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GEOTECHNICAL INVESTIGATION
ALASKA ENERGY AUTHORITY
DAVES CREEK SUZSTATION
DRAFT REPORT
Prepared for:
ALASKA ENERGY AUTHORITY
P.O. Box 190869
Anchorage, Alaska 99519-0869
Prepared by:
Arne Tikka
Mike Tauriainen,P.E.
NORTHERN TEST LAB
Box 937
Soldotna, Alaska 99669
February 1991
Project No. 91019
t Lab
February 2S, 1~91
'l'om Arminski
Alaska Energy Authority
P.O. Box 190869
Anchorage, Alaska 9~51~-0689
~101~
Subject: AEA Daves Creek Substation Geotechnical Investigation
Draft Report
Tom:
Enclosed are two copies of our draft report for subject project.
The work was performed in accordance with our January 18 &
February 5, 1991 proposals and discussions with you and Stone &
Webster Engineering Corporation personnel.
'l'he recommendations contained herein reflect our understanding of
the proposed project. Alternate solutions to those we have
suggested may be appropriate and we would appreciate the
opportunity to discuss them with you.
Please call if you have any questions regarding this report. We
encourage your careful review and comment. The final report will
be completed after your review of this draft.
Sincerely, a --r: vi/'!
~-!~ ! --~~ ,_
Arne Tikka
Project Engineer
llb:aeaaaves.rpt
Attachments
35186 s~UR HWY SOLDOTNA. AK 99669 ,907]262-4624 FAX 252-5777
Ar.arvtlcal, Environmental. Geotechnical. C,:;nstructlon Mater1als Tescng
DAVES CREEK SUBS'l'ATION
GEOTECHNICAL INVESTIGATION
CONTENTS
l. INTRODUCTION • • • • • • •
1.1 Background ••••
1.2 Scope ••••••••
2. SITE TOPOGRAPHIC AND GEOMORPHIC CONDITIONS.
3. FIELD !NV EST !GAT ION. • . . . . . . . . . . . .
4. LABORATORY TESTING • . . . . . . . . . . .
. . .
. . . .
1
1
1
2
3
3
5. SOIL, GROUNDWATER AND SURFACE WATER CONDITIONS • • • 3
6. EXIS'l'ING UTILITIES AND O'll:l.ER SITE CDNDITIONS • 4
7. CONCLUSIONS AND RECOMMENDATIONS ••• . . .
7.1 Bearing Capacity •••••••••••••
7.2 Footings •••••••••••••••••••
7.2.1 Alternate Footing Recommendation
7.2.2 Drilled Piers •••••••••••••
7.3 Fill and Back£ ill. • • • • • ••
7.4 Frost Action •••••••••••••••
7.5
7.6
7.7
Drainage • • •
Construction •
Corrosion.
8. CLOSURE.
ATTACHMENTS
. . . . . . . . . . .
Soil Boring Log Legend. • • • •••••• Drawing Al
Soil Boring Logs. • • • • • • • • • • • • Drawings A2-5
Lab Test Results. • • • ••••••••• Sheet Bl-2
Site plan with Soil Boring Locations. Drawing C
Shallow Footing Details • • • • • • ••• Drawing D
5
6
7
7
8
9
10
10
11
11
12
1. INTRODUCTION
1.1 BACKGROUND
The Alaska Energy Authority (AEA) is proposing to buila an
electrical, power substation adjacent to the existing Chugach
Electric substation, near mile 40 of the Sterling Highway, east-
northeast of Cooper Landing, Alaska. Design snow and wind loads are
unknown for this site. 'l'he proposed substation is locatea in UBC
Seismic Zone 4.
According to AEA personnel, subject property belongs to the National
Forest Service.
1.2 SCOPE
Northern Test Lab (N'l'L) was retained by AEA to conduct a sut:Burface
soils investigation, laboratory testing. and analysis of the data
sufficient to prepare a geotechnical report of foundation soil
characteristics, static bearing, static settlement, and related
properties, for design of improvements to the proposed Alaska Energy
Authority substation.
The work was performed in accordance with our discussions, our
January 18, 1991 proposal, our February 5. 1991 proposal, and our
standard geotechnical procedures.
We understand that improvements to the proposea substation will
consist of towers and poles founded on drilled piers, and other
structures designed with conventional spread footings.
Stone & Webster Engineering Corporation personnel inaicate the
maximum sustainea vertical loaa may be on the order of 2000 -3000
psf. We understand that moderate frost heave (say two inches) can
be tolerated by the proposed facilities.
AEA Daves Creek Substation Draft Report Page 1
2. SITE TOPOGRAPHIC AND GEOMORPHIC CONDITIONS
The proposed substation is located in the Kenai Mountains along the
Chugach Mountains geosyncline. Sedimentary rocks of Jurassic and
late Cretaceous age were highly deformed and partly metamorphosed
durina post-Paleocene time in this area (DSGS Professional Paper
~ .
542-E). The area was uplifted and eroded several times auring the
'I'ertiary Period, and possibly continuing into the Quaternary Period.
Unconsolidated glacial and fluvial deposits presently overlie the
bedrock in most places except on the steeper mountain slopes.
The surrounding Kenai Mountains make most of the region very rugged
terrain, characterized by numerous glaciers and glacial worked
topography. 'I'he area of the site lies in a narrow, glacially
scoured valley near the center of the Kenai Peninsula. Soils in the
area of the site appear to consist of fluvial and/or glacial-fluvial
deposits.
Based on relative soil boring elevations, the area of the pro_[::€rty
investigated appears to be sloping gently toward the southeast,
however, the actual terrain in the area of the soil borings was
quite variable. Quartz Creek flows in a southwest airection just
northwest ot tl:e site.
Vegetation consists of small diameter spruce and some larger
aiameter asper, and cottonwood. Ground cover appears mostly
gravelly,
borings.
however, some surrace organics were encounterro at some
Based on the terrain and vegetation, flooding ot the site
shoula not be unexpectea. 'I'otal reliei appears to be less than five
feet in the area of the soil borings.
elevation is 600 feet above MSL.
'I'he approximate site
The site is bordered on the south by the Chugach Electric
Substation, which is aajacent to the Sterling Highwa1. Cther
surrounding property appears undevelopea.
AEA Daves Creek Substation Draft Report Page 2
3. FIELD INVESTIGATION
The field investigation was performed December 11-12, 1991 using a
Kraxberger Drilling, truck-mounted B-53 mobile drill rig. ~~o soil
borings <SB 1 & 2) were advanced to 30' and four were advanced to a
depth ot 15' using a·· OD hollow stem ausers.
Representative samples were obtained .:rom 1.4'' split spoon samplers
driven into undisturbed material belc'ri the rot tom of the auc;;ers .,.,.i th
a 140i hammer dropping 3U", the Star:dara Penetration Test. Soil
types and blow counts are shown on the attached test hole logs,
Drawings A2-5.
Each sample was visually characterized in the tield and further
verification and classification was performed in the lab.
Approximate boring locations are shown on the a ttacheci site plan,
Drawing c. Borings were located by N~'L personnel, during the field
investigation, according to a site plan prov1ded by AEA. ~·he actual
locations were measured from existing area improvements using a
fiberglass tape, but were not surveyed and are approximate only.
Final boring locations were staked and labeled.
4. LABORATORY TESTING
Approximately 30 samples were retainea from the soil borings and
selected samples were tested for grain size. Test results are shown
on the test hole logs and on the laboratory test results, Sheet Bl.
Similar soils were combined for testing ana are noted. on the summary
sheets.
5. SUBSURFACE SOIL, GROUNDWATER AND SURFACE WATER CONDITIONS
Soils encountered while drilling were variable and. consist mostly ot
noncohesive sand and gravel mixtures with varying silt content,
AEA Daves Creek Substation Dratt Report Page 3
apparent cobble layers, and sand layers. Surface organics from
o.s• -1.0' thick. were encountered in SBs 3, 5, & 6.
An approximate one and one-half foot thick. cobble layer (cobbles to
four ir.ch diameter or more with sar:c, gravel, and silt filHng :::.r:
voids) was encountered within the tof four feet in SB 1, 2, & 3, ano
cobbles were encountered from the surface to four feet deep in SB 4.
Some sticks and organics were obsePied in the split spoon sample
from 5-6.5' in SB 2.
Soft sand and organic silt were encountered from 4.5-6.5' in SB 5
resulting in a low blow count <11 blows per foot) from 5.5 -6.5'.
Some soft to moaerately dense gravelly sand was encountered from 4.0
-11.0' in SB 1 <16 blows per foot from 5.5 -6.5'). Other soils
appeared variable and consist oi sand/gravel mixtures with varying
silt content, coarse gravel or cobble layers, and sand layers.
A groundwater table was encountered in all soil borings at depths
ranging from 8.0 -12.5 feet. The groundwater table could, ana
probably does, rise to higher levels and could affect foundation
bearing capacity and performance. Frozen soils were encountered in
all borings to aFproximately one foot below the grouna sur race. SB
2 & 3 are located on, or adjacent to, a drive kept clear of snow,
ana had frost p;:netraticn to 6' and 3', respectively.
No surface water was encountered in the area of the borings,
however, Quartz Creek flows just ~~ of the site, as aescribea
previously. ~he site appears to lie within the flooa plain of
Quartz Creek., and while the tlooa potenLial appears to be
significant, it was not a part of this investigation.
6. EXISTING UTILITIES AND OWER SITE CONDITIONS
Electrical transmission lines and an electrical substation are
located directly south ot the soil tor ing locations. 'l'he aajacer1t
AEA Daves Creek. Sur..station Draft Report Page 4
, .
Chugach Electric Association (CEA) substation was originally
constructed about 15159. CEA was contacted prior to tne soils
investigation for setback r eq ui rem en ts. CEA personnel were on site
during the field investigation and inoicated setback req.~irements
from the transmission line and substation. No other apparent
u~ilities exist onsit~
According to CEA personnel ons1 te during the t iela i nves t.l sa tl on,
some fill and possible debris may have been buried aaJacent to CEA's
substation, in the area of SB 2 & 3, auring original consuucr.ion.
7. CONCLUSIONS AND RECDMMENDATIONS
We understand that proposed improvements may consist of. towers or
poles founded on drilled piers, or other structures using
conventional footings for the foundations, and our recommendations
are based upon that assumption. The soil conditions at the site
generally appear to be suitable for this type of construction,
provided these recommendations are followed.
The op1n1ons expressed with respect to soil characteristics incluae
only qualitative considerations of the probable aynamic
characteristics of the foundation soils. No deep seated hazards
related to time dependent settlement under static loads or
liquefaction uncer dynamic loads are t:reaicted on tne basis of the
d3. ta and our knew ledge of the local area. However, limi teo areas of
shallow (0-7') soft soils may experience some gravity or seismic
related consolidation. The relationship of the structure tc the
foundation soi 1 rr:ass in terms of ground response unoe r ear tllq uake
load is not part of the scope of this investigation. It is our
opinion based on the data that ground response will be t.hat
associated with moderately dense fluvial deposits resulting in
strong ground motion.
A numter of borings inoicate appare~t. sott and/or organic soils
AEA Daves Creek Substation Draft Report Pase 5
which should be compacted or excavated prior to placement ot
structures. We recommend that sufficient time, as well as unit
prices, be allowed for identification and exca·;ation of any
unsuitable soils at the time of construction. It is our opinion
that this will be the most efficient resolution of the apparent
problem. However, if the owner wan-es to further cefine tte extent
or u n s u i t a c 1 e J.: 2. L e r i a l f or tid a i n g ;: ,__; r p o s e s , t e s t .::-: o 1 e s u. c a v c. t e c
using a backhoe, a resistivity survey, or similar technique could
provice better definition of the unsuitable soils.
7.1 BEARING CAPACITY
A maximum allowable bearing capacity of 4000 psf is recommended for
the moderately dense to very dense sands and gravels below
approximately four feet, provided any loose soils are adequately
compacted or removed. Any soils that do not respond to compactive
efforts should be replaced.
Because of the relatively shallow groundwater table and the
probability that it will rise, the allowable bearing capacity
should be adjusted by a groundwater correction factor tor some
footings:
Cw = 0.5 + 0.5[0w/(Df +B)] < 1.0
where Cw = grounawa ter correction factor
Dw = depth of wa. ter table below ::ooting
Df = depth of footing bel CJ.oJ nearest surface
B = width of footJ.ng
Allowable bearir.g capacities may be increasea 33% fer wino, se1smic
or shock loadir:g. The predicted maxirr:um total settlement shoula not
exceed one inch under the design loaaing conai tior.s, proviaed the
recommendations of this report are followea. Differential
settlement could be up to 3/4 of the total.
A~A Daves Creek Substation Draft Report Page 6
7.2 FOOTINGS
All peri meter he a ted footings should be placed a mini mum ot 3 1/2
feet below final exterior grade (unless a shallow insulated footing
system is used in which case the minicum depth shoulc be lb inches).
1'he hlinimum depth for interior footlngs shcula be 18' incr:es. 'l'he
recommended minimum width of continuous footings is 18 inc.hes. 'l'he
recommended minimum dimension of isolated footings is 24 inches.
Interior footings may be shallower, and all footings may be r.ar rower
provided the recommended bearing capacity is reduced
proportionately. Non-bearing stern walls may be on the order of six
inches wide.
Unheated shallow footings founded in these soils may heave. 'I'o
reduce or prevent significant heaving of unheated footings a variety
of construction solutions may be appropriate, depending on the
design features and allowable heave toleration of proposed
improvements.
Heaving of unheated footings may be reduced by one or a comuination
of the following: 1) found footing below the maximum depth of freeze
and prevent uplift along sides of footing (this option may be
aifficult due to relatively shallow depth to water tacle), 2)
insulate to prevent frost penetration into frost suscepticle soils
under footings, and 3) replace frost susceptible soil witt NFS soil
to below the maximum depth of treeze.
All footings sho~ld bear on on competent and compactea ~FS cackfill,
at least 12 inches thick. Allowable bearing capacities mav be
increased in accoraance with Section 7.3, FILL AND BACKFILL.
7.2.1 Alternate Footing Recommendation
An alternate shallow, insulated. footing system may be considerea
for heated buildings consisting of a footing monolith1c with the
floor slab, or a short stern wall. 'lhi s footing should be set to a
AE.A Daves Creek Substation Draft Report Page 7
minimum depth of 18 inches. Two inches of extruaed polystyrene
insulation should be pla.cea vertically against the outside of the
foundation, then extended outward a sufficient distance to avoid
frost penetration beneath the footing, as shown on Drawing D. The
cost of additional ins~lation is uscally more than cfrse~ cy the
reduced fou.naa t.icn aectr ..
For unheated sr,allow toot:;.ngs the insulation r:-.csr. ce -::r;.:.cr;er
(minimum of 4 inches), must be continuous uncer the enure :::ccr_ing,
and must extend significantly beyond tne footing peri~eter.
7.2.2 Drilled Piers
'l'he allowable end bearing capacity for piers can be taken as 4000
psf given the following conditions and assumptions:
-depth: 10'+
-min. ciarn: 24"
-safety factor: 3.0 in shear
-placed near or into water table
-angle of internal friction: 330
Shaft friction can be taken as 500 psf for sustained loads ana 1000
psf for transitory loads. Maximum anticipated settlement under
these conditions may be expected to be one to two inches.
The lateral earth pressure (total pressure on a ur:it of a vertical
plane extendin<; :rom the surface to a depth H) can i::-e taKen as:
active, Pa = lb.5H2
Therefore, given an effective aepth of nine feet (allowing one toot
of disturbance on a ten foot bury), a aiameter of two feet., ana a
satety factor a: :.tuee, the resistance c:o laterd aisplacer..ent hOL..lc
be 11,340# actin; three feet up fro~ ~~e base. for ::ansitory ~caas
AEA Daves Creek Substation Draft Report Page 8
this could be increased to 15,000#.
Drilled piers foun~ed at or above the water table woulG reduce
construction problems and associated costs. Working below the water
table would likely require casing of the hole and use ot a slurry
(drilling mud) to control sloughing. Belling is prot.acly not
feasible because of tne cohesionless soils, therefore set.s of two
piers, tied at the top, may be desirable.
7.3 FILL AND BACKFILL
Fill and backfill under footings and slabs shoula be NFS, flaced in
maximum loose lifts of nine inches and compacted to at least 95% of
maximum density per ASTM D-1557D, with a correction for oversize
particles in accordance with Alaska 'I'-ll if appropriate. Backfill
under footings should extend from the bottom edge of footings to
undisturbed soil at a maximum slope of 1:2, horizontal to vertical.
The upper six inches of any backfill below footings or slats should
have a maximum size limit of two inches. Final founaa tion bearing
surfaces should te carefully inspected prior to placing relnforcing
steel and concrete to verity that any loose soil has been compacted
or removea and any frozen soil, debris, or organic matter nas been
removed.
Irr.ported fill/bacKfill shculd be reascnably w-ell-gr<;:.aed ar.a able to
be compacted tc a tight, unyielding surface. Fer local ~ater1al
meeting the tollcwing graaation and cor:<pacted to at least 95% or tne
maximum density, an allowable bearing capacity of up to 50 C.G psi may
be usee at the upper surrace of the bccKfill proviaec tne loading of
the in situ so1ls does not exceea the allowable noted ~ncer 7.1
BEARING CAPACI1Y. Soils not meeting th1s gracation shoulc be
evaluated on an inaividual basis.
A~A Daves Creek Substation Draft Report Page 9
Sieve
3"
1"
#2LG
Percent Passing
100
70 -100
35 -75
G -5
The in-situ sc1ls at the bottom ot an excavation shoulc remain
undisturbea, or if disturbea be rer::ovea, prior to placing any
backfill on them.
The onsite soils within approximately 6-8 feet of existing grade are
generally not suitable for backfill material below footings or slabs
due to the silt and cobble content.
Footing and foundation wall backfill not supporting slabs or
pavement should be compacted to 85 -9(J% of maxi mum density. Care
should be utilized adjacent to walls to avoid overcorr.pacting
backfill and laterally displacing foundation&
7.4 FROST ACTION
The depth of frost penetration tor a site is aependent on soil
conditions, exposure and weather. For the sanay/gravelly soils
encountered, with a surface kept clear of snow, normal cepths ot
freeze can be e:;pected to approach b-10 feet, ana 10 feet or more
for NFS backfill. 'I'he actual trost pE:r.etration adjacent to pro:p;rly
designed foundations of heated buildinss will be muc~ less.
7.5 DRAINAGE
Minimum slopes of 5% for a mini~um cistance ot lG feet should be
provided away frcm builaings to promote arainage. Any concentrated
drainage shoulc be directea away from builaing foundation&
The final grades should be carefully consiaered to promote surface
AEA Daves Creek Substation Dratt Report Page lU
drainage and avoid pending and surface water infiltration. Onsite
soils appear free draining to the water table.
7.6 CONSTRUCTION
Soils are mostly nonconesi ve and CL:tS in tne s1 te sands ar.a gravels
can be expected to slough to at least 1:2 slopes and nay do so
without warning.
Com:paction of backfill and frost sl.l.sceptibility of soils s.Goula be
carefully monitored during construction. The existing soils at the
bottom of any excavation should be maintained in their natural
condition, or carefully compacted if necessary.
For footings that cannot tolerate a total maximum settlement of
greater than one inch or differential settlement of more than 3/4
inch, we recommend over excavating, proofrolling, and placement ot
properly compacted backfill material.
Potential occurence of debris, soft sand, and organic silt deposits
exists throughout the site. Materials of these types were
encountered in SB 2 and SB 5. As mentioned previously, some
construction detris from original construction of the aaJacent CEA
substation may te buried.
'I'he groundwater table may, ana i.iOSt likely WJ.ll, rJ.se tO
higher levels c:..;ring otter timee of :::e year and may sigr..:..f 1cantly
atfect construc~1cn activities. Sor..e aewatering or excavations or
aiversion of runoff may be necessary.
7.7 CORROSION
The soils in the Cooper Lanaing area typically have not shown to be
of a very corrosive nature. However, all underground materials
should be correctly selected, properly installed and carefully
inspected at the time of installation to assure satisfactory serv1ce
AEA Daves Creek S~Dstation Draft Report Page 11
life. The need for cathodic protection, coating, or other
protection of the underground materials should be evaluated.
8. CLOSURE
'I'his report is t.asec on oc:r unaerstc.r.:::::..ng of tne prcposea s::.r.t..:c:.:....
and performance criteria. Deviations from these criteria coula
alter our recommendations. Our recommendations are cert.:nnly nvt
all inclusive ant various other techniques and options ~ay te
desirable. We would appreciate tr:e opportunity to rev1ew ana
evaluate any significant foundation related changes.
Due to the variable nature of soils and occasional soft soils on the
site, it is our opinion that subsurface conai tions may vary
considerably, and in some places may require extra excavation and/or
proofrolling. The actual extent of soft soils can best be
determined at the time of construction. We recommend that sui table
provision be made in the contract documents to accomocate varying
earthwork conaitions.
Finally, we recorr:mend the site be carefully checked by a qualitied
engineer during construction to verify that conditions are as
anticipatea in tne design. We are available to aiscuss th1s report
in more detail with the owner and/ or ~is representatives.
AEA Daves Creek Substation Draft Report Page 12
I
STM.VARD SYMBOLS
ORGAPHC MATERIAL COBBLES & BOULDERS
CLAY
SILT
SAND
SRA'JEL
~11?LER TYPE SYMBOLS:
s~ .
Ss •
Sl •
S!': • •
Sx.
Sl.
~ ..
~1 .
CONGLOMERATE
SAilDSTOiiE
1.411 Split Sl:oon with 47# Hamr:~er
1.4" Split Spoon with 140# Hammer
2.5" Sclit Spoon with 140# Hammer
2.5" Split Spoon with 34D# Hammer
2.011 Split Spoon with 140# Har.uner
1.411 Soiit Spoon with 340# Hammer
2.511 Spiit Spoon, Pushed
r.4 11 Spiit ~on Oriven with Air Hammer
2.511 Split S,."'on Oirven with Air Har:-!!ler
lGilEOOS ROCK
IIET AI«JRPH I C ROCK
ICE, MASSIVE
ICE -SILT
'JP.G~f-;IC SILT
Ts •••
Tm
Pb ••
Cs •••
Cd •••
Bs •••
A
G
SA:mY SILT
Sll T GRADWG TO
SAilOY SILT
SANOY GRAVEl, SCATTERED
COBBLES (ROCK FRAGMOITS)
INTERLAYERED SAill &
SA~mY GRAVEL
.
3iLTY CLAY •/TRACE SA~U
Shelby Tube
Modified Shelby Tube
Pitcher Barre 1
Core Barrel with Single Tube
Core Barrel with Double Tube
Bulk Sa:lUie
Auger Sar:~ole
Grab Sa:~ole
•:JT::: Sar.~oier types are eitt·.er .,o::ed above the Boring log or adjacent to it at the respecti·;'! !a.;ole depth •
TEST HOlE ~"t.MBER -TH 2
DA'IE DRillED 5 June 1961
........-SAMPLER TYPE
All Sa~ies Ss
ORG~~;IC HATEF.I .t.:.. (PT)
Ccrsiderable ~isitl e ice 0' -7' ICE -"L-ICE DESCRIPTION
FROZEN . INTERVAL --_ss
STRJ..TA CP.AXGE _... .• ~
~~.0
Cd
30 .0
(ICE~11 -·
G)
BECq8-.:K (Schist) (BX)
T.D.
'IUTAL DEP'IH DRIU.ED
* W.D. -Whi le Jrilling: ~.~. -After Drilling
Nti~ t ;;e;;·;;L·'·i it!"st ,.oca 46 Soil Boring
Log Legend
Materials and Quality Control Teating
C~ECSEO:
D!E:
~~-~~:~------~ Pt\~J.NO .:
Norltlern les t Lab
An11ly tio111., Environmenta 1., Geoteohnio111.,
Construction Materials Testing
SB 1
2-11-9 1
Sandy GRAVEL w/Sm. snt, Gray I
Soil Boring Log Date: 2-18-91
lniti11ls: A.T. AEA Dave·s Creek
Geotechnica 1 Investigation Soale: 1" = 3.0'
SB 1 Sheet: A2 of 5
Dense, Froz:en or Sl. Mo;st, (GM) Ss SAND, Ot;ve, Dense, Wet, (SP)
(Cobbles to 4" ;n Auger Return)
G) 16
Gravelly SAND, Ql;ve, Mod. Dense,
Sl. Moh~t, (SP)
@75
Sandy Gravel w/Tr. to Sm. snt,
Mo;st, (GP-GM)
Water@ 12.5' W .D.
(Cobbles to 4" ;n Auger Return)
@ ~0+ Blows for 6 ··
(No Reoovery)
SAND, Ol;ve, Dense, Wet, (SP)
@e6
Sandy Gravel w/Tr. sm, Ol;ve,
Dense, Wet, (GP-OM)
T.D.
Norlltern lest Lab
Analytical~ EnYironmenta 1 ~ Geotechntca 1 ~
Construction Haterials Testint
SB 2
2-11-91
Sindy GRAVEL w/Sm. Silt1 Gray 1
Soil Boring Log Date: 2-18-91
Initials : A. T. AEA Deye·s Creek
Geotechnica 1 lnY•stitation Seal•: 1" = 3.0'
SB 2 Sheet: A3 of 5
Froztn 1 (GM) Ss Samt u Abovt
(Cobblts to 4"1n Au9tr Rtturn)
(Cobblts or Co.rst Oravtl W .D.)
(!) 84 @100
SAND w /Sm. Gravtland Tr. SHt 1
SAND w/Sm. Silt1 Olivt 1 Froztn1 (SM)
("'/Stick~ ind Org~'ic Debris in
Simplt)
V. Dense 1 Wtt 1 (SP-SM)
Wittr@ 8.0' W.O.
@s6
SAND w/Sm. Oravtland Tr. S11t 1
Olivt 1 Dtnse 1 Wtt 1 (SP-SM)
@32
SAND 1 Olin 1 Dtnst 1 Wttl
T.D.
(SP)
@98
Sand~t~ OR AVEL 'W' /Sm. Silt 1 Olin 1
V. Dens• 1 W tt 1 (OM)
Soil Boring Log Dat•: 2-18-91 Norlltern lest LDb lntttals: A.T . AEA Dave·s Creek Seal•: 1 " = 3.0' Ana lv ttca 1, Envtronm•nta 1, G•ot•chntca 1, G•ot•ohnioa 1 lnv•sttgation Construotion Hater a ls T esttnt Sh••t : A4 of :S
SB 3
2-12-91
Surfaot ORGANICS, Brown,
Froztn, (w /Sticks or W'ood
Dtbr;s)
Snty SAND, Ql;ve, Froztn,
Sindy GRAVEL w/Sm. SHt, OHvt,
(Pt)
(SM)
Froztn, (Rooks to!"), (GM)
(!)78
Sindy GRAVEL .., /Tr. snt I 011vt I Ss
V. Dtns:t, Moist, (GP-GM)
B.O'
'w'~t•r@ 1 0.5' 'w' .0.
(Cobblts or Coirst Gravel W'.D.)
@38
SAND w /Sm. Or an 1, OHvt, Dtnn,
W'tt, (SP)
T.D.
SB 3 & SB 4
SB 4
2-12-91
Sandy GRAVEL w/Sm. SHt, OHvt,
DtnSt, Froztn or Moist, (GM)
(Cobblts to 4" 1n iUQtr rtturn)
(!)34
Sindy OR AVEL .., /Tr. snt I 011vt I
Dtns:t, Sl. Moist, (OP-OM)
® 49
Sandy OR AVEL w /Tr. Silt, Olivt,
Dtnst, W'tt, (OP-OM)
W'attr ~ 11 .5' W' .D.
@68
Sand!J GRAVEL w/Tr. to Sm. SHt,
011vt , V. Dtnst, W'tt, (OM)
T.o.·
Norlltern lest Lab
Ana 1y tic a 1., EnYironm•nta 1., G•ot•chnica 1.,
Construotton Materials T•sting
so 5
2-12-91
Surfact ORGANICS 1 Brown 1
Frcztn 1 ( w /Sticks or Wood
ow;s)
SandiJ GRAVEL w/Sm. Snt1
OHvt 1 Dtnst 1 Froztn or Moist 1
G) 11
(Pt)
(GM)
Soil Boring Log Oat•: 2-24-91
Initials: A.T. AEA Dave·s Creek Seal•: 1" = 3.0' Geotechnica 1 lnYutigation
Sheet : A:S of :1 so 5 & so 6
so 6
2-12-91
2.0'
G
Surface Or'jlanics 1 Brown 1 Frozen 1 (Pt)
Sandv GRAVEL w/Sm. Snt 1 01iVt 1
Dtnst1 Froztn or Moist1 (GM)
(Cobblts to 4" in Au'jltr Rtturn)
(!)64
SandiJ GRAVEL w /Tr. Silt 1 Olivt 1
V. Dtnst 1 Sl. Moist 1 (GP-GM)
SAND w /Sm. OrQanto Silt 1 Oltvt
(sand) IT an (silt) 1 Loost/Soft 1
Moist1 (SP/Ml)
(Coarse Gravtl or Cobbles W.O.)
042
S1nd1J GRAYEL w/Tr. to No Silt1
Dtnse 1 Wtt 1 (GP-GM)
W attr @ 11.0 "w' .D.
(Cobblts or Coarse Gravel W.O.)
(!)a6
SAND w /Sm. Gr avt 11 OHvt 1 V .Dtnst 1 S.nd\j GR AYEL w /Tr. to No sm I
Wtt1 (SP)
T.D.
Olin • V. Dtnse I Wtt, (GP) r.o .·
:lett' 2/22/91 I Project No.' 91019
PrO)tCI• Daves Creek Subdivision
Atttntlon • tl6r ltiltAiiLASKi i!iit ~[846
Materials and Quality Control Testing
Architect /En9in11r •
Contractor •
BILLING/ RESULTS TO:
Copy•
Alaska Energy Authority
P.O. Box 190869
Pooe .#B1
.~chorage, Alaska 99519-0689
SUMMARY SHEET
c:i
Lab# Q?~i Q?RT Q?RT Q?~T
....: Date 2/11/91 2/11/91 2/11/91 2/11/91
UJ 1111 r.r~mhi nPri A C,omhi necl R TH!.J.. ...J a.. S::~lTinl P 1 S::~nmlP ? Samnle ,qs SAmnle 1 ~
<t 'Jnrf>ri (/) .
3"
2"
11/2" 100 100
I" 100 92 89 100 I
I 3/4" 90 81 86 91
1/2" 85 63 75 80 I I
I
(!) 3/8" 78 57 67 76 I z
iii #4 53 42 so 60 (/)
I ~ #10 31 27 35 42 I
I ..... #20 17 17 ' 24 27 I I z I
w #40 12 ll 17 17 I (.) I
a:: #100 5 7 11 9 :
i w : I a.. 3.2 ts.J I #200 5.2 ! 6.1 i
.02mm
.05 mm I i I
002mm ! I !
YOISTUR>:: ! i
•
_,QUID UMIT i I i
: ;JLASTIC tNDEX i I I
SPECIFIC GRAVITY i i :
i :o/o FRACTURE -t-#4 ! I l
: JSC CLASS C:P r:P-f:\-1 i GP---G.'-1 . GP-G\1 :
:);o BITUMINOUS ! i
r:ROST CLASS i i I
' MAXIMUM DENSITY !
! ADJ. LAB DENSITY I i :
:PT!MUM MOISTURE I !
i
ZES NOT CONFORM I :
1,2; 1H l, Sc.j_~le ·). TH ?)!' Scl!-;::Jle 1.
' 0
If) -
140'
200'
----------170' ------------!
0 SB-1
<100.0> AEA SITE
r1s·
r----0
SB-6
(97.8)
-------120' ---+-------i
r-------+-60' ---......f
.-------+-------0 SB-5
(97.5)
140'
r-0 sB-3
1 <97.7>
DRIVE
25'
~D
NORTH
30 60
I
NORTHEAST END OF
EXISTING C.E.A. SUB.
EXISTING FENCE
0 SB-3
(97.7)
DRA \.liNG 'C'
-SOIL BORING w/
RELATIVE ELEVATION
ALASKA ENERGY AUTHORITY
DAVES CREEK GEOTECHNICAL
APPROX. SOIL BORING LOCATIONS
fEB. 1'391 AEA
PREPARED BY
Northern lett Lcm
I
·I
Norlltern lest Lab
An~ 1y ttca 1, Envtronm•nb I, G•ot•chnica 1,
Construction Hater'ia ls T •stinCJ
•NON-BEARING WAl.L-6" MIN. _
BEARING WALL -A5 ~E:QUI~ED,
· · 12.'' MIN •.
AEA 5UbSt8t1on D~t•: 11-28-90
G•ot•chnic~l lnv•sttCJ~tion lniti~ls: A. T.
Shellow Footing Details Seal•: NTS
Drawing: D
~ "'tJG.. s ~ P; ..J;
wxf.,-to~ 10 .,J.,J,::.
w -. z• ~~o · f'OL.',c;;rr~N€
-=n,r:;,tJL}rlot-.1..
5HALLD\A/ GONVEblTIONAL FCVTI~s
~T~