TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2)BASED ON 1982 DATA. EKLUT RESERVOIR TEMPE OCT \ \A.. ---~Y __1 C ~--A pAl---7 RE , I I 17 27 VEM86R MONTH NA LAKE HATURE SIMULATION TO DEC 7 17 DECEMBER 27 FIGURE E.2.171 - r~ - - 2200 2150 2100 2050 ~2000 ~::;; l&J ...J l&J 1950 1900 1850 1800 17~0 , , _I I I I I I _J , I ( V--1 / I / ,,/ L~....~Io' ~-~::;i"":i'" k--:::;;'- ~- I, II I LEGEND: JUNE 1,1981 ---JULY 1,1981 ---AUGUST',1981 II • - 2 3 NOTE:TEMPERATURE PROFILES SIMULATED USING 1981 DATA. 4 5 6 7 8 WATER TEMPERATURE (Oe) 9 10 II 12 WATANA RESERVOIR TEMPERATURE PROFILES JUNE TO AUGUST FIGURE E.2.172 '"'"' - ..... ..... 2200 2150 2100 2050 i='w l.LJ .!=. ~2000 ti:> l.LJ ..J l.LJ 1950 1900 1850 1800 1750 ,...u \I I, '"I......I '..:"!'I.. I I ~//' ~~ ~,~ /~ I , ~Vi" ~ \~-'l~ ~~~~ I ,I\~f/ R =1 I I I :1 ·1 LEGEND: II ----SEPTEMBER 1,1981_ II OCTOBER 1,1981 .I ---NOVEMBER I,1981 :1 ---DECEMBER I,1981 II _•••-DECEMBER31,1981_ I I ~ 2 3 NOTE:TEMPERATURE PROFILES SIMULATED USING 1981 DATA. 4 5 6 7 8 WATER TEMPERATURE (OCl 9 10 II 12 WATANA RESERVOIR TEMPERATURE PROFILES SEPTEMBER TO DECEMBER FIGURE E.2.173 14 i___':'1 lNFLOW- /".-./',r"'_(' ,'--10--,, J,,' , I I ,,I ~'\,.),,\, I ,r \I ~L'~_I-_J ~ f"1:\-.OUTFLOW V /"'\\ I ,:'I6f,I,I I ,I ,I I V II 12 ~"'\,/\ 10 I V' 8IJJa:: ::::> I- 0([a:: IJJa.. ~ IJJ I- 4 2 o 10 20 30 9 19 JUNE JULY NOTES: I)TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2)BASED ON 198/DATA,WATANA OPERATION 3)RUN W4020j WITH OUTFLOW TEMPERATURE FOLLOWING INFLOW TEMPERATURE. 4)JULY INFLOW TEMPERATURES ESTIMATED WATANA RESERVOIR INFLO JUN ('-..._A A ....,........... , I ......'",,, \I, I , ~,JL._ 29 MONTH 8 AUGUST 18 28 7 17 SEPTEMBER 27 7 W AND OUTFLOW TEMPERATURES TO SEP FIGURE E.2.174 o I """'......... ....-.-----.........~':...TFL/ .................................. ....,.....,......... ..., ,,'" r \'NFL7 ~-r-""".-/~- 14 12 10 u 8 0 W 0::: ::::l f- <:{ 0::: Wa. :::::6w f- ,..'- 4 2 7 17 OCTOBER 27 6 NO NOTES: I)TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2)BASED ON 1981 DATA,WATANA OPERATION 3)RUN W4020;WITH OUTFLOW TEMPEF1ATURE FOLLOWING INFLOW TEMPERATURE. WATANA RESERVOIR INFLO~ OCT 1 ------------~----,~-~-------------------------- I •'\ \ ""--"'\ \.-..----------------I--------- , --I I 6 16 DECEMBER 26 5 ,AND OUTFLOW TEMPERATURES ·0 DEC FIGURE E.2.175 12.5 12.0 11.5 11.0 --------__JUL 31-----------~-...........-----~-- 10.5 (J 0 wa: ::> !;;: 10.0a:wa. ~w I- 9.5 9.0 8.5 AUG 31 8.0 AUG 15 ----~._- 7.5 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 NOTE: I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA. 2.WATANA TEMPERATURE AND DISCHARGE FROM DYRESM MODEL.(RUN WA4020l . RIVER MILE WATANA DOWNSTREAM TEMPI WATANA DISCHARGE (CFSl: JUN 15 4410 JUN 304210 JUL 15 4130 JUL 31 3970 AUG 15 6250 AUG 31 21000 (RELEASE) ----------'---~ ...;::a_-..________ -~-----~~---- 149.00 155.00 161.00 167.00 173.00 179.00 185.00 OPERATION: ERATURES -JUN TO AUG FIGURE E.2 .176 9.0 B.5 B.O 7.5 7.0 u 0 w 6.5a:: ::l !«a::w ll. ::::i!:w 6.0f- 5.5 5.0 4.5 4.0 -------/---------- 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143 R NOTE: l.MODEL ASSUMES 19BI METEOROLOGICAL DATA RECORDED AT WATANA. 2.WATANA TEMPERATURES AND DISCHARGE FROM DYRESM MODEL.(RUN WA4020) WATANA DOWNSTREAM WATANA DISCHARGE ICFS); SEP 15 12200 (RELEASE) SEP 30 9460 ,00 149.00 155.00 161.00 167.00 173.00 179.00 185.00 IVER MILE OPERATION TEM PERATURES -SEP FIGURE E.2.177 4.0 3.5 3.0 2.5 0e.. ILl 0:: ::l ~2.00:: ILl IL ::Ii ILl ~ 1.5 1.0 0.5 o 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTES: I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA. 2.WATANA TEMPERATURES AND DISCHARGE FROM DYRESM MODEL.(RUN WA4020) WATAN, DOWNSTREAM TEMF WATANA DISCHARGE (CFS); OCT 15 6110 OCT 31 5820 NOV 15 6580 NOV 31 10070 DEC 15 10540 DEC 31 12500 149.00 155.00 161.00 167.00 173.00 179.00 185.00 A OPERATION = ~ERATURES -OCT TO DEC FIGURE E.2.178 14 12 /\I , \I 10 '~, """ u 0 -.'-w 80:: ~ l- e:( 0:: W D.. :::Ew I- '""",",0::6w ~ ~ ~......... 4 2 o 10 JUNE 20 30 10 JULY 20 NOTES: I.TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2.OBSERVED DATA FOR SUSITNA RIVER ABOVE FOURTH OF JULY CREEK (RM 131.3)ADF8G 1982. 3.PREDICTED WATER TEMPERATURES (RM 130.5) DURING WATANA OPERATION USING 1981 DATA. 4.TEMPERATURES REPORTED ARE MEAN DAILY VALUES. COMPARISON OF 1981 OB~ NEAR SHERMAN AND ~8 WATAN 30 MONTH ( 1 ~Ir,I \, " I I I 9 19 AUGUST 29 OBSERVED 8 ,1'--. I \~ \ \1\~\, 18 SEPTEMBER ./\( \ I, 28 SERVED WATER TEMPERATURES I TEMPERATURE SIMULATION OF A OPERATION FIGURE E.2.179 4.0 3.5 3.0 2.5 u 0 wa::: ='I-2.0<fa:::wa.. :::ii:w I- 1.5 1.0 05 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.QO RIVER MILE NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT WATANA.WATAr DOWNSTREAM TEM OUTFLOW WATANA DISCHARGE (CFS): OCT.6770 NOV.8670 DEC.10300 JAN.9400 149.00 155.00 161.00 167.00 173.00 179.00 185.00 ~A OPERATION: IPERATURES -OCT TO JAN TEMPERATURE 4 0 C F[GURE E.2 .[FlO 4.0 - 3.5 3.0 ----------~-APR 30 -----------------~-..,.----_.--...-------., APR 15 ---...-..................---_.----",,,,,,,,.----' 2.5o o wcr. :::l I- ~2.0w a. ::::i!:w I- 1.5 1.0 Q5 0.0 95.00 101.00 ./ /" 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT WATANA. WATANA DOWNSTREAM TEMPE OUTFLOW TE -----------.....------ --- WATANA DISCHARGE (CFS!: JAN 9400 FEB 8690 MAR 8100 APR 7480 i49.00 155.00 161.00 167.00 173.00 179.00 185.00 OPERATION: :RATURES -JAN TO APR MPERATURE 4 0 C FIGURE E.2.181 4.0 3.5 3.0 1.0 05 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT WATANA. WATANA OPERATION:DOWNSTRI OUTFLOW TEMPE WATANA DISCHARGE (CFS): OCT 6770 NOV 8670 DEC 10301 JAN 9400 149.00 155.00 161.00 167.00 173.00 179.00 185.00 EAM TEMPERATURES -OCT TO JAN :RATURE 4 TO 2°C FIGURE E.2.182 4.0 3D 2.5 u 0 W 0::: ::::l !<i:Z.o ----APR 300::: Wa...-::2:APR 15w-----I- 1.5 1.0 0.0 95.00 101.00 107.00 113.00 119.00 125.00 131.00 137.00 143.00 RIVER MILE· NOTE: I.MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT WATANA.WATANA OPERATION:DOWNSTRE OUTFLOW TEMPE WATANA DISCHARGE (CFS); JAN 9400 FEB 8690 MAR 8100 APR 7480 149.00 155.00 161.00 te7.00 173.00 179.00 185.00 AM TEMPERATURES-JAN TO APR :RATURE 4 TO 2°C FIGURE E.2.183 r---------------.-..u,~...----'----------------------_ ICE FROfI NOV 30 I I I I I 120 RIVEI ICE FRONT ICE FRONT NOV 20 NOV 25 I . I I I I I I I I I I I I I I I I 95 100 105 110 115 10~ lJJ IL. II) II) lJJ 2 :ll::: U:c 5 I- NOTE: I.BASED'ON RESERVOIR OUTFLOW TEMPERATURE MODEL(SEE FIGURE E.2.175). 2 THE DASHED HORIZONTAL LINE OVERLYING SOLID LINE INDICATE THE INCREASED ICE THICKNESS AS SIMULATED. FOR THE NEXT ICE FRONT LOCATION. OL------.L..-----...L..-...l...-~-------I...----.........IL-+_ NOTES: I.BASED ON RESERVOIR OUTFLOW TEMPERATU RES STARTING AT 4°C ON NOV.lAND DROPPING TO 2°C BY JAN 15. 2.THE DASHED HORIZONTAL LINE OVERLYING SOLID LINE INDICATE THE INCREASED ICE THICKNESS AS SIMULATED FOR THE NEXT ICE FRONT LOCATION. 95 100 105 110 115 120 RIVER WATANJ SIMULATED ICE THICKNE ISO145140135130 FINAL H ICE FRONT ICE FRONT ICE FRONT DEC 5 DEClO DEC 15 I I IIIII I I I I I I I I I 125 :R MILE :>NT 125 t MILE 130 ICE FRONT JAN 15 I [ I I I 135 140 145 FINAL ICE FRONT FEB 15 I I I I I 150 ~OPERATION ::SS AND ICE FRONT LOCATION FIGURE E.2.184 10 l- W W IJ.. W (f) <l:w DEC 15-0::: (Jz 5 w --, (!I \----, <l:\Il- (f)\~/0:::w> 0::: 0 95 100 105 110 115 NOTES: I.BASED ON RESERVOIR OUTFLOW TEMPERATURES STARTING AT 4°C ON NOV I AND DROPPING TO 2°C BY JAN 15. 2.CHANGE IN STAGE DURING FREEZEUP BASED ON OPEN WATER DISCHARGE OF 9900 CFS. WATANA DISCHARGE (CFS) NOV 8670 DEC 10300 JAN 9400 FEB 8690 10 l- Ww NOV 20IJ.. W (f) ,1<l:w NOV 250::: (J 5~~w /(!I \, j:!\,\--_,,1(f) a::w> a::\ 0 95 100 105 110 115 NOTES: I.BASED ON OUTFLOW TEMPERATURES FROM RESERVOIR TEMPERATURE MODEL. 2.CHANGE IN STAGE DURING FREEZEUP BASED ON OPEN WATER DISCHARGE OF 9900 CFS. WATANA DISCHARGE (CFS) NOV 20-26 8890 NOV 27-3 9410 DEC 4-10 10070 DEC 11-18 10300 WATAN RIVER STAGE INC ~ "1\ I \ JAN 31 ,\/, \DEC 31 yFEBI5IJAN15I\/ ~\I \I , I \I \ ..../\ I \1 \ I ~\...'1 I , L 120 125 130 135 140 145 150 RIVER MILE DEC 10 150145 "I \ 140 I VDECI5 \"rUPSTREAMoJ\.LOCATION OF ."ICE FRONT, ---- 135130125 /\ "/\......../'V~ I\¥'DEC 5 120 RIVER MILE \IA OPERATION ;REASE DUE TO ICE COVER FIGURE E.2.185 J / v / / / II 1/, ) _1./ j,/' 180 165 150 135 u;120 LLu o 0105o w ~90 <l: J: U ~75 0 .-60 45 ,... 30 .-15 0 1.005 2 5 10 2050100 1000 10,000 RECURRENCE INTERVAL (YEARS) .- NOTE: FLOWS ROUTED THROUGH WATANA IMPOUNDMEN~ DEVIL CANYON FLOOD FREQUENCY CURVE FIGURE E.2.186 / / ,/ / .:. 8... <J \oj 9J /'" ( 4-I ....() -~-'~."\ '-'\ -- \' ,\" l ' \ ,',,, 0 I'"IVER S,U./,,/--,. I // " REFERENCE:BASE MAP FROM RaM ,19BI-1"·200'OEVIL CANYON TOPOGRAPHY,RETRACED AT 25'CONTOURS USBR,I960 COE,1978 WCC,I978 BORROW SITE G L EGEN D -----BORROW SITE LIMIT NOTES ENTIRE BORROW SITE LIES WITHIN PROPOSEO DEVIL CANYON RESERVOIR LIMITS. 2.BORROW SITE LIMITS BASED ON FIELD AND AIR PHOTO INTERPRETATION OF BORROW MATERIAL.FINAL UMITS SUBJECT TO RESULTS OF DESIGN INVESTIGATIONS. 3.25 FOOT CONTOUR INTERVAL ADDED FROM SOURCE MAP (REFERENCED)IN BORROW SITE ONLY. 4.PHOTO TAKEN AUGUST,1981. DEVIL CANYON BORROW SITE G SCALE O~IIIIIIIIII~2~0ii;0iiiiiiiiiiii4~90 FEET FIGURE E.2.187 '. I § I ~,, / \\ I ,QQ(!'------I JlI 14 ~'-""I""OOO=--__ ....!!.~ooo __ Zl / / ,, REFERENCE:BASE MAP FROM R 8 M,1981 -1"=200' DEVIL CANYON TOPOGRAPHY. COORDINATES IN FEET,ALASKA STATE PLANE (ZONE 4) C BC l 1.1 ,I I ' \ LOCATION MAP 0~1IIIIIIIII1IIIIIIIII4"'iiiiiiiiiiIiiiiijjS MILES SCALE '0 LEGEND ---SORROW/QUARRY SITE LIMITS NOTES TOPOGRAPHY AND DETAILS SHOWN ON INDIVIDUAL FIGURES . .'-. SJS •, f o SCALE i 1000 2000 FEET DEVIL CANYON ORROW SITE MAP FIGURE E.2.188 d It; \ ---./ 0 0 0 0 0 0 0 0 0 ~0 0 0 0 II)ID ., (\l --etJ ID ID ID W W W W )/-,\Ii II, / N 3,212,000 N ,216,000 N 3,21 ,000 REFERENCE:BASE MAP FROM USGS 1:63,360 ALASKA QUADRANGLE TALKEETNA MOUNTAINS (0-5). COORDINATES IN FEET,ALASKA STATE PLANE (ZONE 4) DE QU 0 0 0 0 N 0 - 0 lD 0 l.&J -<0 \ /~ / SCALE EVIL CANYON ~ARRY SITE K LEGEND ---MATERIAL LIMITS NOTES I.ENTIRE QUARRYPROPOSEDRESER~g~ci~,~OUTSIDE OF 2.MATERIAL S.LIMIT LIMIT SHOWN IS~-igP:~fA~~~~M~~~~:~2~~:~:~OfO LOCATION OF SASME~L:~CK CLIFFS,AND 3.CONTOURS TRAC~EFERENCE BAS~D :ROM ENLARGED NTERVALS.AP,AT 100 I 1 o~~~~~~IO~O;O;'~I 2000 FEET ! FIGURE E.2.189 - 13,600 15,20011,300 DISCHARGE (CFS) 6,800 9,0004,700 90 t----t-I---+----+---I-----_+__~"---------+__----_+__----_+__-~___I 74 t----t-------+-----+------+------+------+-------1 86 t---f--t----------,f---+-----_+__----+__-----+------_+__--___I ',800 2 1300 94 r+-..,......----...,....-----..,..._.----~----...,.......----..,..._.-__+__ ~0 >-uz 82w Q l.L l.L W ~ 78 70 ....l........1....-,,1..-....1....-""""'--__---' 100 200 300 400 PLANT OUTPUT (MW) 500 600 DEVIL CANYON -UNIT EFFICIENCY AND DISCHARGE OPERATING RANGE (AT RATED HEAD) FIGURE E.2.190 2200 MEDIAN YEAR (WY 1966)-- MAX YEAR (WY 1956) \ \ \ "'", \ \ \ \ \ \,, "'"''\ \ \ \"/"/" .....ww ~2130 zo ~~w 2120 --Iw 2110 2100 2090 2140 2080 2170 2180 2070 2150 2160 2190 - OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP WATANA RESERVOIR WATER LEVELS (WATANA AND DEVIL CANYON IN OPERATION) FIGURE E.2.191 1460 1450 I MAX YEAR "/,-MEDIJ\N I (WY 1956)'V~MIN YEAR YEAR' \~(WYI966) ~I (WY 1970) ~1440 ~I ~~z I~1430 I:; w I.J '\lLII420 I I 1410 " 1400 OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP DEVI L CANYON RESERVOIR WATER LEVELS FIGURE E.2.192 40 1-}= I' I' II '"30...II , <J I' I,I §I',II I I lJ , II II "Il I I I'II 'I "II I I I'I'II I'III II I'I ZO I "L Il,.I-.l,~ "JO II '1 '1 ,I I II 1 I I I (.)I'I,I',1.11 I I'I ~I I I I '"/1 I'U 1..11 I 1 I ,I I111II I I 15 I I ,,I ,I I 10 0 ~19~19!12 19:)3 1954 19:):)19:)6 19~7 19~8 19~9 1960 1961 1962 1963 Lt:G£ND: [~.=J INFLOW WAl •OUTFLOW 2200 6 ~ r~ 1 l2000 19~0 19:)1 19~2 19~3 ~195~~6 1957 1958 19:)9 1960 1961 1962 1963 WA1 +±~ - ~J\~~[\\~~iJ\Jt JI ~nl\J\ In n. ¥~lnr lf U ~r L r UUlJt W1 if ~I ".Tr 1;I ul If I 1=1 --r -- l --I T -- - 20 I:) Ul... <J § ~10 ~ (.) '"is o 1950 19!>l 19lI2 1954 195~1956 19~7 1958 1959 1960 1961 1962 1963 NOTE: BASED ON 2010 ENERGY DEMAND DI ,... WATANA AND DEVIL C~ I "" I---+----+---I---I----~--~-----_~I ,I'1: I n"I'I : i I ,I'r:'l 1111 :1 f'j II nIl :I,n I'll I,',~II '",," I 1'"II ,'I,Ii '"IJ , 'I ,I ,jl,',UI 1'1 IU,I,I,' I I'"I , ,~"4 '.;.I II I'"I':'I , ,I,:'I I I,-,-,--Ti ",I',I I'I I I I I , I ,"11 " I ,it I"'I I ,"'11 1 I ',~1,I :r I,I .." , ' I I I L "I I ,~I I I I 'u,I 'I 1 r I I ",':" I 'I h"'"J'~~-i --I "',--1,+---';,+I "'",r 'I 'I "",I I I , ' "I I I I n I Ft.I I r1 n rl I I::~I I I In:I r l i I I n I :1 :1 ~I ::I ',,f'.,I .Il,",J1 i '11 n'..""'l~_-/l-:,n "',Il,,:l,.J-",I l:"1.s'\..I:I l Jl,."I I 1.1\.,:lAo : U ~::IU 1))~!!I~d :l!l~:'lin ::KJ>,:~U !-i~:Ill\.!Y V 'hN 'l,llt..:~~'l~l In I'll ~i IU"h 1-'1.,:~!v',_,~I-~!.t1 ~U lJ-l-J·UL_~LJu,.~~JU\~1'J~l~::lJ [V~lt ,~E II!'t 1964 1965 1966 WATER YEAR 1967 1968 1969 1970 1971 1972 1973 1974 1975 1976 1978 1979 1980 1981 TANA INFLOW AND OUTFLOW 1964 1965 1966 WATER YEAR 1969 1970 1971 '972 1974 1975 1977 1978 1979 1980 1981 TANA RESERVOIR ELEVATION -I f\JJ\1\IJ~~J\n j\..,I~~~\1\~\ 'lJ 1 If ~UI I)uu In nl II 1 In ~IL f'1.I 11 In In n In In nIl u lJ 1fJ ~ += UlJ LJJ )UI [)U IIrV ~ ,-,-I-e--- - '964 '965 1966 WATER YEAR :>EVIL CANYON INFLOW 1967 1969 1970 1971 1972 1973 1974 1976 1978 1979 1980 ~NYON SIMULATED RESERVOIR OPERATION FIGURE E.2.193 196319621961196019591958Ite119l16111115I~11111319!52ltelIlIlIO --\-[-'---1 -I -·_·-T --I I I L--.---- -- ~\AIn I J~J~\1\J\r \IJ\1\\l 1['~f ~r [,1 J1n ~I n n .n l r lJl W ~l ~~ I---,-- C=l -t-I --o 20 Vi 15 IL 0 § ... '"a:10« J: 0 III is II I I - J l I I I _I_~I J I II, 1415 E ~ ~14211 ~ .J... 131& IlIlIO tlIlll 19112 19l13 '954 19~1956 1957 1958 1959 1960 1961 1962 '963 DEli I 1lO1---t---+---t----:---- I I '---tit=I Ii II I, I r I, I, (\InrI : \.JJ GOLD CR 1958 1959 1960 1961195319541911519l16195119521911019111 LEGEND' [~=-~PRE IIlIPOST 0'- 401---I---+---t--+--.---t-----t-- I I i! I i ,I n [l II II I~n "301---+---1--1;-[-,---1----;1----".--,+----+,-+,+--~II --~I--H,,---!I I:'~,,~,,i''I 'I'"I ~r.l I L , "'I I'II."r---!-I--+--I~I'+---t7'-+--..."+t1+----,1 I ft j\,.'1--. ",,,I I I I,~I,L.,r :,~I I ,l, ""n II I,,11'1 ,I I I I ,", 'l,'I .."I~'la~_1 "I I 'e.II I '"I I "20 1--,r,!-l,Ir!----i',-4ot--+,-:;r I I:1 i I"'-t --rt ~:r-r ~:I :: I 'I'I ,J:I "~, "I L '~,, 'I " I I " I I ",, I I ,J'"I 1II I ,"r ''-I ',.-I ----r'-·"~J-r..i I ...111 4:1-1 J1'l.i ni\~/1".]01 (\ri.~~j 1\:I:!\~D'I\m r :~"-~l.~~:uJ ~l~~(,1 U J ~~U ~11J~j 11J IU'~!U'~V' ~~'-~U I I\J U-\J ~)I~J 1962 1963 III ILo o ~ ... '"a:c J:o III is NOTE' 8ASED ON 2010 ENERGY DEMAND WATANA AND DEVIL Cj UUl )n 19811980'-19-7-6""""-19-=77 ~'--::-9=C78-L 19791975 I -- I I I I I 1 n ~,n IJ \n 1\n\ I n ~~n~I~l n ) rJ I l I~~~U l U ~ I 1974197319721971 I I 1f\!\ 111 1 n n n Lv1 ~l~lJ - I 1970 .~--- 1969 I 1968 r\n n [ I i r 1961 1--.---- u tr 1965 1966 WATER YEAR I 1'- 1964 -- DEVIL CANYON OUTFLOW h--~-~--~.----.-. l l u u I~l I l f--L---L----'__-"--~'___...J..:_ 1964 1965 1966 WATER YEAR 1967 1968 1969 1970 1971 t--- 1972 1973 1974 1975 1976 1977 1978 1979 1980 1981 IL CANYON RESERVOIR ELEVATION 1964 1965 1966 WATER YEAR 1967 -1----+-- 1968 , -I- 1975 1976 1977 1978 1979 1980 1981 lEEK PRE-AND POST-PROJECT FLOW NYON SIMULATED RESERVOIR OPERATION FIGURE E.2.194 LEGEND: PRE-PROJECT - - -WATANA!DEVIL CANYON OPERATION lYffi':£J ELEVATION CHANGE EXTRAPOLATED / 1/ / :;. . . : . .../CHANr EL BOTTOM f/ ° 746 756 748 754 SEPJULAUG MINIMUM FLOWS JUNMAYSEPAUGJUL MEAN FLOWS JUNMAY FIGURE E.2.195 10,000 20,000 30,000 LRX 57 RATING CURVE(2) GOLD CREEK DISCHARGE (CFS) WATANA/OEVIL CANYON OPERATION;MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER MILE 142.3 SEP 746 756 748 754 752 i~fflf~~~~¥iH~f:r I~::l:j~~J~JJi nttM:~::lli 752 ~/::::;'~~,'t- o }t~~1"r ,:;~,~:~t t:r~(:{~;M:[~~~g'~~:;t~-:-~-tt:;~~.':tfflltr :::;)~j~~~f-f-1~;;{w 'af~~~~::::Nt~{IT o:i~Ul;w .'~~~'"::':'~~x-~~:WW':1.fi-d'~,.Wr.;:*d lL.lL.i'~Fl !.nfsfi ~-z ;::~.~4~:;:;~:z 0 '+t;4:~'i~titr&l :::.:.:.:.;.:.:.:.:~.::::0 t=750 nill1Tfi .;.:~~:~:.:.i=750 <t ...._;:W-W"""<t>>w '~gf~~w -!-!W W MAY JUN JUL AUG MAXIMUM FLOWS NOTES: I.WATER SURFACE ELEVATION ABOVE RATING CURVE 2.RATING CURVE BASED ON GOLD CREEK DISCHARGE AND OBSERVED 1982 WATER LEVELS (ADF 8 G 1982) / / / / /. ,, ,, :CHANNEL BOTTOM AT EL 605.5 . o tO,ooo 20,000 30,000 LRX 35 RATING CURV~2) GOLD CREEK DISCHARG E (CFS) SEPJUNJULAUG MINIMUM FLOWS MAYSEPJUNJULAUG MEAN FLOWS MAY WATANAIDEVIL CANYON OPERATION:MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER MILE 130.9 SEP 620 ~Hb-Ltilui:!jt::lkl:Fif]I I kmmt'L---I I -l 620 612 ~I I I I I I I I I I I I I I I I -t 612 [f::.~:F]ELEVATION CHANGE EXTRAPOLATED 622 I ,_-.~~.'..~:.~.'",~,~.',~,n :;I Iii iii Iii iii 622 614 l-I I I I I I I I I I I l:¢lt~'V1H I I I -;614 618 r~l"·lfl I i.jJfrfl :;~~g1 .,l 61£f~.t;1E:::-~g8i·.:~:<I.-~'t"l.::-.~~ '.•.•. f:~ttif1t *-~:t>"•.•-~"m.us I-j!f;ifmtfi <ijk·.w I I I,-<i-.:':':W W ;t.;;-:.~$w u..;:::-::::H::;~'t-i:.~'~u.. ~ z I r~l rl z0~.:...~~:0-616 616I-~<I>>w w ..J ..J W W MAY JUN JUL AUG MAXIMUM FLOWS NOTES: I.WATER SURFACE ELEVATION ABOVE RATING CURVE 2.RATING CURVE BASED ON GOLD CREEK DISCHARGE AND OBSERVED 1982 WATER LEVELS(ADFElG 1981). FIGURE E.2.196 554 q:iWli .~.~~~~-./:~illl:554 ~ l-I- ILl ILl ILl ILlu..u.. ~~ z z 0 0 !;t 552 ~552>>W ILl ..J ..J W ILl 10,000 20POO 30,000 LRX 28 RATING CURV~2) GOLD CREEK DISCHARGE (CFS) / / /v .I : : : ~CHiNNEL Bor'l" 558 556 550 548 oSEPJUNJULAUG MINIMUM FLOWS MAYSEPJUNJULAUG MEAN FLOWS ItfnlfJ ELEVATION CHANGE EXTRAPOLATED MAYSEPJUNJULAUG MAXIMUM FLOWS MAY 556 1;;,,,,,,,,,,,,,,,,11 550 558 f i·.·...~·\:,'L:\'.~'..~..!i.·~.·..:::·......:.?~.I 548 I I I I I NOTES: I.WATER SURFACE ELEVATION ABOVE RATING CURVE. 2.RATING CURVE BASED ON GOLD CREEK DISCHARGE AND OBSERVED 1982 WATER LEVELS (ADF aG 1982). WATAf\JAlDEVIL CANYON OPERATION:MONTHLY AVERAGE WATER SURFACE ELEVATIONS AT RIVER MILE 124.4 FIGURE E.2.197 5 o L...-_....L...-_ o 40 1-----+--::::;;; 180 r----r--- 140 I---+__- 160 I---+__- ~120 1---'----- U INFLOW: o OUTFLC :100 1~80 I---+__- <t:ru (f)60 I---+--o 20 I-t------->d--- 35 POWERHOUSE AND .SERVICE SPILLWAY -+---+-----1 OPERATING POWERHOUSE 5 10 15 20 25 30 TIME (DAYS) PROBABLE MAXIMUM FLOOD EMERGENCY SPILLWAY OPENI---'Ne-::-G__-+-_-+-_---+ --j;OWERHOUSE CLOSED..-t -------+-----1 OUTFLOW MATCHING I--_--+-~-+-_~INFLOW ,--_-+-_--+__1 oo 80 40 w ~ tr 160« ::I:u ~120o ~240 I--------+---~f_____-_+_-___+-~<+_-__+-___+ u o g 200 I------.:-f--~-+__J----L.-----+_-_+-__l 280 I----+-----!l+---+_ RESERVOIR INFLOW/ 320 1----+-------f-1H--,;~__+____'~___+-OUT FLOW 5 1450 L...-_...I.-_ o 1460_--- i= !:=.1458 I----+_-zo ~g 14561---+__- W ...J W ~14541--+----o>0:: ~1452 I-----t-- Wa:: 35510 15 20 25 30 TIME (DAYS) PROBABLE MAXI MUM FLOOD I I RESERVOIR ELEVATION MAX WSEL ~EMERGENCY:1465.3~SPILLWAY OPERATING J /1\~----- \POWER HOU;E \! OPERATING 1\---_.-------------_.e-------r ._..-+-_..- I ~ I . ! I 1 i joo 1400 1410 1480 1460 1470 i=u.. -1450zo ~g 1440w...J W ~1430·0> 0:: W ~1420 0:: DE'v FLOOD DISCHA SURFAC 30510152025 TIME (DAYS) RESERVOIR ROUTING 1:50 YEAR FLOOD (SUMMER) I I POWERHOUSE AN D V OUTLET FACILITIES /OPERATING I' 'f\ "-MAX.WSEL=1455 I I I/INFLOW=OUTFLOW V N I-.... L/~POWERHOUSE AND OUTLET FACILITIES OPERATING 1460 o o w ~20 <{:cu ~10o 50 ~40 u og 30 .....u.-1458z Q I-: :;1456 w ...J W !?::1454 ~ 0:: ~1452 w 0:: 5 r"'\. I ,, ~ DW N 1\ /\..-.. r\ V ~1"0- / ~~MAIN SPILLWAY OPERATING -- WERHOUSE AND OUTLET 'GIUTI ES OPERATING I I I I 10 /5 20 25 30 3 TIME (DAYS) RESERVOIR ROUTING 1:10,000 YEAR FLOOD ~f---. POWERHOUSE OUTLETifFACILITIESANDMAINSPILLWAY~OPERATING - I J •I I ~MAX WSEL=1455- J450 o 5 10 15 20 25 TIME (DAYS) RESERVOI R ROUTING /:50 YEAR FLOOD (SUMMER) 30 10 15 20 25 TIME (DAYS) RESERVOIR ROUTI NG I:10,000 YEAR FLOOD 30 35 IL CANYON RGES AND RESERVOIR E ELEVATION S FIGURE E.2.198 ~-------=-A 1 )")l J )1 ]1 1 I J J ~~ V ",," """ ......2010 ./ V ./ // ~/ / (/ /./ ./ _J____/ -," ----- 100 90 80 70 60 50 (f) lI.. U 400 0 Q-w 30 (9 0:: <:I I U (f) 0 20 10 1.02 NOTES, I.BASED ON WEEKLY RESERVOIR SIMULATIONS FOR 2002 AND 2010 DEMAND. 1.11 125 2 5 10 RECURRENCE INTERVAL (YEARS) 20 50 100 GOLD CREEK ANNUAL FLOOD FREQUENCY CURVES WATANA/DEVIL CANYON OPERATION FIGURE E.2.199 I I 'I I I II I I II I I 'I ,I 'I I r ~LEGEND: GOLD CREEK PRE -PROJECT FLOW ••••••••..DEVIL CANYON OUTFLOW r--- - - -GOLD CREEK POST-PROJECT FLOW ~ --~ --- -- I--~ ~ ~ --~ .. ,J\r \ \ ~f\'\~~'--.,,..... ~-~.--~-------.:-.--. ..... 0-........-......-.....---.------".............-..._~...--."-':1 ~.... .-- I I I I dII I I I I II I II I I I 88 72 64 56 en ~u o 48o Q ILl (!) a::« ~40en a 32 24 16 8 o JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1964 DEVIL CANYO SIMULATION ---..._~----.,...-........--,.,.-.,.. IE JULY AUGUSTIMONTH ~N AND GOLD CREEK FLOW IUSING 2002 DEMAND SEPTEMBER OCTOBER NOVEMBER DECEMBER FIGURE E .2.200 88 ---..,...-....,....-------......,,......-or---..,..--........--r----r--..,....----,r---r---~-_r_-_r 80 LEGEND: ---GOLD CREEK PRE-PROJECT FLOW ••••• ••..DEVIL CANYON OUTFLOW --- -GOLD CREEK POST-PROJ ECT FLOW 72 1-------------'--------------------------------- 641-------------------------------------- 56 (i) I.L (J 8 48 0 I.LI (!) 0:«::r 400 (/) 0 321--------------------------------------t-~- 24 I------------------------------------f----'-------It---- 16 1------------------------------+-\-1-------- -------~-~--~-......---~-...8 I---.------------=...::....:.==-=-=----__--=====-----------Ir---\:-:,.,.L----=-::c=-~.............:_••-... JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1967 DEVIL CANYO SIMULATION 1 ------.-----.-.-.----------_-----.1 I TT 1 I I I I I I I I I , I I I T T T I I J I T T - - - I I - - r\ r ....- : I ~- ,~ ~u ~l i~I L ....'~_ r f-'"·····1 - •I -_."''''4/i ........ J W I \/_.\JI I ~l -I I I I 'tI I ~1 ·...0 -I I "-''t I I '"J :~-----~------~----.---..--~.......;.J '\".-..--J._~__• -'--f..........'J••••••l ~!"•••••••••••••...................... i - I I I I I I I I I I I I I I I I I I I I I I I I I JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER MONTH N AND GOLD CREEK FLOW USING 2002 DEMAND FIGURE E.2.201 88 -------......-......------.,....--_--......-_-......,.r-----,r----r---"T"""'I'-~- 80 LEGEND: ---GOLD CREEK PRE-PROJECT FLOW ...•••••..DEVIL CANYON OUTFLOW - - -GOLD CREEK POST-PROJECT FLOW 721-------------------------------------- 641------------------------------------- 56 (/) IL. U 0 48 0 Q w (!) a:«40z 0 (/) 0 32 241------------------------------------- 16 I------------------------------f--+--+-~::_+__...___t__E_ ---_.....-----....._~-....-.....-...._----8 ----....---- FEBRUARY MARCH APRIL MAY - JUNI NOTE-_ TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1970 DEVIL CANYC SIMULATION L DECEMBERNOVEMBEROCTOBER • . ,p=.-J \_~.-:=.-d SEPTEMBERAUGUST "","-~--,,--r .r••••••••••• r MONTH JULY .................................: )N AND GOLD CREEK FLOW JSING 2002 DEMAND FIGURE E.2 .202 88 I I II I I II I I II I I 'I I I l(I I -LEGEND: GOLD CREEK PRE -PROJECT FLOW.........DEVIL CANYON OUTFLOW80----GOLD CREEK POST-PROJECT FLOW - 72 I--~ 64 r- 56 I-- en I.L.u o 48 0 ~Q w I-- (.!) 0::«z 40<.> (/) 0 I-- 32 ~---------------------------------I------- 24 t------------------------------------t----- t'\ 16 t----------------------------------f--F--.,--\--"- I \ r \ I '--J-----.,',."-------\,.' \,.'.,'",L I •00, 8 t-------------'----------------~~=;:::__--------....l,..t....-.~.........I_'---:".:...----------,_-J''r "-----..... - o L::=JI==IC=IIC::::::II==CI=::tII::::~t::=:t::=:dI=::::t:=::::!==:]IC:=CI=JI~_LlII_---lI_--l..1 JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1964 DEV IL CANYO SIMULATION ~'-""\"'.....I •••• e ••••• ~, ,\ I·..\'"~\".--.,~i .V."•••••~••'I • ~..,-'-"'~''''''-~-'t . . . . . . .,".-.-~---.....-...--.........r--···· I MONTH ,N AND GOLD CREEK FLOW [USING 2010 DEMAND FIGUR E E.2.203 I I I I I I I I I JI I I 'I I I I I I I LEGEND I-, GOLD CREEK PRE-PROJECT FLOW ••••••••DEVIL CANYON OUTFLOW- - - -GOLD CREEK POST-PROJECT FLOW - - f- I-- - ~- ~ I--~~~ f\ I-- V fr---/\ -~--------,"'\,'''oJ''''''''1'\1 '-"'__If L __________""\-~~....., ~........~.................................~I.... ~ I ~, ll- I II I I I I I I II I I I I 88 80 64 56 (i) u.. lJ 8 48 0 ~ t!) 0::«40:r 0 ~ c 32 24 16 8 o JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE: TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1967 DEVIL CANYON SIMULATION US I I I I , I I I I I I I I I I I ,I I I 1 I I r I - - - - - - ~- \J J\1 ~1i····.~- I t ~! W \J "f !~~,I ::....-r...... J I ,J ,.J"........;~!....~...,--.....;--~---.......,,-~--~t •r- i"l r···..·······I1\'\J ....,-\• ••••::\-~=l II""•...... i ...._-....J.J :~-:_............"--'................ - I I I I I I I I I I I I I I I I I I I I I I I I I MONTH JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER AND GOLD CREEK FLOW ilNG 2010 DEMAND FIGURE E.2.204 88 ....----1....--......1-......11-......-'-'...----r-......r-......-r-I........--I"""Tr--r\-"TT"II-I,...---"""Tr--rll-r---....'-r-Ir ......LEGEND: GOLD CREEK PRE-PROJECT FLOW •••••••••DEVIL CANYON OUTFLOW 80 ------GOLD CREEK POST-PROJECT FLOW f- 72 f- 64 f- 56 -f-- II) IL. U 0 48 0 0 ~ LaJ f- (!)a::« :J:400en 0 f- 32 f- 24 - 16 ,'.--- - I A.\r.I - "--"'-1!8 I--...-.__=._=_=_:-:-:_=-=_=-------------------,=;;}----+_:-:-J...,.,....~,,---_-..r~..,.;;::_~J";-....,.~_=_=-_-"1I.J-----------------------_.J J ... o L=:::::I:=::;:t:::::::jtfl:=t:::=:::::t:==±I==:±::::::::jt:::::ft.1==:r::::=r:=:'~...lIL--lII__L-I_.L'L1-l'_..lI.-j JANUARY FEBRUARY MARCH APRIL MAY JUNE NOTE,. TIME SCALE IS IN INCREMENTS OF 10 DAYS. 1970 DEVI L CANYON SIMULATION US DECEMBERNOVEMBEROCTOBER -~""'-:::::.":":'~:::.~::-.~.~.~;::.-::. SEPTEMBERAUGUSTJULY MONTH .•••••••••••••••••••••••••••J AND GOLD CREEK FLOW ING 2010 DEMAND FIGURE E.2.205 I .........- "'........."....- , "'-......--',-- j 10 2 0 10 20 30 • %OF TIME DISCHAI 105 8 6 10 2 0 10 20 30 ~ %OF TIME DISCHAI 10 2 0 10 20 30 ~ %OF TIME DISCHAI 105 8 6 4 2 10 4 8 Ul 6...u 4 1&.1 C)a:«2zu Ula 10 3 8 6 4 2 4 2 10 4 8 Cfl 6lo- U 4 1&.1 C)a:«2zu Cfla 10 3 8 6 4 2 10 5 8 6 4 2 10 4 8 Cfl 6...u 4 1&.1 C)a:«2zu Cfla 10 3 8 6 4 2 ....-- - ~r-.. F~BR~A~Y ~"--t---..... ------ dUllY f---r------ I-r----r---r- D~CEIMBfR 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 2 4 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 1&.1 C)a: :i 2u Ula 10 3 8 6 10 5 8 6 4 2 10 4 Cfl 8...6u 41&.1 C)a:«2zu Cfla 10 3 8 6 4 2 4 2 10 4 Cfl 8...6u 4 LJJ C)a:«2zuCfla 10 3 8 6 4 2 Ul...u I'r--_----..... ............ ---..-..r-~ JUINE ~----1---- ...........r---r--- J~NUA~Y ------ ........-.....-.....-t----1--...... I 1N~VE~BfR 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 o 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 105 8 6 10 5 8 6 4 2 104 Cfl 8...6u 41&.1 C)a:«2zu Cfla 103 8 6 4 2 4 2 _10 4 Cfl 8...62 4 1&.1 C)a:«2zu Cfla 10 3 8 6 4 2 10 5 8 6 4 2 10 4 Cfl 8...62 41&.1 C)a:«2zu Cfl -a 10 3 8 6 4 2 IO!!IO!!. 8 8 6 6 4 4 2 2 --I-. 104 10 4-lii 8 -~8 (/)...6 ...6 ~to)to)---.-4 -4auI&J \Cl f------..~II:ic(2 f--.c(2J:J:to)~to) Ul (/) 15 10 3 15 10 3 8 8 6 6 4 4 2 2 ~A~CHI 10 2 AP~IL 10 2 M~Y ~O 50 60 70 80 90 100 0 10 20 30 40 !!O 60 70 80 90 100 0 10 20 30 40 !SO 60 70 80 90 100 RGE EQUALLED .OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10!!10!! 8 8 6 6 4 4 2 2--........~t-r-...10 4 -104 ro----~8 ~8Ul........Ul I-.-...6 ...6to)~-1'"-_-~-i"",au 4 4 -""'-au Cl Cl ........II:II:~2 c(2J: to)to) Ul ,(/) 15 10 3 15 10 3 8 8 6 6 4 4 2 2 ,UGIUST 10 2 SE1PT ~"~ER 10 2 °ICTI)B~R W5060708090 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 RGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIM£DISCHARGE EQUALLED OR EXCEEDED NOTE:i...E.JEND: I.CURVES BASED UPON AVERAGE MONTHLY PRE-PROJECT FLOWS FLOWS FOR 32 YEARS OF SYNTHESIZED ----WATANA /DEVIL CANYON FLOWS RECORDS DERIVED FROM HISTORICAL AND-FILLED DATA.... \.... \.... \. "i'."--MONTHLY AND ANNUAL "-FLOW DURATION CURVES SUSITNA RIVER AT WATANA ~N~UA~ 10 50 60 70 80 90 100 RGE EQUALLED OR EXCEEDED FIGURE E.2.206 r---.............-......... 10 2 0 10 20 30 %OF TIME DISCHt 10 5 8 6 4 2 10 4 8 IJl 6IL- U 4ILl Cl II::«2:I: U IJl 0 10 3 8 6 4 2 ~r-- F~BR~A~Y 10 2 o 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 2 IJl IL- U ILl 4 Cl II:: ~2u IJl 15 10 3 8 6 4 f-+----------- """"-.I-r--r---- J~N~ARIY 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 IJl 8 IL-6u 4ILl Cl II::«2:I: U IJl 0 103 8 6 4 2 \ "-...... \...."-.... ..........-................-'......---- 10 2 0 10 20 30 %OF TIME DISCH, 10 2 0 10 20 30 %OF TIME DISCH~ 10 5 8 6 4 2 10 4 8 IJl 6IL- U 4 ILl Cl II::«2:I: ~ 0 10 3 8 6 4 2 10 5 8 6 4 2 10 4 8 IJl 6IL- U 4 l1J Cl II::«2:I: U IJl 15 10 3 8 6 4 2 1------...--f-_ r"-.............r----..... D~CEIMBfR .....r----j'..... --.- dUllY 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TI'l'E DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 IJl 8 IL-6u 4ILl (!) II::«2:I: U IJl 15 10 3 8 6 4 2 2 10 4 IJl 8 IL-6u 4 l1J (!) II::«2:I: U IJl 0 10 3 8 6 4 2 f---f--ro-~ -.......-'--..........r-................ N~VE~BfR .......~--r-................ I r-....- -~ I JU1NE 10 2 0 10 20 30 40 50 60 70 80 90 100 %·OF TI ME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 2 10 5 8 6 4 2 10 4 IJl 8 IL-62 ILl 4 (!)a::«2:I: U (/) 0 10 3 8 6 4 2 ILl Cl II:: ~2u (/) 15 10 3 8 6 4 ...................--- ,. \ M~Y 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 8 Ul 6IL. U 4 I&J l.!la: <I:2:I: U Ul 15 10 3 8 6 4 2 - "-'r-.r-r-- AP~IL 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED O'R EXCEEDED 10 5 8 6 4 2 10 4 8 Ul 6IL. U 4w l.!la: <I:2:I: U Ul 15 10 3 8 6 4 2 IMA~CHI 40 50 60 70 80 90 100 IRGE EQUALLED OR EXC EEDED -----...... --....... °ICT?B~R2 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 8Ul IL.6 ~ 4w l.!la: <I:2:I: U Ul 15 10 3 8 6 4 2 .........r-.-.........r-- " SEIPT~M~ER 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 10 4 Ul 8 IL.6u w 4 l.!la: <I:2:I: U Ul 15 10 3 8 6 4 2 40 50 60 70 80 90 100 IRGE EQUALLED OR EXCEEDED -r------- ,UGIUST MONTHLY AND ANNUAL FLOW DURATION CURVES SUSITNA RIVER AT DEVIL CANYON "'." '\ "'-r---..... ~N~UA~ NOTE; I.CURVES BASED UPON AVERAGE MONTHLY FLOWS FOR 32 YEARS OF SYNTHESIZED RECORDS DERIVED FROM HISTORICAL AND FILLED DATA. LEGEND: PRE-PROJECT FLOWS - - ---WATANA I DEVIL CANYON FLOWS 40 50 60 70 80 90 100 ~RGE EQUALLED OR EXCEEDED FIGURE E.2.207 ..---- ""'-'-- ~A~ 10 2 0 10 20 30 40 51 %OF TIME DISCHARGE! 10 5 8 6 4 2 10 4 8 Ul 6... (,) 4.... C) It: ~2 (,) Ul 0 103 8 6 4 2 -----1--- .......'--- F~BR~A~Y 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 2 Ul... (,) .... ~ ~2 (,) Ulo 10 3 8 6 4 ~------- r-... '--r- J~N~A~Y 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 2 104 'in 8...6(,) 4.... C) It:<[2:I: (,) Ul 0 103 8 6 4 2 I\. r---..... 'r--."'-..r\. " 'N~I I'....--r-, .......I----- 'UGI' 10 2 0 10 20 30 40 5( %OF TIME DISCHARGE E 10 2 0 10 20 30 40 5( %OF TIME DISCHARGE E 10 5 8 6 4 2 10 4 8 Ul 6... (,) 4.... C) It: <[2:I: (,) Ul 0 10 3 8 6 4 2 10 5 8 6 4 2 10 4 8 Ul 6... (,) 4.... ~ <[2:I: (,) Ul 0 10 3 8 6 4 2 -.--I----1--- ........10-.---..r---r-........... D~CEIMBfR ---..---""'\-- dUllY 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 8 6 4 10 5 8 6 4 2 10 4 Ul 8...6(,) ....4 C) It: <[2:I: ~ 0 103 8 6 4 2 2 10 4 Ul 8...6.(,) 4.... C) It: <[2:I: (,) Ul is 10 3 8 6 4 2 .......... """-..... I---I-- r---"1--- JU1NE r-1---- .........,... -:--r---I'--.~ N~VE~BfR 10 2 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 2 10 2 0 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED ,10 5 8 6 4 10 5 8 6 4 2 104 ~8...6~ 4.... C) It: <[2:I: (,) Ul 0 10 3 8 6 4 2 .... C) It: ~2 ~o 103 8 6 4 10 5 10 5 8 8 6 6 4 4 2 2 i'o... l"--t--r-....... 104 I----10 4 l-i----~8 ~8 (/) 6 (/) I&.I&.6 1\U U \.~4 ~4........<!l fi!a:: 21'--..<C(<C(2:I:-t--:I: lil r-ut--t--(/)Ia 10 3 r---+--a 10 3 8 8 6 6 4 4 2 2 tCH I APRIL M~Y 10 2 1 10 2 ()60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 \0 20 30 40 50 60 70 80 90 100 EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 5 10 5 8 8 6 6 4 4 2 ~2 :J '.r-.r- 1'....t--'-----,...--10 4 10 4-~8 ~8(/)(/)--I&.6 I&.6u~.~r--4 4....................<!l <!la::a:: <C(2 <C(2:I::I:U U (/)(/)a 10 3 a 10 3 8 8 6 6 4 4 2 2 1 UST 10 2 SErr~M~ER 10 2 °ICT?B~R o 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 ~QUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED NOTE:LEGEND: I.CURVES BASED UPON AVERAGE MONTHLY PRE-PROJECT FLOWS FLOWS FOR 32 YEARS OF SYNTHESIZED ----WATANA I DEVIL CANYON FLOWS-RECORDS DERIVED FROM HISTORICAL DATA. ..... "'\ .........I'--.1'..MONTHLY AND ANNUAL FLOW DURATION CURVES SUSITNA RIVER AT GOLD CREEK UA~ )60 70 80 90 100 ~UALLED OR EXCEEDED FIGURE E.2.208 I'llo.......... .~ ---. -~ 1 3 10 0 10 20 , %OF TIME DIS 3 10 0 10 20 ~ %OF TIME DIS 3 10.0 10 20 : %OF TIME DIS 10 6 8 6 4 2 10 5 8Ul6I&- U 4 LLI (!) ll::«2:I: Urn 0 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 UJ 6II.. U 4LLI (!) ll:: <[2:I: ~ 15 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 Ul 6I&- U 4 LLI (!) II::«2:I: U UJ 15 10 4 8 6 4 2 .....-..r---r---1----- I--.. r---~ D~CE~B~R -1---~--- JU1LY ~~---- -..... -I"--... F~BR~A~Y 2 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 2 3' 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 10 5 rn 8 I&-6u 4LLI (!) II:: ~2u UJ 0 10 4 8 6 4 2 4LLI (!) II:: ~2u UJ 15 104 8 6 4 4 2 10 5 UJ 8 II..6,U 4 LLI (!) II::«2:I: Urn 0 10 4 8 6 4 2 I--:-r--,------ -...... I N~VE~BfR ----.;.-........-. JU1NE - --I--~-.I- -----............. J~NUA~Y 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 3 10 0 10 20 30 40 50 60 70 80 90 100 %·OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 ~105 rn 8I&-60 4 1&1 (!) II::«2:I: ~ 0 10 4 8 6 4 2 2 10 5 UJ 8 I&-6~ 41&1 (!) II:: <[2:I: 0rn 0 10 4 8 6 4 2 10 6 8 6 4 2 105 UJ 8 I&-6u 4 1&1 (!) II:: <[2:I: U UJ 0 10 4 8 6 4 2 --....r-...---~----"""-.-~~ ..~y ---..~l-I---I---r-I- I °ICT?B~R 10 3 o 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 2 105 8Ul6u.u 4 UJ Cla: c(2:I: U Ul 15 10 4 8 6 4 2 4 2 10 5 8Ul...6 ~ 4UJ Cla: c(2:I: U Ul is 10 4 8 6 4 2 r-----'--............ AP~IL I -.-10..-..~-:-t----1---~"'"---... I SEIPT~"~ER 10 3 o 10 20 30 40 50 60 70 80 90·100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 4 2 10 5 Ul 8...6u UJ 4 Cla: c(2:I: U Ul is 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 Ul 6... u 4 UJ Cla: c(2:I: U Ul 15 10 4 8 6 4 2--- IMA~CHI --ro-.. ~ ,UG,UST ,0 40 50 60 70 80 90 100 :HARGE EQUALLED OR EXCEEDED 10 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED MONTHLY AND ANNUAL FLOW DURATION CURVES SUSITNA RIVER AT SUNSHINE , - "1\1"-,'"- '"i"'.. "'i'--.. ~N~UA~ NOTES I.CURVES BASED UPON AVERAGE MONTHLY FLOWS FOR 32 YEARS OF SYNTHESrZED RECORDS DERIVED FROM HISTORICAL AND FILLED DATA. LEGEND PRE-PROJECT FLOWS - - -WATANA!DEVIL CANYON FLOWS o 40 50 60 70 80 90 100 :HARGE EQUALLED OR EXCEEDED FIGURE E.2 .209 ~t--.. !"'--.-. ~ r-.... 10 3 0 10 20 %OF TIME DI~ 3 10 0 10 20 : %OF TIME DI~ 10 3 0 10 20 ~ "10 OF TIME DIS 106 8 6 4 2 10 5 8 (I)6lo- U 4 lIJ Cl II:«2xu (I) is 104 8 6 4 2 106" 8 6 4 2 10 5 8 (I)6lo- U 4 1&1 Cl II: :!2u (I) is 10 4 8 6 4 2 10 6 8 6 4 2 10 5 8 (I) 610- ~4 1&1 Cl II: :!2 ~ is 10 4 8 6 4 2 80 90 100 OR EXCEEDED ~--_.-----1-.....- ...... F~BR~AI IY ... ~,-'----- dUllY """..........-,-"--.............~ --. .......... D~CEIMBfR 10° 8 6 4 10 3 0 10 20 30 40 50 60 70 "10 OF TIME DISCHARGE EQUALLED 10 6 8 6 3 10 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED (I) 10- ~ 1&1 Cl II: ~2u (I) is 10 4 8 6 4 2 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 2 10 6 8 6 4 2 10 5 (I)8 10-6u 41&1 Cl II:«2xu (I) is 10 4 8 6 4 2 4 2 10 5 (I)8 10-6u 4 1&1 ClII:«2xu Ul is 104 8 6 4 2 ~--r------.........--~r- "~N~A~Y ......."""'-~-......--- ...... dU1NE - 100... ~~--1'000....--r-""'-r--""--.............. N~VE~B~R 2 2 2 2 2 104 8 6 4 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 106 8 6 4 10 3 0 10 20 30 40 50 60 70 80 90 100 %OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 3 o 10 20 30 40 50 60 70 80 90 100 %.OF TIME DISCHARGE EQUALLED OR EXCEEDED 10 6 8 6 4 10 6 8 6 4 2 10 5 (il 8 10-6u 4 1&1 C!I II:«2xu (I) is 10 4 8 6 4 2 10 6 10 6 8 8 6 6 4 4 2 10 5 10 5 U;8 ~8 6 U) 61L1L ... U U -~~4 ~4 -l.LI l.LI ~(!)i!0:: <C 2 <C 2J:-J: U -.U----""--U)-....---U)r--is 104 """----l-is 10 4 8 8 6 -6 4 ......4 2 2 IMA~CHI 10 3 AP~IL 10 3 M~Y 50 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED "to OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED 106 106 8 8 6 6 4 4 2 2-105 10 5 ~8 ~8U)-U) 1L 6 1L 6u-~~-~......... l.LI 4 ...l.LI 4 -III....!!..---...(!)(!) 0::0::<C 2 <C 2 -J:J:U U(I)U) is is 10 4 104 8 8 6 6 4 4 2 2 ,UGIUST 10 3 SEIPT~M~ER 10 3 °ICT?B~R 10 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED %OF TIME DISCHARGE EQUALLED OR EXCEEDED , NOTES LEGEND I.CURVES BASED UPON AVERAGE MONTHLY PRE -PROJECT FLOWS FLOWS FOR 32 YEARS OF SYNTHESIZED ----WATANA/DEVIL CANYON FLOWS RECORDS DERIVED FROM HISTORICAL ~.AND FILLED DATA. '"'""-"- "~...... "'" 1""'.."'-... MONTHLY AND ANNUAL ~FLOW DURATION CURVESr"'o.. "SUSITNA RIVER AT SUSITNA STATION. ~N~UA~ ~o 40 50 60 70 80 90 100 CHARGE EQUALLED OR EXCEEDED FIGURE E.2..210 100908070605040302010 I~~ \\'",\ \,\~....- \. I--_ 100 __ I'-__ \'--\-....--"""--~.:::=4\- \~ \ ~ '"'"'"i\ \ \ 0.4 o 0.6 0.8 2 20 6 80 60 10 40 w ~cr <! :J: ~4 a ent 8 o 8 - - - - PERCENT OF TIME DISCHARGE EQUALLED OR EXCEEDED -LEGEND:NOTE:FLOW DURATION CURVES ARE BASED PRE -PROJECT ON MEAN WEEKLY DISCHARGE. WATANA/DEVIL CANYON OPERATION-2002 DEMAND WATANA/DEVIL CANYON OPERATION-20JO DEMAND ,.... ANNUAL FLOW DURATION CURVE SUSITNA RIVER AT GOLD CREEK PRE -PROJECT AND WATANA /DEVI L CANYON OPERATfON FIGURE E.2.211 38 36 34 32 30 28 26 24 (/) LL U 0 220 0 w Cl 0::20« :I:u (/) Ci 18 16 14 12 10 8 6 4 LEGEND: ----3%I-- _00_25% 50% ----70% >-----_0-90% ----97% \,, \:..:----~~~ \" 00 ........,~.--~1'.--..~~,.-/0 , ..~~L.......,..,.,'-o I --0.\./-J I \,'\ I "---. I ~~J ~~~...----~':-_"-_-:~ I:-..~.,-~::::-::::::-::-:::,....._-----==-.=;.;........ ,,{/, I .I I ..I 2 4 OCT 6 8 NOV 10 12 DEC 14·16 JAN 18 20 22 24 WEEK 01 FEB MAR NOTE:ASSUMES 2010 ENERGY DEMAND.WATANA /DE GOLD CREEK [ PROBABILr A Ii I I J /, I I \ I ft.1 \II \, V \ \ \ I \/•..../ i J i /\1 I \ 1\1/\. \II :\ I :!\/\'\.L-..--,_..~..r 1 v·..,-.'-'-,~..--........."\\./'.----' \~..,~r--/'\~'.1\\..J 1~~5 /'/\. I~---~.'..\......r----.----"V·/.\\.--/.-.....-'--i-""".""",--:::::::.:-:::::::,-.. ~_./_--.../ / I I I I I I -,I I I I I I 26 28 30 32 34 36 38 WATER YEAR APR MAY JUN 'IlONTH IlL CANYON OPERATION ISCHARGES FOR VARIOUS IES OF EXCEEDANCE 40 42 44 46 48 JUL AUG 50 52 SEP FIGURE E.2.212 1350 t= ILl ILl lJ.. z 13000 fi>ILl ..J W ,.., 1250 r- I I II l ~IU_~j -:::::'.,..:--::'-~ ;(r I ~l--.t / '(/ 1,,, rJ (I I I I I I I I (}J I I LEGEND: I JUNE 1,198\ ---JULY 1,198/ ---AUGUST I,1981 f ----SEPTEMBER 1,1981 I I I ..... - ..... 1500 1450 1400 1200 1150 1100 o 2 3 45 6 7 8 WATER TEMPERATURE (Oe) 9 10 II ..... DEVIL CANYON RESERVOIR TEMPERATURE PROFILES JUNE TO SEPTEMBER FIGURE E.2.213 I l I I IIr'-1 I, I I ~l-/ PI . ·I f· I I I I I 1 I I ··· LEGEND: OCTOBER 1,198\ ---NOVEMBER 1,1981 ---DECEMBER 1,\981 - _•••-DECEMBER 31,1981 ,"1""\ I - - 1500 1450 1400 1350 z 9 1300 ~ IJJ ...J IJJ 1250 1200 1150 1100 o 2 3 4 5 6 7 8 WATER TEMPERATURE (OCl 9 10 " .- I i - DEVIL CANYON RESERVOIR TEMPERATURE PROFILES OCTOBER TO DECEMBER FIGURE E.2.214 14 12 I 'i',I \i \I \,'',I J,I L \1'l..'J LJ '~u INFLOW-k.,,'--+-_r---~-~j ,.../-""""";--,r/-\I~\' -_,!f \r'\I ",,'\: ,.,..,I V " \~"\ "I,,Ir Ii.II 1 . 8 j\n 6 10 W 0:: :J ~ 0:: Wa. :::!:w f- uo 4 2 o 10 20 30 9 19 JUNE JULY NOTES: I.TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2.BASED ON 1981 DATA. 3.WATANA ASSUMED UPSTREAM.(DYRESM RUN W4010) 4.OUTFLOW TEMPERATURES ARE BASED ON DYRESM RUNS DC 1020,DC 1021 AND DC 1022. DEVI L CANYON RESERVOI R I~ JUNE" ~r - J ,......1\, V~-A.1\--.'.... '{V .~,,'1'---_v,~'--./-, \ I ,", OUTFLOW l -,..-", /-/i'---.-~~-, r/-, I .;"-'I.r ..7 \ I ...... ~~\(~ \, ~ , I I I - 29 MONTH 8 AUGUST 18 28 7 17 SEPTEMBER 27 7 FLOW AND OUTFLOW TEMPERATURES '0 SEPTEMBER FIGURE E.2.215 14 12 10 ~ u 0 w K-1-_- a::----...1-_-::::> ti:---"""~-a::6w ~'"OUTFLO~a. :!:\r 1'"..-"w I-~-.... '"4 ""~ 2 0 I 1 7 17 27 6 OCTOBER NO NOTES: I)TIME SCALE IS IN INCREMENTS OF 10 DAYS. 2)BASED ON 1981 DATA. 3)WATANA ASSUMED UPSTREAM.(DYRESM RUN W4010) 4)OUTFLOW TEMPERATURES ARE BASED ON DYRESM RUN OC1022. DEVIL CANYON RESERVOIR INFL OCTOBER ,] 1"--.........----------------....._~....1 -..... '\ \. , I I 16 VEMBER MONTH 26 6 16 DECEMBER 26 OW AND OUTFLOW TEMPERATURES TO DECEMBER FIGURE E.2.216 9.0 8.5 --.JUL31--.;:,.:..----.----. 8.0 7.5 u ~ lJJa:::::> ~ ~7.0 a. ::!: lJJ f- 6.5 6.0 5.5 AUGI5 ------------'-----......- .------.. 5.0 95.00 101.00 107.00 113.00 11900 125.00 RIVER MILE NOTE; I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA. 2.DEVIL CANYON TEMPERATURE AND DISCHARGE FROM DYRESM MODEL.(RUNS DCI020 AND DC1021)WATANA /DEVIL DOWNSTREAM TEMF AUG 15.--- SEP 15----~.-- SEP 30;/?~ DEVI L CANYON DISCHARGE (CFS): JUN 15 7920 JUN 305740 J UL 15 6830 JUL 31 6480 AUG 15 9940 AUG 31 24100 (RELEASE) SEP 15 13750 SEP 30 10600 OCT 15 7450 131.00 137.00 143.00 149.00 CANYON OPERATION ::RATURES -JUN TO OCT FIGURE E.2.217 6.0 r---...,.....--...,....-----,----,--,..---r--........-----,----,---r--- 5.5 125.00 RIVER MIL 119.00 WATANA /DEVIL I DOWNSTREAM TEMPI 113.00107.00101.00 5.0 4.5 2.5 4.0 2.0 1.5 1.0 0.5 L...-_...J.---_....l..-_----'-_----l._----JL....-_...L...-_....L..._----'-_----L__I....----l. 95.00 u 3.50 w lr :::> !;t lr Wa. :::!:3.0wr- NOTE: I.MODEL ASSUMES 1981 METEOROLOGICAL DATA RECORDED AT WATANA. 2.DEVIL CANYON TEMPERATURE AND DISCHARGE FROM DYRESM MODEL.(RUN DCI022 ) LE CANYON OPERATION ERATURES -OCT TO DEC DEVIL CANYON DISCHARGE (CFS): OCT 31 8690 NOV 15 10300 NOV 30 10500 DEC 15 10900 DEC 31 11100 FIGURE E.2.218 4.0 3.5 3.0 2.5 u o wa:: ::J ~a::2.0 w Q. ~w I- 1.5 1.0 0.5 0.0 95.00 NOTE: 101.00 107.00 113.00 119.00 125.00 RIVER MILE MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT DEVIL CANYON. WATANAI DEVIL CANYON OPERATION DC OUTFLOW TE~ DEC 15 AND DEC 31 DEVIL CANYON DISCHARGE (CFSl: OCT 7320 NOV 9440 DEC 11,130 JAN 10,480 131.00 137.00 143.00 149.00 OWNSTREAM TEMPERATURES -OCT TO JAN vlPERATURE 4° FIGURE E.2.219 4.0 ---APR 30 3.5 3.0 1.0 0.5 ------~R~_--- 0.0 95.00 101.00 107.00 113.00 119.00 125.01 RIVER MILE NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT DEVIL CANYON. WATANA/DEVIL CANYON OPERATION OUTFLOW T o ........-_........ 131.00 137.00 143.00 149.00 DEVIL CANYON DISCHARGE (CFS): JAN 10,480 FEB 10,090 MAR ·9200 APR 8010 DOWNSTREAM TEMPERATURES -JAN TO APR 'EM PERATURE 4°C FIGURE E.2.220 4.0 3.5 3.0 2.5 u 0 W 0::: ~ ~ 0:::20wa.. ::!:w I- 1.5 1.0 0.5 0.0 9500 10LOO 107.00 113.00 119.00 12!: RIVER M NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT DEVIL CANYON. WATANA/DEVIL CANYON OPERATION OUTFLOW TEM DEVIL CANYON DISCHARGE (CFS): OCT 7320 NOV 9440 DEC 11,130 JAN 10.480 5.00 tILE 131.00 137.00 143.00 149.00 DOWNSTREAM TEMPERATURES -OCT TO JAN PERATURES 4 TO 2°C FIGURE E.2.221 4.0 3.5 3.0 (.)2.5 0 w Cl:: ;:) ~APR 30Cl::2.0wa.. ::!:APR ISw I- 1.5 1.0 0.5 0.0 95.00 101.00 107.00 113.00 119.00 125.00 RIVER MILE NOTE: MODEL ASSUMES DAILY BASED LONG TERM AVERAGE METEOROLOGICAL DATA AND MEAN MONTHLY FLOWS AT DEVIL CANYON. WATANA/DEVIL CANYON OPERATION OUTFLOW TEMI DEVIL CANYON DISCHARGE (CFS): JAN 10,480 FEB 10,090 MAR 9200 APR 8010 131.00 137.00 143.00 149.00 DOWNSTREAM TEMPERATURES-JAN TO APR PERATURE 4 TO 2 0 C FIGURE E.2.222 FR AZI L -;:...:;~:;;::-;~:-=~ ICE PHOTO E.2.1 FRAZIL ICE UPSTREAM FROM WATANA NATURAL LODGEMENT POINT PHOTO E.2.2 ICE COVER DOWNSTREAM FROM WATANA SHOWING NATURAL LODGEMENT POINT PHOTOS E.2.5 E.2.6 E.2.7 E.2.8 PHOTO E.2.3 SLOUGH 9 APPROXIMATELY 3500 FEET UPSTREAM FROM SLOUGH MOUTH,DECEMBER 1982 '-----+--MOUTH SLOUGH 8A PHOTO E.2.4 SLOUGH 8A FREEZEUP,DECEMBER 1982 PHOTO E.2.6 PHOTO E.2.7 PHOTO E.2:5'SLOUGH SA NEAR LRX -29 LOOKING UPSTREAM PHOTO E.2.6 SLOUGH SA - FIGURE E.2.8 PHOTO E.2.7 SLOUGH 8A SHOWING FLOODING DURING FREEZEUP PHOTO E.2.8 ENLARGEMENT OF PHOTO E.2.7 SHOWING TURBULENT FLOW APPENDIX E.2.A RELATIONSHIP BETWEEN MAIN CHANNEL FLOW AND SLOUGH PHYSICAL HABITAT VARIABLES Table of Contents Page List of Tables ii List of Figures iii A.l Introducti on 1 A.2 ·Selection of Sloughs 1 A.3 Definition of Flow Regimes 2 A.4 Main Channel Flow and Physical Habitat 3 Variables of Sloughs A.5 Summary of Methods of Analyses 5 A.6 Discussion of Resu lts 10 A.7 References 14 -i- -ii- - - ""'" - ~I I'''''' -iii - ,- I""'" A.I Introduction Side sloughs of the Susitna River consist of springfed overflow channels between the.mainstem Susitna and its side channels and the edge of the floodplain.The side sloughs are generally separated from the mainstem by well-vegetated gravel bars.Exposed alluvial berms at the heads of the sloughs normally separate the sloughs from mainstem or side channel flows.The controll ing berms at the upstream end of the side sloughs are approximately at the water surface elevations of the mainstemfor mean monthly flows observed during June,Jtily,and August. At intermediate and low-flow periods in the mainstem,the side sloughs convey clear water from small tri butari es and/or upwell i ng groundwater which is essential to the existence of this habitat type.At intermediate mainstem flows,the water surface elevation of the Susitna River causes a backwater to extend well up into the sloughs from their lower end.Even though substantial backwater often exi sts,the sloughs function hydraulically very much like small stream systems and there is a net discharge from the sloughs.At high flows the water surface elevation of the mainstem river is sufficient to overtop the upper end of the slough.. Over thirty sloughs have been identified in the reach of the Susitna River between Devil Canyon and Talkeetna.These slough habitats have been identified by the Alaska Department of Fish and Game (ADF&G)as the main producers of chum salmon in this reach of the river.This reach will be impacted mos t by the regul ated flows from the'proposed Sus itna Hydroe 1ectri c Project.Numerous add it i onal s laughs have been identified between Talkeetna and Cook Inlet. Incremental flow analyses have been prepared for three sloughs in the reach from Talkeetna to Devil Canyon and for one slough in the reach from Cook Inlet to Talkeetna.The analyses performed for these four sloughs consist strictly of hydrologic and hydraulic relationships be- tween the sloughs and the mainstem of the Susitna ..The analyses des- cribe the effects of mainstem flow on slough discharge,water surface elevation,flow depth arid velocity,wetted surface area wetted peri- meter and water table elevations.These relationships provide the hydraulic boundary conditions throughout a range of flows in the Susitna River within which fishery habitats can be defined. A.2 Selection of Sloughs The ADF&G and R &M Consultants,Inc.(R&M)began collecting hydraulic and hydrologic data in the Susitna River ~loughs to describe the rela- tionships between mainstem flow and slough physical characteristics. Although hydraulic data is currently being collected as part of the ongoing studies,data collected primarily in 1981 and 1982 were uti- lized for this analysis.For the incremental analysis,three sloughs upstream of Talkeetna and one slough downstream of Talkeetna have been selected.These sloughs were selected on the basis of location (representative reach of river),salmon productivity (the three sloughs upstream from Ta"1 keetna provide spawning habitat for 60 to 80 percent 1 - of the adult salmon spawning in side sloughs),susceptibility to mainstem flow (changes in mainstem flow under present conditions affect the physical characteristics of the slough),and data availability (detailed-studies have been conducted in these sloughs).The representative selected sloughs are: Above Talkeetna: o Slough 8A (approximate River Mile 126) o Slough 9 (approximate River Mile 129) o Slough 21 (approximate River Mile 142) Below Talkeetna: o Rabideux Slough (approximate River Mile 84) Rabideux Slough is located in the upper portion of the Talkeetna to Cook Inlet reach of the Susitna River and is,therefore,more likely to be affected by altered flows from the proposed project than are sloughs located further downstream. The locations of the sloughs selected for these analyses are shown on Figure A-I.Maps of each of the sloughs are presented in Figures A-2, A-3,A~4,and A-5,respectively. ,...,., A.3 Definition of Flow Regimes As the flow in the Susitna mainstem changes,several characteristic flow regimes are evident in each slough.These regimes are defined as follows:- o Regime I -This flow regime is characterized by a slough flow which is essentially independent of flow in the mainstem (i.e.,there is no backwater effect into the mouth of the slough from themainstem).In this flow regime,the slough acts as a minor tributary to the mainstem. - Regime II -This regime is characterized by mainstem back- water extend i ng into the mouth of the slough because the mainstem water level acts as a hydraulic control.However, the discharge from the slough is largely independent of the mainstem discharge since the upstream berms at the heads of the sloughs are not overtopped. o o Regime III -At sufficiently high flows in the mainstem,the upstream berms of the sloughs are overtopped.Under these conditions,the slough hydrologic and hydraulic characterist- ics are nearly entirely dependent on the mainstem flows. A factor which complicates the distinction of these regimes is that in several cases the sloughs may have two or more channels and associated upstream berms which overtop at different mainstem flows.Therefore, 2- CREEK AND SLOUGH WHISKERS CREEK AND SLOUGH CANYON \0 1 21 20 19 MILES -LEGEND ..... •USGS-- Gaging Station o ! '---LANE CREEK AND SLOUGH e SLOUGH SA Sunshin.Cr. SUNSHINE CREEK AND SIDE CHANNEL u __-WH ITEFISH SLOUGH - Figure A·1 Slough Location Map I i - i j, ~I ~I !ll'!l;\ I~IiJ)C'.J I ~t· I ~" ~I ~-~ '::.~ .~ \", ~ l~ ~ ~~ ~-~j ~ ~Co)-'"=~iii :::'"":z ~ >-l ~1:11 ::::l !l...en ::s Q z V.Ilol 0 a:Co) -e 2~w ..a:a:~ -~ '<:'~........ "-"'0 ~"""-....."-~~:-.... I-.......~ 4...\,.,"() ~s:'-.J ~ <:l ~'-,~I ~ 0J ~ J ~c::J..~.I -1 ~~ ~ oj ~~~. ..........", :-.~:~ "'-.~...':. :;.~......... '".. ':.~ -]~J 1 1 )1 1 1 -.]1 1 -j -,J 1 SUS I T NA .R I V E R .- SLOUGH 9 h, 6:J :J'\ G'I '>: ('b -rtl ......5b ADf ao TRANseCT (lge2.) Q STATION (Raw TAGLINE) WATER QUALITY WEASUREMENT SITE DATAPOD SITE STAff GAGE Raw STAGE RECORDER SURFACE THERMOGRAPH -0 1000II fEET CAPPROll.lCAL11 t----i"--i 8 ID) /),. A <V froYl-5"d :; ({'l81 ) 'DIU <)Jo.c t'j (t.'("C (d 1'( 'S tel.t'{' ~o.~e~ '113A """Ii 'h~~ ';\/ ~. G~ CJ't- .~' .-01 ~\ ./ ....;...').,r;·i~...·;r·-.:..-;·~.~•.,:~ ":JP':.r~·t-';';-' "".p .~:. ':':.:: .'f.~,ci. J. I:i. ';'~ :~;; :! " 'h~"S~L f 5"(1'l81) 5ftA.tt ~a~e-s /2Ci.Z.WIA a,-...1. J 20,.2 WI B ~ I W ~/O(7)q lh'c,~rl7 /14;' :Y\ ~ f 1\ (tl ~ I ~ r:a )It UI... ?~~O FEET «appro..Ie a I.) ~STAFF GAGE A RaM STAGE RECORDER mJ DATAPOD (!)THERMOGRAPH ..",;;:.;,:.•;=_,!'L' -t{2,'v p r tl ;/e 14 2. ",'IE R ,..-- ....-SlJ S'rliA I I MOl,I~ "..;" ~ I -+:- WO/:::/C.SNEE"T /)L O(J6/1 .2 /tile I AllrV leI ;<1 p .J J 1 1 "I )J .1 .1 I ;1 J .J ] II'PfIRl'<. .2-5 RoM 83.5i ~I I I ~, ~.f\r'-,~ ;"{HIN ~I Ber)s~'1.., I"""', subsets of Regime II occur when one or more upstream berms are over- topped by mainstem flow,but the berm with the highest thalweg elevation is not overtopped.These intermediate regimes are defined as Regimes II-A,II-B,etc. Mainstem discharges which distinguish the hydraulic regimes in the slough are referred to as threshold discharges.For each of the four sloughs analyzed,threshold discharge ~stimates are presented in Table A-I along with the ranges of mains tern flows wh i ch encompass the f1 ow regimes described above.Determination of these threshold values were based on computations from available data,field observations,and aerial photographs. Descriptions of these distinct flow reqimes are necessary to describe how mainstem flow and slough physical ~habitat variables are interre- lated.The relationships within each regime can then be used to estimate the physical habitat variables '",ithin and beyond the range of observed values through interpolation and extrapolation for each regime.The methods and information used to define the relationships between mainstem flow and physical habitat characteristics in the sloughs are presented in the Attachment to this Appendix. A.4 Main Channel Flow and Physical Habitat Variables Of Sloughs The following slough physical habitat variables were analyzed with respect to mainstem discharges: o slough discharge o water surface elevations at the mouth,near mid-slough,and near the upstream berms o water depths at the mouth,near mid-slough,and near all upstream berms o average velocities mid-Slou¥?,and sloughs.- at cross-sections at the mouth, near the upstream berms of near the "... o total wetted surface area o wetted perimeters at cross-sections at the mouth,near mid-slough and near the upstream berms of the sloughs o water table elevations in the vicinity of the sloughs. 1/Observed lateral velocity distributions and velocity ranges are provided in the Attachment for selected cross-sections (transects). ! ! Table A-I THRESHOLD DISCHARGE ESTIMATES Susitna River Discharge at Gold Creek Sus itn a River Discharge at Sunshine - Slough 8A (cfs) Slough Slough 9 21 (cfs)(cfs) Rabideux Slough (cfs)-Discharge at which mai nstem acts as a hydrau 1ic control of slough water- surface elevation 10 OOoll 11 OOo§.l 21 40G!./<10 OOO~/at mouth (Regime ,,,, II flow begins) Discharge at which intermediate berm 26,00o~/l/N/A§!24,80C/l N/AE.I .~. is overtopped (Regime II-A flow begins)-Discharge at whi ch 30 OOoll 20,50o§.l 2600~1 65 ooo1-Q.Ihighestbermis,,, overtopped (Regime 32,0Q()±!23 OOoll -! III flow begins), N/A -Not applicable -II flow exists during very low Regime II assumed to occur for and 15,000 cfs. 101 §/ II Field estimate. 21 Based on field observations on June 29,1982. 31 IISl oug h Hydrology,Interim Report,1I R&M,Dec.1982,p.2-1. 41 Based on aerial photo. 51 Based upon data in IIpreliminary Assessment of Access of Spawning Salmon to Side-Slough Habitat above Talkeetna,1I E.W.Trihey,Nov.1982. 61 Slough 9 and Rabideux Slough rlo not have intermediate berms.!J Based on staff gage data in IIS us itnaHydro Aquatic Studies, Phase II Base Data Report,Volume 4:Aquatic Habitat and Instream Flow Studies 1982,Appendix A,Alaska Department of Fish and Game,1983,11 Table 4-A-3,p.4-A-67. IIS us itna Hydro Aquatic Studies,Phase II Basic Data Report,Volume 4:Aquatic Habitat and Instream Flow Studies,Part I,ADF&G, 1983,11 Table 41-3-2,p.43. ~I Aerial photos indicate Regime mainstem flows of 15,000 cfs. discharges between 10,000 cfs Based on aerial photos. 3-1 r- Regime I Regime II ,'i'tl>1~ Regime I I-A to """II-n Regime III, TABLE A-I (Cont1d) REGIME DISCHARGE ESTIMATES Sus itna River Susitna River Discharge Discharge at at Gold Creek Sunshine Slough Slough Slough Rabideux 8A 9 21 Slough (cfs)(cfs) (cfs)(cfs) <10,000 <11,000 <21,400 N/A 10,000-11,000-21,400-10,000- 26,000 20 500Y 24,800 65,000, 26,000-N/A 24,800-'N/A 30 00011 ,,26,000, >30,000 >23,000 >26,000 >65,000 l!IISlough Hydrology,Interim Report.II R&M,December 1982,P.2-1 Based on aerial photography this flow is estimated to be 32,000 cfs. Yllpreliminary Assessment of,Access of Spawning Salmon to ,Side-Slough Habitat above Talkeetna,lI E.W.Trihey,November,1982. Based on data in "Slouth Hydrology,Interim Report",R&M Consul- tants,December,1982.p.2-1,this flow is 23,000 cfs. 3-2 For the reach from Talkeetna to Devil Canyon,the relationships between mainstem flows and the slough physical habitat variables were analyzed for average daily discharges of the Susitna River at Gold Creek (USGS gage no.15292000)for ice-free conditions.Physical characteristics of the sloughs are presented for mainstem flows ranging from 1000 cfs to 31,000 cfs in increments of 2000 cfs and at 12,000 cfs. Tables A-2,A-3,and A-4 present tabulated results of the effects of the mainstem discharges on physical habitat variables for Sloughs 8A, 9,and 21,respectively.The methods of analysis and the information used in preparing the tables are presented in the Attachment,Parts 1, 2,and 3. For analyzing the effects of mainstem flow on Rabideux Slough,located downstream from Talkeetna,it was necessary to expand the range of flows considered.Contributions from the Chulitna and Talkeetna Rivers constitute approximately 40 and 20 percent,respectively,of the natural flows in the Susitna River at the Sunshine Gaging Station. The Chulitna and Talkeetna flow contributions,therefore;reduce the influence of Susitna River flows measured at Gold Creek on the physical characteristics of Rabideux Slough.Mainstem flows at Gold Creek of 1000 to 31,000 cfs encompass only the low flow conditions downstream from Talkeetna as measured at the Sunshine Gaging Station (USGS Gage No.15292780).In order to account for the wider range and higher average flows encountered at Rabideux Slough,three flow conditions at the Sunshine Gage Station were defined based on the Chulitna and Talkeetna River flows.The incremental flows of the Susitna River at Go 1d Creek were added to the sum of flows from the Chu 1itna and Talkeetna Rivers.In this way the majority of pre-and post-project flow conditions and the effects on Rabideux Slough physical characteristics could.be analyzed.The three flow conditions used for the analysis were: Condition 1:.Sum of the mean daily low flow for the Chulitna and Talkeetna Rivers during September,typically the lowest flow month during the ice-free season.The low flow contribution from each river consists of the 90 percent exceedance flow.Flows·at Gold Creek were added incre- mentally to the sum of these flows to defi ne the lower third of the potential range of flows observed at Rabideux Slough.. Condition 2:A medium flow range at Rabideux Slough was derived from the fifty percent exceedance flows in the Chulitna and Talkeetna Rivers using the mean monthly flow in August. August fl ows were sel ected because of the salmon mi gra- tion activity which occurs in August.Gold Creek flows ranging from 1,000 to 31,000 cfs were incrementally added to the sum of the mean August month ly flows from the Chulitna and Talkeetna Rivers to provide a medium flow range at Rabideux Slough. 4 Sheet 1 of 3 Table A-2 MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 8A Water Surface Elevation Flow Depth Susitna River Slough Inter-Inter- Discharge at Di scharge Mid-mediate Upstream Mid-mediate Upstream Gold Creek at Mouth Mouth Slough Berm Berm Mouth Slough Berm Berm (cfs)(efs)(ft~msl)(ft~msl)(ft~msl)(ft ~ms 1)(ft)(ft)(ft )(ft) 1~000 3 559.4 568.6 N/A N/A 1.1 0.2 0 0 3~000 3 559.4 568.6 N/A N/A 1.1 0.2 0 0 5~000 3 559.4 568.6 N/A N/A 1.1 0.2 0 0 7~OOO 3 559.4 568.6 N/A N/A 1.1 0.2 0 0 9~000 3 559.4 568.6 N/A N/A 1.1 0.2 0 0 11 ~000 8 561.4 568.8 N/A N/A 3.1 0.4 0 0 12~000 8 561.8 568.8 N/A N/A 3.5 0.4 0 0 13 ~000 8 562.1 568.8 N/A N/A 3.8 0.4 0 0 +>0 15~000 8 562.5 568.8 N/A N/A 4.2 0.4 0 0 I 17 ~000 8 562.8 568.8 N/A N/A 4.5 0.4 0 0I--' 19~000 8 563.0 568.8 N/A N/A 4.7 0.4 0 0 21~000 8 563.2 568.8 N/A N/A 4.9 0.4 0 0 23~000 8 563.3 568.8 N/A N/A 5.1 0.4 0 0 25 ~000 8 563.4 568.8 N/A N/A 5.2 0.4 0 0 27~000 8 563.5 568.8 573.2 N/A 5.3 0.4 0.1 0 29~000 11 563.5 568.8 573.3 N/A 5.4 0.4 0.2 0 31~000 43 563.6 569.8 573.4 N/A 5.5 0.4 0.3 0 N/A -Not Applicable Note:See Figure A-2 for location of mouth~.mid-slough~intermediate berm,and upstream berm. See Attachment,Part I,for narrative and worksheets explaining method of determining slough physical habitat variables.. ,I •.J J ,I ',.1 ,'J .1 J "I J J ],..1 C'I ']1 .~-)1 'I )')1 ]-1 1 1 Sheet 2 of 3 Table A-2 (Cont'd) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 8A Average Velocity Wetted Perimeter Susitna River Inter-Wetted Inter- Discharge at Mid-mediate Upstream Surface Mid-mediate Upstream Gold Creek Mouth Slough Berm Berm Area Mouth Slough Berm Berm' (cfs)(ft/sec)(ft/sec)(ft/sec)(ft/sec)(ft2)(ft)(ft)(ft )(ft ) 1,000 0.06 0.3 N/A N/A 305,000 62 54 0 0 3,000 0.06 0.3 N/A N/A 305,000 62 54 0 0 5,000 0.06 0.3 N/A N/A 305,000 62 54 0 0 7,000 0.06 0.3 N/A N/A 3U5,000 62 54 0 0 9,000 0.06 0.3 N/A N/A 305,000 62 54 0 0 11,UOO 0.03 0.4 N/A N/A 480,000 147 59 0 0 12,000 0.03 0.4 N/A N/A 500,000 152 59 0 0 +::>13,000 0.02 0.4 N/A N/A 520,000 155 59 0 0I N 15,000 0.02 0.4 N/A N/A 570,000 160 59 0 0 17,000 0.02 0.4 N/A N/A 610,000 163 59 0 0 19,000 0.02 0.4 N/A .N/A 650,000 165 59 0 0 21,000 0.01 0.4 N/A N/A 700,000 166 59 0 0 23,000 0.01 0.4 N/A N/A 740,000 .167 59 0 0 25,000 0.01 0.4 N/A N/A 780,000 167 59 0 0 27,000 0.01 0.4 0.5 N/A 830,000 168 59 7 0 29,000 0.02 0.4 2.5 N/A 870,000 169 59 15 0 31,000 0.07 0.4 7.0 N/A 910,000 170 59 81 0 N/A -Not Applicable Note:See Figure A-2 for location of mouth,mid-slough,intermediate berm,and upstream berm. See Attachment,Part 1,for narrative and worksheets explaining method of determining slough physical habitat variables. Sheet 3 of 3 - Table A-2 (Cont'd)~ MAINSTEM DISCl1ARGE VS.PHYS ICAl HABITAT VARIABLES SLOUGH 8A -, Water Table Elevation Sus itna Ri ver Mid-Mid- Discharge at Slough Slough Upstream Gold Creek Well A Well B Well (cfs)(ft,ms1)(ft,ms 1)(ft,msl)- 1,000 565.6 568.0 574.7 3,000 565.6 568.0 574.7 5,000 565.6 568.1 574.8 7,000 565.6 568.2 574.8 9,000 565.6 568.3 574.8 11,000 565.6 568.3 574.9 -12,000 565.6 568.4 574~9 13,000 565.6 568.4 574.9 15,000 565.6 568.5 574.9 -, 17,000 565.6 568.5 575.0 19,000 565.6 568.6 575.0 21,000 565.6 568.6 575.0 23,000 565.6 568.7 575.0 -, 25,000 565.7 568.7 575.0 27,000 565.7 568.8 575.1 29,000 565.7 568.8 575.1 .. 31,000 565.7 568.9 575.2 .-"N/A -Not App 1 icab 1e Note:See Figure 2 for well locations. See Attachment,Part 1,for narrative and worksheets explaining method of determining water table elevations 4-3 'j .~)-1 c ~~'1 1 1 1 I 1 I 1 I ] Sheet 1 of 3 Table A-3 MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 9 Water Surface Elevation Flow Depth Susitna River Slough Di scharge at Discharge Mid-Upstream Mid-Upstream Gold Creek at Mouth Mouth Slough End Mouth 'Slough End (cfs)(cfs)(ft,msl)(ft,msl) (ft,msl)(ft )(ft )(ft ) 1,000 3 589.6 593.3 N/A 0.1 0.9 0 3,000 3 589.6 593.3 N/A 0.1 0.9 0 5,000 3 589.6 593.3 N/A 0.1 0.9 0 7,000 3 589.6 593.3 N/A 0.1 0.9 0 9,000 3 589.6 593.3 N/A 0.1 0.9 0 11,000 3 589.6 593.3 N/A 0.1 0.9 0 12,000 6 589.9 593.3 N/A 0.4 0.9 0 13,000 6 590.1 593.3 N/A 0.6 0.9 0 +:>15,000 6 590.5 593.3 N/A 1.0 0.9 0I +:>17,000 6 591.0 593.3 N/A 1.5 0.9 0 19~000 6 591.4 593.3 N/A 1.9 0.9 0 21,000 22 591.7 593.4 602.8 2.2 1.0 1.8 23,000 80 592.1 593.9 603.4 2.6 1.5 2.7 25,000 152 592.6 594.3 603.9 3.0 1.9 3.1 27,000 232 592.9 594.5 604.2 3.4 2.1 3.4 29,000 320 593.3 594.8 604.5 3.8 2.4 3.7 .31,000 405 593.7 595.2 604.6 4.2 2.8 3.9 N/A ~Not Applicable Note:See Figure A-3 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 2,for narrative and worksheets explaining method of determining slough physical habitat variables. Sheet 2 of3 Table A-3 (Cont1d) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 9 Average Velocity Wetted Perimeter Sus itna River Wetted Discharge at Mid-Upstream Surface Mid-Upstream Gold Creek Mouth Slough End Area Mouth Slough End (cfs)(ft/sec)(ftlsec)(ft/sec)(ft2)(ft )(ft)(ft ) 1,000 0.8 0.1 N/A 130,000 27 89 0 3,000 0.8 0.1 N/A 130,000 27 89 0 5,000 0.8 0.1 N/A 130,000 27 89 0 7,000 0.8 0.1 N/A 130,000 27 89 0 9,000 0.8 0.1 N/A 130,000 27 89 0 11,000 0.8 0.1 N/A 130,000 27 89 0 12,000 0.8 0.1 N/A 230,000 29 89 0 +:>13,000 0.5 0.1 N/A 300,000 33 89 0 I 15,000 0.2 0.1 N/A 390,000 48 89 0lT1 17,000 0.1 0.1 N/A 470,000 78 89 0 19,000 0.1 0.1 N/A 530,000 145 89 0 21,000 0.1 0.4 0.4 590,000 185 96 50 23,000 0.3 0.8 1.0 640,000 193 117 80 25,000 0.5 1.0 1.4 690,000 193 136 100 27,000 0.6 1.3 1.5 740,000 194 148 150 29,000 0.7 1.4 1.5 780,000 195 150 220 31,000 0.7 1.4 1.5 820,000 195 152 290 N/A -Not Applicable Note:See Figure A-3 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 2,for narrative and worksheets explaining method of determining slough physical habitat variables. ,!<J J ..l ~J J J I l ,.~]J - Sheet 3 of 3 Table A-3 (Cont'd) MAINSTEI~DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 9 Water Table Elevation Susitna River Mid- Discharge at Slough Upstream Upstream Gold Creek Well Well A We 11 B (cfs)(ft,msl)(ft,msl) (ft,msl) 1,000 593.3 599.3 602.9 3,000 593.3 599.5 603.1 5,000 593.5 599.6 603.2 7,000 593.6 599.8 603.3 9,000 593.7 600.0 603.5 11,000 593.8 600.2 603.5 12,000 593.9 600.3 603.6 13,000 594.0 600.4 603.7 15,000 594.1 600.5 603.8 17,000 594.2 600.6 603.9 19,000 594.3 600.8 604.0 21,000 594.5 601.0 604.1 23,000 594.6 601.2 604.3 25,000 594.7 601.5 604.4 27,000 594.9 601.6 604.5 29,000 595.0 601.8 604.6 31,000 595.1 602.0 604.8 N/A -Not Applicable Note:See Figure A-3 farwell locations. See Attachment,Part 2,for narrative and worksheets explaining method of determining water table elevations. 4-6 Sheet 1 of 3 Table A-4 MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 21 Water Surface Elevation Flow Depth .Susitna River Slough·Inter-Inter- Di scharge.at Discharge Mid-.mediate Highest Mid-mediate Upstream Gold Creek at Mouth Mouth Slough Berm Berm Mouth Slough Berm Berm (cfs)(cfs)(ft~msl)(ft~msl)(ft~msl)(ft~msl)(ft )(ft )(ft)(ft) 1~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 3~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 5~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 7~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 9~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 11 ~OOO 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 12~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 .t::o 13,000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 I 15~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0-....J 17~000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 19,000 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 21~OOO 5 744.7 744.9 N/A N/A 1.6 0.6 0 0 23,000 9 744.8 745.1 N/A N/A 1.6 0.7 0 0 25,000 9 745.0 745.1 754.6 N/A 1.9 0.7 0.01-/o . 27~000 12 745.3 745.3 754.8 755.5 2.2 0.9 0.2 0.01-/ 29,000 19 745.6 745.8 755.1 755.6 2.5 1.4 0.5 0.1 31,000 34 746.0 746.3 755.5 755.6 2.9 2.0 0.9 0.1 N/A -Not Applicable Note:See Figure A-4 for location of mouth,mid-slough,intermediate berm,and upstream berm. See Attachment,Part 3,for narrative and worksheets explaining method of determining slough physical habitat variables. l./Flow depth is less than 0.05 ft. I I J ••J >J •,.......1 .1 }J ~I I 1 1 )")')~I "'',J '}1 _..-1 i A Sheet 2 of 3 Table A-4 (Cont'd} MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES SLOUGH 21 Average Velocity Wetted Perimeter Susitna River Inter-Wetted Inter- Di scharge at Mid-mediate Upstream Surface Mid-mediate Upstream Gold Creek Mouth Slough Berm Berm Area Mouth SlOU 5h Berm Berm (cfs)(ft/sec) (ft/sec)(ftlsec)(ft!sec)(ft2)(ft)(ft (ft )(ft ) 1,000 0.1 0.5 N/A N/A 46,000 50 25 a a 3,000 0.1 0.5 N/A N/A 46,000 50 25 a a 5,000 0.1 0.5 N/A N/A 46,000 50 25 a a 7,000 0.1 0.5 N/A N/A 46,000 50 25 a a 9,000 0.1 0.5 N/A N/A 46,000 50 25 a a ll,000 0.1 0.5 N/A N/A 46,000 50 25 a a 12,000 0.1 0.5 N/A N/A 46,000 50 25 a a 13,000 0.1 0.5 N/A N/A 46,000 50 25 a a +::0 15,000 0.1 0.5 N/A N/A 46,000 50 25 a aIco17,000 0.1 0.5 N/A N/A 46,000 50 25 a a 19,000 0.1 0.5 N/A N/A 46,000 50 25 a a 21,000 0.1 0.5 N/A N/A 46,000 50 25 a a 23,000 0.2 0~7 N/A 1/N/A 115,000 98 26 a a 25,000 0.1 0.7 0.0-:-:N/A 155,000 101 26 3 a 27,000 0.1 0.7 1.4 -180,000 103 36 24 4 29,000 0.2 0.7 1.4 -200,000 105 45 44 12 31,000 0.2 0.8 1.0 -220,000 108 55 65 20 N/A -Not Applicable Note:See Figure A-4 for.location of mouth,mid-slough,intermediate berm,and upstream berm. See Attachment,Part 3,for narrative and worksheets explaining method of determining slough physical habitat variables. l/Velocity is less than 0.05 ft/sec. !i Sheet 3 of 3 Table A-4 (Cont'dJ MAINSTEM DISCHARGE VS~PHYSICAL HABITAT VARIABLES SLOUGH 21 Water Table Elevation Susitna River Discharge at Gold Creek (cfs) 1,000 3,000 5,000 7,000 9,000 11,000 12,000 13,000 15,000 17,000 19,000 21,000 23,000 25,000 27,000 29,000 31,000 (ft,ms1)(ft ,ms 1) 1/ (ft,ms 1) 1/No well data available for Slough 21;for a description of expected water table conditions in Slough 21,see Attachment, Part 3. 4-9 -, Condition 3:A high flow range at Rabideux Slough was derived from the sum of the 10 percent exceedance flows from the Chulitna and Talkeetna Rivers on a daily basis during the month of June,which is typically the high flow month of the year. The range of flows at Gold Creek were added incrementally to this sum to provide the high range of flows at Rabideux Slough.. The results of the analyses of the effects of mainstem flow on the hydraulic characteristics of Rabideux Slough are presented in Table A-5 for the three flow conditions and result in a total range of flows at Rabideux Slough from 10,000 cfs to 85.000 cfs.Discussion of the methods used in the analyses for Rabideux Slough are presented in the Attachment.Part 4. A.5 Summary of Methods of Analyses This section contains a summary of the methods used to derive the following parameters: a a a a a o a a slough discharge threshold discharges water surface elevation fl ow depth vel oc ity wetted surface area wetted perimeter water table elevation. Since the methods vary among the sloughs.a separate summary is given for each.More detailed descriptions are found in the attachment for Slpughs 8A.9.and 21 and Rabideux Slough. The slough physical parameters given in Tables A-2 through A-5 should be considered estimates of the average values.Slough discharge is .influenced by mainstem water level effects on groundwater upwell-ing. local runoff.and regional groundwater.For this reason field measure- ments of the relations between slough discharges and Susitna River mainstem discharges showed considerable variability i~all Regimes but especially in Regimes I and II.To simplify the analyses a constant slough discharge was assumed for each slough for each of Regimes I and II. A.5.1 Slough 8A A map of Slough 8A is shown on Figure A-2.Methods of analyses are given in the Attachment,Part 1~ Threshold Discharges The threshold Susitna River discharge for overtopping the upstream berm (30.000 cfs to 32.000 cfs)was estimated from aerial photography of the 5 Sheet 1 of 16 Table A-5 MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH ~, Susitna River C dO 0 11/C dOt O 21/dOt 0 31/on ltlOn -on 1 lOn -Can 1 lOn - Oi scharge at Mainstem Slough Mainstem Slough Ma i nstem Slough <~Go ld Creek Discharge Discharge Discharge Di scharge Discharge Discharge Ccfs)Ccfs)Ccfs)(cfs)(cfs)Ccfs)Ccfs) 1,000 10,000 °'31,000 °55,000 0 3,000 12,000 0 33,000 0 57,000 0 5,000 14,000 0 35,000 0 59,000 0 7,000 16,000 0 37,000 0 61,000 0 9,000 18,000 °39,000 0 63,000 0 11,000 20,000 0 41,000 0 65,000 0 -,12,000 21,000 0 42,000 0 66,000 8 13,000 22,000 0 43,000 0 67,000 20 15,000 24,000 °45,000 °69,000 60 17,000 26,000 0 47,000 0 71,000 108 19,000 28,000 °49,000 0 73,000 165 21,000 30,000 °51,000 °75,000 230 ~. 23,000 32,000 °53,000 °77,000 300 25,000 34,000 °55,000 °79,000 380 27,000 36,000 °57,000 °81,000 468 !O!'I>., 29,000 38,000 °59,000 °83,000 560 31,000 40,000 °61,000 °85,000 660 .!.!See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,narrative and worksheets explaining method of determining slough physical habitat variables. 5-1 - ..- I Sheet 2 of 16 Table A-5 (conit)0 MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH Condition 1Y -d't-'2 1/Can 1 lon -Cond it i on 3Y Susitna River Discharge at Gold Creek (cfs) -1,000 3,000 . 5,000 7,000 9,000 11,000 12,000 13,000 15,000 17,000 19,000 21,000 23,000 25,000 27,000 29,000 31,000 Mainstem Discharge (cfs) 10,000 12,000 14,000 16,000 18,000 20,000 21,000 22,000 24,000 26,000 28,000 30,000 32,000 34,000 36,000 38,000 40,000 Water- Surface Elevation at Mouth (ft,msl) 255.3 255.5 255.8 256.0 256.3 256.5 256.6 256.8 257.° 257.3 257.5 257.8 258.0 258.3 258.5 258.8 259.° Mainstem Discharge (cfs) 31,000 33,000 35,000 37,000 39,000 41,000 42,000 43,000 45,000 47,000 49,000 51,000 53,000 55,000 57,000 59,000 61,000 Water- Surface Elevation at Mouth (ft,ms 1) 257.8 258.2 258.4 258.7 258.9 259.1 259.2 259.3 259.5 259.8 260.0- 260.1 260.3 260.5 260.7 260.9 261.° Mainstem Discharge (cfs) 55,000 57,000 59,000 61,000 63,000 65,000 66,000 67,000 69,000 71,000 73,000 75,000 77,000 79,000 81,000 83,000 85,000 Water- Surface Elevation -at Mouth (ft,ms1) 260.5 260.7 260.9 261.0 261.2 261.4 261.5 261.6 261.7 261.9 262.1 262.3 262.5 262.7 262.8 263.0 263.2 l/See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. -See Attachment,Part 4,for narrative and worksheets explaining method of ,-determining slough physical habitat variables. ,F""'_ 5-2 I i """', Sheet 3 of 16 ~ Table A-5 (con1t) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH ~ Cond it i on 1-1'Cond it i on 21/Cond it i on J~j Water-Water-Water-*Surface Surface Surface Sus it na Ri ver Elevation E1ev at ion Elevation Discharge at Mainstem at Mainstem at 1Vlainstem at ....", Gold Creek Discharge Mid-Slough Discharge Mid-Slough Discharge r~id-Slough (cfs)(cfs)(ft ~ms 1)(cfs)(ft ~ms 1)(cfs)(ft~msl) 1~000 10~000 N/A'l:/31 ~000 260.3 55~000 260.6 3~000 12~000 I~/A 33~000 260.3 57~000 260.7 ~f5~OOO 14,000 N/A 35,000 260.3 59~000 260.9 7,000 16~000 N/A 37~000 260.3 61,000 .261.0 9~000 18~000 N/A 39 ~000 260.3 63~00O 261.2 11,000 20~00O N/A 41~000 260.3 65~OOO 261.4 12~000 21~000 N/A 42 ~000 260.3 66~000 261.5 13,000 22~000 N/A .43,000 260.3 67~000 261.6 15~OOO 24~000 N/A 45~000 260.3 69,000 261.7 17 ~000 26~000 260.3 47~000 260.3 71 ~000 261.9 19,000 28~OOO 260.3 49~000 260.3 73~000 262.1 21,000 30,000 260.3 51,000 260.3 75~000 262.3 23~OOO 32~000 260.3 53~000 260.3 77,000 262.6 25,000 34,000 260.3 55~000 260.5 79,000 262.9 lI!J!!I. 27~000 36,000 260.3 57~000 260.7 81,000 263.2 29,000 38~000 260.3 59~OOO 260.9 83,000 263.4 31~000 40,000 260.3 61,000 261.0 85,000 263.7 J""'; y See last page of this table for explanation of conditions. ~/Transect 7 reported as dry at discharge of 25,800 cfs (ADF&G 1982) Note:See Figure A-5 for location of mouth,mid-slough~and upstream berm. See Attachment,Part 4~for narrative and worksheets explaining method of determining slough physical habitat variables~ 5-3 .... Sheet 4 of 16 IF'" Table A-5 (can't) 1-Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-4 I I 11 See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-5 ~ ,:1 (~ ,"'. Sheet 6 of 16 Table A-5 (con't) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH Condition 11/Condition 2.!/Condition J!'! Susitna River Flow Depth Flow Depth Flow Depth Discharge at Mainstem at Mainstem at Mai nstem at Gold Creek Discharge Mid-slough Discharge Mid-s lough Discharge Mid-slough (cfs) (cfs)(ft)(cfs)(ft)(cfs)(ft) 1,000 10,000 o ~I 31,000 0.3 55,000 0.5 3,000 12,000 0 33,000 0.3 57,000 0.7 5,000 14,000 0 35,000 0.3 .59,000 0.9 7,000 16,000 0 37,000 0.3 61,000 1.0 9,000 18,000 0 39,000 0.3 63,000 1.2 11,000 20,000 a 41,000 0.3 65,000 104 12,000 21,000 0 42,000 0.3 66,000 1.5 13,000 22,000 0 43,000 0.3 67,000 1.6 15,000 24,000 0 45,000 0.3 69,000 1.7 17,000 26,000 0.3 47,000 0.3 71,000 1.9 19,000 28,000 0.3 49,000 0.3 73,000 2.1 21,000 30,000 0.3 51,000 0.3 75,000 2.3 23,000 32,000 0.3 53,000 0.3 77 ,000 2.6 .25,000 34,000 0.3 55,000 .0.5 79,000 2.9 27,000 36,000 0.3 57,000 0.7 81,000 3.2 29,000 38,000 0.3 59,000 0.9 83,000 3.4 31,000 40,000 0.3 61,000 1.0 85,000 3.7 1/See last page of this table for explanation of conditions. ~/Transect 7 reported as dry for discharge of 25,800 cfs (ADF&G,1982). Note:See Figure A-5 for location of mouth,niid-:slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-6 I I Sheet 7 of 16 Table A-5(con 1 t) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH !""" Condition 1-1/Cond it ion 201/~dOt"31/L.on 1 lOn ~ Flow Depth Flow Depth Flow Depth Sus itna River at at at Di scharge at Mainstem Upstream Mainstem Upstream Mainstem Upstream Gold Creek Discharge Berm Discharge Berm Discharqe Berm """"(cfs)(cfs)(ft)(cf's)(ft)(cfs)(ft) 1,000 10,000'0 31,000 0 55,000 a ....... 3,000 12,000 a 33,000 0 57,000 a 5,000 14,000 a 35,000 0 59,000 0 7,000 16,000 a 37,000 a 61,000 0 9,000 18,000 0 39,000 0 63,000 0 11,000 20,000 0 41,000 a 65,000·a 12,000 21,000 0 42,000 0 66,000 0.3 ·~l 13,000 22,000 0 43,000 0 67,000 0.4 15,000 24,000 0 45,000 0 69,000 0.5 17 ,000 26,000 0 47,000 0 71,000 0.6 """.19,000 28,000 0 49,000 0 73,000 0.6 21,000 30,000 a 51,000 0 75,000 0.7 23,000 32,000 .0 53,000 0 77 ,000 0.7 !~1 25,000 34,000 0 55,000 0 79,000 0.8 27,000 36,000 0 57,000 0 81,000 0.9 29,000 38,000 0 59,000 0 83,000 1.0 -, 31,000 40,000 0 61,000 0 85,000 1.3 11 See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. .- 5-7 F'· II See last page'of this table for explanation of conditions. 21 Velocity is less than 0.05 ft/sec. Note:See Figure A-5 fo~location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-8 I I """\ Sheet 9 of 16 -- Table A-5 (con1t) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES ....., RAB IDEUX SLOUGH Condition 1Y Cond it i on 2Y Cd"31/on ltlon - Average Average Average Sus itna Ri ver Ve lac ity Ve 1ocity Ve lac ity Discharge at Mainstem at Mainstem at Mainstem at Gold Creek Discharge Mid-Slough Discharge Mid-Slough Discharge Mid-Slough (cfs)(cfs)(ft/sec)(cfs)(ft/sec)(cfs)(ft/sec) 1,000 10,000 0 31,000 0 55,000 0 3,000 12,000 0 33,000 0 57,000 0 5,000 14,000 0 35,000 0 59,000 0 7,000 16,000 0 37,000 0 61,000 0 9,000 18,000 0 39,000 0 63,000 0 11,000 20,000 0 41,000 0 65,000 0 12,000 21,000 0 42,000 0 66,000 0.3 13,000 22,000 0 43,000 0 67,000 0.5 ,,..,,, 15,000 24,000 0 45,000 0 69,000 0.9 17 ,000 26,000 0 47,000 °71,000 1.1 19,000 28,000 0 49,000 0 73,000 1.3 21,000 30,000 0 51,000 0 75,000 1.3 23,000 32,000 0 53,000 0 77 ,000 1.3 25,000 34,000 0 55,000 0 79,000 1.2 27,000 36,000 ,0 57,000 0 81,000 1.2 29,000 38,000 0 59,000 0 83,000 1.2 31,000 40,000 0 61,000 0 85,000 1.2 1/See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-9 ,I"'" Table A-5 (con1t) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH Sheet 10 of 16 d"11/Cond it ion 2.!!Condition 3.!!Con ltlon -, Average Average Average t-Velocity Vel oc ity Ve loci ty Susitna River at at at Discharge at Mainstem Upstream Mainstem Upstream Mains tern Upstream Gold Creek Discharge Berm Discharge Berm Discharge Berm (cfs),(cfs)(ft/sec)(cfs)(ft/sec)(cfs)(ft/sec) 1,000 10,000 N/A 31,000 N/A 55,000 N/A 3,000 12,000 N/A 33,000 N/A 57,000 N/A 5,000 14,000 N/A 35,000 N/A 59,000 N/A f~7,000 16,000 N/A 37,000 N/A 61,000 N/A 9,000 18,000 N/A 39,000 N/A 63,000 N/A 11,000 20,000 N/A 41,000 N/A 65,000 N/A f!"'"12,000 21,000 N/A 42,000 N/A 66,000 1.3 13,000 22,000 N/A 43,000 N/A 67,000 1.4 15,000 24,000 N/A 45,000,N/A 69,000 1.6 17,000 26,000 N/A 47,000 N/A 71,000 1.7 19,000 28,000 N/A 49,000 N/A 73,000 1.7 21,000 30,000 N/A 51,000 N/A 75,000 1.8 23,000 32,000 N/A 53,000 N/A 77 ,000 1.9 25,000 34,000 N/A 55,000 N/A 79,000 1.9 27,000 36,000 N/A 57,000 N/A 81,000 1.8 r 29,000 38,000 N/A 59,000 N/A 83,000 1.6 31,000 40,000 N/A 61,000 N/A 85,000 1.4 N/A -Not Applicable ,...1/See last page of this table for explanation of conuitions. Note:See Fi gureA-5 for 1ocat ion of mouth,mid-slough,and upstream berm. ,/'"""See Attachment,Part 4,for narrative and worksheets explaini~g method of determining slough physical habitat variables. ,r- 5-10 1/See last page of this table for explanation of conditions. Note:See Figure A~5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables. 5-11 .,'-" 1/See 1ast page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determining slough physical habitat variables . 5-12 II Sheet 13 of 16 ;l"'!!" Table A-5 (can't) ~ MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES I .RABIDEUX SLOUGH d <<111 dOt'211 Cd'0 3 11Can,tlOn -Can , ,on -.on ,t,on - Wetted Wetted Wetted Susitna River Perimeter Perimeter Perimeter Di scharge at Mai nstem at Mainstem at Mainstem at Gold Creek Discharge Mi d-S laugh Discharge Mid-Slough Discharge Mid-Slough A 1,000 10,000 rJ-I 31,000 12 55,000 16 3,000 12,000 o?!33,000 12 57,000 22 5,000 14,000 rJj 35,000 12 59,000 24 7,000 16,000 ~I 37,000 12 61,000 25 9,000 18,000 r#39,000 12 63,000 26 -, 11,000 20,000 r#41,000 12 65,000 28 12,000 21,000 ril 42,000 12 66,000 29 13,000 22,000 ri l 43,000 12 67,000 30 ...... 15,000 24,000 fil 45,000 12 69,000 30 17,000 26,000 12 47,000 12 71,000 31 19,000 28,000 12 49,000 12 73,000 32 """21,000 30,000 12 51,000 12 75,000 33 23,000 32,000 12 53,000 12 77 ,000 35 25,000 34,000 12 55,000 16 79,000 210 27,000 36,000 12 57,000 22 81,000 3UO 29,000 38,000 12 59,000 24 83,000 310 31,000 40,000 12 61,000 25 85,000 310 11 See last page of this table for explanation of conditions. lJ Transect 7 reported as dry at discharge of 25,800 cfs (ADF&G,1982). ~Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method 6f determining slough physical habitat variables. ""1 5-13 ~­ ,I Sheet 14 of 16 1/See last page of this table for explanation of conditions. Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,fornarratfve and worksheets explaining method of determining slough physical habitat variables. 5-14 I I Sheet 15 of 16 Table A-5 (con1t) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RAB IDEUX SLOUGH Condition 11:/Condition 21:/Condition 31:/ Susitna River Discharge at Gold Creek (cfs) Mainstem Discharge (cfs) Water Table Elevation (ft ,ms 1) IVlainstem Discharge (cfs) Water Table Elevation (ft,msl) Mainstem Discharge (cfs) Water Table Elevation (ft,msl) 1,000 3,000 5,000 7,000 9,000 11,000 12,000 13,000 15,000 17,000 19,000 21,000 23,000 25,000 27,000 29,000 31,000 10,000 31,000 55,000 12,000 33,000 57,000 14,000 35,000 59,000 16,000 37,000 61,000 18,000 39,000 63,000 20,000 41,000 65,000 21,000 42,000 66,000 22,000 2/43,000 2/67,000 2/ 24,000 45,000 69,000 26,000 47,000 71,000 28,000 49,000 73,000 30,000 51,000 75,000 32,000 53,000 77,000 34,000 55,000 79,000 36,000 57,000.81,000 38,000 59,000 83,000 40,000 61,000 85,000 -1:/See last page of this table for explanation of conditions. 2/No well data avaible for Rabideux Slough;for a description of expected water table conditions,see Attachment A-4.~ Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of .~ determining slough physical habitat variables. -., 5-15 Sheet 16 of 16 Table A-5 (can't) MAINSTEM DISCHARGE VS.PHYSICAL HABITAT VARIABLES RABIDEUX SLOUGH Mainstem Discharge =QGC +QC +0T in which, QGC = QC = QT =.-Cond it ion 1: Susitna River at Gold Creek (USGS Gage No.15292000)discharge Chulitna River near Talkeetn~(USGS Gage No.15292400)discharge Talkeetna River near Talkeetna (USGS Gage No.15292700)discharge QGC = r'.QC = °T = 1,000 to 31,000 cfs in 2000 cfs increments 90%exceeded flow during the month of September 90%exceeded flow during the month of September Condition 2: QGC =1,000 to 31,000 cfs in 2000 cfs increments QC =average monthly flow in August 0T =average monthly flow in August f"'"Condition 3: QGC =1,000 to 31,000cfs in 2000 cfs increments 0c =10%exceeded flow during the month of June' 0T =10%exceeded.flow during the month of June Note:See Figure A-5 for location of mouth,mid-slough,and upstream berm. See Attachment,Part 4,for narrative and worksheets explaining method of determinihg slough physical habitat variables. 5-16 - ~, slough at a Susitna River discharge (measured at Gold Creek)of 31,100 cfs.The threshold discharge for overtopping the intermediate berm (29,000 cfs)was estimated by comparing computed and/observed Susitna River water surface elevations with the berm crest elevation.'The threshold discharge between Regimes I and II (10,000 cfs)was estimated from field observations. Slough Discharge Slough discharges were estimated to be 3 cfs for Regime I and 8 cfs in Regime II based on field measurements (ADF&G,1982).Slough discharge for Regime IIA was estimated by computing discharge over the interme- diate berm and adding this to Regime II discharge. Water Surface Elevation Water surface el evat ions at the slough mouth are based on a rating curve developed from staff gage readings between 11~500 cfs and 26,500 cfs.Between 10,000 cfs and 11,500 cfs,and between 26,500 cfs and 31,000 cfs,the rating curve was extrapolated.Hydraulic computa- tions,assuming uniform flow,were made to estimate slough mouth water surface elevations for discharges less than 10,000 cfs. Mid-slough water surface elevations are based on in-field measurements for mainstem discharges which exceed 10,000 cfs.For mainstem dis- charges less than 10,000 cfs~hydraulic computations were made. Water surface elevations at the intermediate and upstream berms were estimated using broad crested weir computations. Flow Depth Flow depths w~re computed by subtracting thalweg elevations from water surface elevations~determined as described above. Velocity Average slough flow velocities were computed by dividing the slough discharges by flow cross-sectional areas.Lateral distributions of velocity-were measured at cross sections about 1600 feet upstream of the slough mouth and are shown in the Attachment. Wetted Surface Area For ma i nstem discharges greater than 10,OOOcfs,wetted surfacE:!areas were estimated using aerial photographs for mainstem discharges greater than 10,000 cfs.For mainstem discharges less than 10,000 cfs the wetted surface area was estimated using computeds lough water surface profil es and surveyed cross sections. 6 Wetted Perimeter Wetted perimeters at the slough mouth,mid-slough,and the intermediate berm were measured from the surveyed cross sections and the water surface elevations determined as described previously.. Water Table Elevations Water table elevations were derived from data collected at observation wells in the slough. A.5.2 Slo~gh ~ A map of Slough 9 is shown on Figure A-3.Methods of analyses are given in the Attachment,Part 2. Threshold Discharges The threshold Susitna River mainstem discharges between Reg'ilile I and Regime II (11,000 cfs)and between Regime.II and·Regime III (20,500 cfs)are based on plots of measured mainstem and slough discharges. Slough Discharge The slough discharges are based on the same field measurements as for Threshold Discharges. Water Surface Elevation Slough mouth water surface elevations are based on staff gage readings for mainstem discharges greater than 11,000 cfs.For mainstem dis- charges less than 11,000 cfs,the slough mouth water surface elevation was assumed constant.This water surface elevation reflects an esti- mate of flow depth at staff gage 129.0 for a mainstem discharge of 10,000 cfs and a slough discharge of 3cfs (Trihey,1982,Table 4,p. 21)• All mid-slough water surface elevations are based on a rating curve derived from staff gage readings.Upstream end water surface eleva- tions are based on water surface profiles computed with the U.S.Army Corps of Engineers computer program for water surface profiles,HEC-2. Flow Depth Flow depths were computed by subtracting the thalweg elevations from water surface elevations determined as described above. Velocity Average slough flow velocites were determined by dividing slough dis- charge by the flow cross sectional areas.Lateral and longitudinal distributions of velocities obtained in the field are shown in the Attachment. 7 - - ..- i Wetted Surface Area For mainstem discharges greater than 11,000 cfs,wetted surface areas were estimated from aeri a 1 photography.For ma i nstem discharges 1ess than 11,000 cfs,the wetted surface area was estimated using computed slough water surface profiles and surveyed cross sections.. Wetted Perimeter Wetted perimeters were·estimated to be equal to wetted surface widths (top widths)for the slough mouth and the upstream end of this slough. Top wi dths were estimated from aeri a 1 photos and computed s laugh water surface profi les and surveyed cross sections.Wetted perimeters were computed from surveyed cross sections for mid-slough. Water Table Elevations Water ta~le elevations were derived from data collected at observation wells in the slough. A.5.3 Slough..?l A map of Slough 21 is shown on Figure A-4.Methods of analyses are given in the Attachment,Part 1. Threshold Discharges The threshold Susitna River mainstem discharges between Regimes II-A and III (26,000 cfs)and between .Regimes I and I I (21,300 cfs)are based on field measurements of slough and mainstem discharge. Slough Discharges Slough di scharge est imates are based on the same fi e 1d measurements indicated in the preceding paragraph. Water Surface Elevation For mainstem discharges greater than 21,300 cfs,water surface eleva- tions at the slough mouth are based on a rating curve derived from staff gage readings.A constant water surface elevation at the slough mouth was assumed for all mainstem discharges less than 21,300 cfs. Mid-slough water surface elevations were estimated from staff gage readings and average daily elevations from a stage recorder.Constant water levels were assumed for Regimes I,II,and II-A. Intermediate and upstream berm water levels were estimated from staff gage readings. 8 Flow Depths Slough flow depths were estimated by subtracting the thalweg elevation from water sDrface elevations determined as described above. Vel oc ity Average slough flow velocities were estimated by dividing slough discharges by flow cross sectional areas.Average velocities for four measured flows are shown in the Attachment.Lateral and longitudinal distributions of velocities obtained in the field are shown in the Attachment. Wetted Surface Area Slough wetted surface areas were estimated from aerial photography. Wetted Perimeter Slough wetted perimeters were assumed to be equal to wetted surface width (top widths)based on aerial photography and field measurements. Water Table Elevations There is not sufficient information to estimate the water table level at this slough since wells have not been installed.Geologic materials are expected to De similar to sloughs 8A and 9. A.5.4 Rabideux Slough A map of Rabideux Slough is shown on Figure A-5.Methods of analyses for this slough are presented in the Attachment,Part 4. Threshold Discharges There is very little flow in this slough until the upstream berm is overtopped (Susitna River mainstem discharge 66,000 cfs). Slough Discharges Slough discharge estimates are based on four field observations.Two observations of slough discharge when the upstream berm was not overtopped (Regime II)indicated negligible flow in this slough.Two observati ons of slough di scharge when the upstream berm was overtopped were used to estimate slough discharge in Regime III. Water Surface Elevations Water surface elevations at the slough mouth are based on staff gage readings and a surveyed water surface level.Mid-slough water surface levels are based on surveyed water levels and measurements of top 9 - widths from aeri a1 photography projected on surveyed cross sections. The transect at mid-slough has been observed to be dry at a mainstem discharge of 25,800 cfs.Mid-slough water levels are influenced by water levels at the mouth for mainstem discharges greater than 53,000 cfs.Upstream berm water surface levels were estimated from hydraulic computations assuming a triangular broad crested weir. Flow Depths Slough flow depths were determined by subtracting the slough thalweg elevations from water surface elevations derived as described above. Vel oc ity Average slough flow velocity was computed by dividing slough discharge by the slough cross sectional area.Lateral and longitudinal distribu- tions of velocities as measured in the field are shown in the Attach- ment. Wetted Surface Area Wetted surface areas were estimated from aerial photography. Wetted Perimeter Wetted perimeters were estimated from field surveyed cross sections at the slough mouth and·mid-slough.Wetted perimeters were estimated to be equal to wetted surface wi dths (top wi dths)measured from aeri a 1 photography at the upstream berm. Water Table Elevations There is not enough information to estimate water table levels at this slough since wens have not been installed.However,groundwater levels are expected to respond in a manner similar to sloughs upstream of Talkeetna (Sloughs 8A and 9), A.6 Discussion of Results The following discussion refers to the results presented in Tables A-I through A-5 .. A.6.1 S 10 ug h 8A A summary of the results for Slough SA is presented in Table A-2. Regime II occurs over a mainstem flow range of 10,000 to 26,000 cfs. and thus is the dominant regime characterizing Slough SA in the range of incremental flows analyzed.Intermediate and upstream berms are not overtopped unt il ma i nstem fl ows have reached 26.000 and 30.000-32,000 cfs.respectively (Table A-I). 10 Slough discharges are generally low at mainstem flows less than the overtopping discharge and vary between 3 and 20 cfs.A correlation of slough flows with mainstem flows at less than overtopping discharges is not apparent at this level of analy~is,perhaps because of local runoff and groundwater inflow from upland areas.Therefore,constant slough flows of 3 and 8 cfs were assumed for Regimes I and II,respectively. In Regime I,water surface elevations at the slough mouth are con- trolled by a berm downstream of the mouth.Hence,for the 3 cfs dis- charge the water surface elevation at the mouth remains constant.In Regime II,water surface elevations and depth at the slough mouth in- crease as Susitna River flows increase because of a backwater effect. The depths presented in Table A-2 represent maximum depths at cross- section WI (see Figure A-2).For Regime 1,the depth at the controll- ing berm downstream of cross-section WI is estimated to be 0.1 ft. For all regimes,the water surface elevations and depths at mid-slough are dependent on slough discharge.At the upstream berms,depths are zero until the berms are overtopped. At mainstem flows less than 29,000 cfs,average velocities in the slough are low because of the low slough discharges. Wetted surface area is constant for all mainstem flows in Regime I.As higher mainstem flows increase the backwater effect of Regime II,wett- ed surface area increases.Wetted perimeter at the mouth also in- creases as mainstem flows in Regime II increase. Groundwater elevations at mid-slollgh,Well A,do not appear to be significantly correlated with mainstem discharge.At mid-slough,Well B,and the upstream well,there is a direct relationship with mainstem discharge.This relationship is depicted on Sheet 3 of Table A-2. Slough 2 Summary information for Slough 9 is presented in Table A-3. For Regime I (mainstem flow less than 11,000 cfs)and Regime II (11,000 to 20,500 cfs),there is little variation in sloDgh discharge.Hence, based on observed data,constant slough discharges of 3 cfs and 6 cfs were assumed for Regimes I and II,respectively.At discharges greater than the upstream berm overtopping discharge (Regime III),slough dis- charge increases with mainstem discharge.Regime III slough discharges presented in Table A-3 represent values estimated from a plot of the observed data. In Regime I,water surface elevations at the mouth of Slough 9 are con- trolled by a berm downstream of the mouth.For the assumed 3 cfs slough discharge,the water surface elevation remains constant.At 3 cfs,the depth over the berm is computed to be 0.1 feet.In Regimes II and III,the water surface elevations and depths at the mouth of the slough increase with increasing mainstem discharge. 11 - .,.. 'I, I~ The mid-slough water surface elevations and depths shown in Table A-3 are at a mid-slough pool.The water surface elevations and depths are essentially independent of mainstem discharges for Regime I and II. However,when the upstream berm·is overtopped,the increase ins laugh discharge results in an increase in water surface elevation and depth. Once overtopped,the water surface el evat ions at the upstream berm increase directly with mainstem Susitna water surface elevations. The average velocities presented for the mouth of Slough 9 are the velocities over the berm at the slough mouth.Since the cross section- al area at the berm is a minimum,velocities are higher than for any other cross section near the mouth.Mid-slough velocities are low throughout Regimes I and II but increase when the upstream berm is overtopped. The wetted surface area remains constant throughout Regime L However, in Regime II,as the backwater from the mainstem increases with increasing SusitnaRiver discharge,the wetted surface area increases. The wetted perimeter at the mouth is constant through Regime I and increases through Regimes II and III.Mid-slough and upstream berm wetted perimeters do not change until overtopping occurs. Water table elevations at Slough·9 presented in Table A-3 exhibit considerably more change with mainstem discharge than do those pre- sented for Slough 8A (see Table A-2). Slough 21 Summary information for Slough 21 is contained in TableA-4. Regime I flow at Slough 21 ihcludes flows up to a mainstem discharge of 21,400 cfs .Regime II flow occurs avera range of discharges from 21,400 cfs to 24,800 cfs.Regime II-A,resulting from overtopping of the·intermediate berm,occurs during mainstem flows of 24,800 cfs to 26,000 cfs and Regime III occurs when the highest berm is overtopped at 26,000 cfs. Slough discharges measured during Regime I flows were low,varying between 2 and 12 cfs.Since there is no apparent correlation with mainstem discharge,a constant slough flow of 5 cfs was assumed (see Table A-4).For Regime II,at mainstem flows between 23,000 and 25,000 cfs,a slough discharge of 9 cfs was assumed.For Regime III,a relationship based on observed data was used to estimate slough dis- charge. As a result of the assumed constant slough flow for Regime I,the water surface elevation and slough depth at the mouth are constant.The depths presented reflect a pool depth upstream from the cantrall i ng berm and not the depths over the berm.As backwater effects and over- topping of the upstream berms begin,the water surface elevations and depths increase. 12 At mid-slough,the water surface elevation (and depth)is constant throughout Regime I.As slough discharge increases from 5 to 9 cfs, (Regime I to Regime II),there is a slight increase in water surface elevation (and depth).The increase at mid-slough is attrioutable to the increase in discharge since the backwater effects do not extend upstream to the mid-slough location. Average velocities throughout all flow regimes and for all locations analyzed,remain low.As illustrated in Table A-4,velocities at the slough mouth do not exceed 0.2 feet per second for the range of flows considered. In Table A-4,wetted surface area begins to increase due to backwater (Regime II)at a mainstem flow of 21,400 cfs.At flows higher than 26,000 cfs,the increases in wetted surface area are the result of both backwater and upstream berm overtopping. Wetted perimeter at the mouth responds to mainstem flow in a mann-er similar to wetted surface area.The wetted perimeter at the mid-slough is essentially constant until the upstream berm is overtopped.- ~o groundwater elevation data is available for Slough 21. Rabideux Slough Summary _information for Rabideux Slough is contained in Table A-5 (Sheets 1 through 16). Rabi deux Slough is affected by the backwater from the Sus itn a Ri ver (Regime II)at mainstem flow conditions (at the sloL1gh)as low as approximately 10,000 cfs.This regime persists until the upstream berm is overtopped at a mainstem flow of approximately 65,000 cfs. Measured slough discharges at flows less than the overtopping discharge were eithe~not measurable or were less than 1 cfs.Therefore,slough discharge was assumed to _be zero for Regime II.However,once over- topped,Rabideux Slough discharge increases significantly. Water surface elevation (Table A-5,Sheet 2)and depth (Table A-5, Sheet 5)at the slough mouth increase with mainstem discharge over the range of flows considered.' The selected mid-slough location is dewatered at flows less than 26,000 cfs (Table A-5,Sheets 3 and 6).At hi gher fl ows,i so 1ated ponded water has been observed.Therefore,from flows of 26,000 cfs to 53,000 cfs a constant water surface elevation and a depth of 0.3 feet were assumed.At flows greater than 53,000 cfs,water levels and depths increase as the resu It of backwater from the ma i nstem.Once overtopping of the upstream berm occurs,the water level at mid-slough increases at a greater rate than during Regime II.The water surface elevation (Table A-5,Sheet 4)and depth (Table A-5,Sheet 7)at the 13 - - - ..... upstream berm change only after the berm is overtopped.At the higher overtopping discharges,the upstream berm becomes submerged because of backwater.. Velocities at the mouth (Table A-5,Sheet 8)are zero until overtopping occurs.However,because the cross sectional area is relatively large, velocities at the slough mouth remain low even during an overtopped condition.At mid-slough (Table A-5,Sheet 9),velocities remain low during overtopping because of the backwater effect.Velocities at the upstream berm (Table A-5,Sheet 10)during overtopping also remain low because of backwater. Total wetted surface area (Table A-5,Sheet 11)increases with increas- ing mainstem discharge as a result of backwater up to the overtopping discharge of 65,000 cfs,and as a result of both backwater and over- topping once overtopping 6ccurs.The wetted surface area includes the areas of both the pond at the ups tream end of the slough and the lower slough even though they are not hydraulically connected at lower flows. The wetted perimeter at the slough mouth (Table A-5,Sheet 12)in- creases because of the backwater effect.The wetted perimeter responds to the shape of the cross section,increasing quickly at first and then remaining relatively constant.At high flows,the wetted perimeter exhibits a large increase because of overtopping of the flood plain. The wetted perimeter at mid-slough (Table A-5,Sheet 13)is 12 feet or less until backwater effects occur at a mainstem flow of 53,000 cfs. Ata discharge of 79,000 cfs,the water surface encroaches on the flood plain resulting in a large increase in wetted perimeter. The wetted perimeter at the upstream berm (Table A-5,Sheet 14)is zero until the Upstream berm is overtopped. A.7 .References .Alaska Department of Fish and·Game,lIS us itna Hydro Aquatic Studies, Phase I Final Draft Report ll ,Volume 1,1982. Alaska Department of Fish and Game,lIS usitna Hydro Aquatic Studies, Phase II Basic Data Report",Volume 4,1983. Chow,V.L,Open Channel Hydraulics,McGraw-Hill,New York,1959. R&M·Consultants,Inc,"Susitna Hydroelectric ProJect,·Hydraulic Project,and Ice Studies",for Alaska Power Authority,Anchorage, Alaska,March 1982. ,"Susitna Hydroelectric Project,1982 Hydrographic Sur-----.....------,;:-veys",for Alaska Power Authority,Anchorage,Alaska,December 1982a • 14 ,"Susitna Hydroelectric Project,Slough Hydrology Interim--~----;-;;-Report ll ,for Alaska Power Authority,Anchorage,Alaska,Decem- ber 1982b. Trihey,E.W.,"Preliminary Assessment of Acres by Spawning Salmon to Side Slough Habitat above Talkeetna",for Alaska Power Authority, Anchorage,Alaska,November 1982. U.S.Army Corps of Engineers,"HEC-2,Water Surface Profiles,Users Manual",Hydrologic Engineering Center,Davis,California, January 1981. 15 ~ i - ." i - -