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Susitna‐Watana Hydroelectric Project Document
ARLIS Uniform Cover Page
Title:
Water quality modeling study, Study plan Section 5.6, 2014 Study
Implementation Report SuWa 289
Author(s) – Personal:
Author(s) – Corporate:
URS Corporation
Tetra Tech, Inc.
AEA‐identified category, if specified:
November 2015; Study Completion and 2014/2015 Implementation Reports
AEA‐identified series, if specified:
Series (ARLIS‐assigned report number):
Susitna-Watana Hydroelectric Project document number 289
Existing numbers on document:
Published by:
[Anchorage : Alaska Energy Authority, 2015]
Date published:
November 2015
Published for:
Alaska Energy Authority
Date or date range of report:
Volume and/or Part numbers:
Study plan Section 5.6
Final or Draft status, as indicated:
Document type:
Pagination:
54 pages in various pagings
Related work(s): Pages added/changed by ARLIS:
Notes:
All reports in the Susitna‐Watana Hydroelectric Project Document series include an ARLIS‐
produced cover page and an ARLIS‐assigned number for uniformity and citability. All reports
are posted online at http://www.arlis.org/resources/susitna‐watana/
Susitna-Watana Hydroelectric Project
(FERC No. 14241)
Water Quality Modeling Study
Study Plan Section 5.6
2014 Study Implementation Report
Prepared for
Alaska Energy Authority
Prepared by
URS Corporation/Tetra Tech, Inc.
November 2015
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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FERC Project No. 14241 Page i November 2015
TABLE OF CONTENTS
1. Introduction ....................................................................................................................... 1
2. Study Objectives................................................................................................................ 2
3. Study Area ......................................................................................................................... 2
4. Methods and Variances .................................................................................................... 3
4.1. Methods................................................................................................................... 3
4.1.1. Model Selection .............................................................................. 3
4.1.2. Reservoir and Downstream River Modeling Approaches .............. 3
4.1.3. Focus Area Modeling ...................................................................... 3
4.1.4. Scales for Modeling and Resolution of the Output ......................... 3
4.1.5. Selection of Model State Variables and Options ............................ 4
4.2. Variances from Study Plan ..................................................................................... 4
5. Results ................................................................................................................................ 4
5.1. Reservoir Model ...................................................................................................... 4
5.2. River Model ............................................................................................................ 5
5.3. FA-128 (Slough 8A) Model .................................................................................... 6
6. Discussion........................................................................................................................... 6
7. Conclusion ......................................................................................................................... 7
8. Literature Cited ................................................................................................................ 7
9. Tables ................................................................................................................................. 9
10. Figures .............................................................................................................................. 11
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LIST OF TABLES
Table 3-1. Susitna River Basin Temperature and Water Quality Monitoring Sites. ...................... 9
Figure 3-1. Stream Water Quality and Temperature Data Collection Sites for the Susitna-Watana
Hydroelectric Project. ............................................................................................................ 12
Figure 5.2-1. River Model Temperature Calibration Plots (PRM 152.7, 152.2, 142.3, 140). ...... 13
Figure 5.2-2. River Model Temperature Calibration Plots (PRM 88.3, 87.8, 59.9). .................... 14
APPENDICES
Appendix A: April 2014 Proof of Concept Result Plots
ATTACHMENTS
Attachment 1: Relationship between Turbidity and Total Suspended Solids: A Correlation Model
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LIST OF ACRONYMS, ABBREVIATIONS, AND DEFINITIONS
Abbreviation Definition
AEA Alaska Energy Authority
CFR Code of Federal Regulations
Commission Federal Energy Regulatory Commission
DO dissolved oxygen
EFDC Environmental Fluid Dynamics Code
FA Focus Area
FERC Federal Energy Regulatory Commission
ILP Integrated Licensing Process
ISR Initial Study Report
POC proof of concept
PRM Project River Mile
Project Susitna-Watana Hydroelectric Project
RSP Revised Study Plan
SPD study plan determination
TSS total suspended solids
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1. INTRODUCTION
This Water Quality Modeling Study, Section 5.6 of the Revised Study Plan (RSP) approved by the
Federal Energy Regulatory Commission (FERC or Commission) for the Susitna-Watana
Hydroelectric Project, FERC Project No. 14241, focuses on predicting the potential impacts of the
dam and its proposed operations on water quality through the development of a water quality
model. The goal of the Water Quality Modeling Study will be to utilize the extensive information
collected from the Baseline Water Quality Study (Section 5.5 of the RSP) to develop a model(s)
to evaluate the potential impacts of the proposed Project and operations on various physical
parameters within the Susitna River watershed.
A summary of the development of this study, together with the Alaska Energy Authority’s (AEA)
implementation of it through the 2013 study season, appears in Part A, Section 1 of the Initial
Study Report (ISR) filed with FERC in June 2014. As required under FERC’s regulations for the
Integrated Licensing Process (ILP), the ISR describes AEA’s “overall progress in implementing
the study plan and schedule and the data collected, including an explanation of any variance from
the study plan and schedule.” (18 CFR 5.15(c)(1)).
Since filing the ISR in June 2014, AEA has continued to implement the FERC-approved plan for
the Water Quality Modeling Study. These efforts have included the following:
On September 30, 2014, AEA filed with FERC the Water Quality and Lower River
Modeling Technical Memorandum (AEA 2014a), which provided results of the analysis
and recommendation of extending the Water Quality Model below Project River Mile
(PRM 29.9) and an evaluation of the adequacy of the water temperature and meteorological
data collected through 2014. Based on the findings, AEA did not propose extending the
model downstream beyond PRM 29.9.
On October 16, 2014, AEA held an ISR meeting about the Baseline Water Quality
Monitoring Study (Study 5.5), Water Quality Modeling Study (Study 5.6), and Mercury
Assessment and Potential for Bioaccumulation Study (Study 5.7).
Since the 2014 ISR, the riverine model was calibrated for temperature using observed
temperature data from 2012 and 2013.
Although turbidity is not a direct output from the water quality models, it is a parameter
that will be included when evaluating potential Project effects. Because turbidity and the
concentration of suspended sediment, which is a modeled constituent, are correlated,
relationships between these two variables are required to interpret model results. These
relationships were developed for the Susitna River from data collected by Study 5.5, and
the results are presented in Attachment 1 of this report.
In furtherance of the next round of ISR meetings and FERC’s SPD, this report describes AEA’s
overall progress in implementing the Water Quality Modeling Study during calendar year 2014.
Rather than a comprehensive reporting of all field work, data collection, and data analysis since
the beginning of AEA’s study program, this report is intended to supplement and update the
information presented in Part A of the ISR for Water Quality Modeling through the end of calendar
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year 2014. It describes the methods and results of the 2014 effort, and includes a discussion of the
results achieved.
2. STUDY OBJECTIVES
The collective goal of the water quality studies (Baseline Water Quality Study, Water Quality
Modeling Study, and the Mercury Assessment and Potential for Bioaccumulation Study) is to
assess the impacts of the proposed Project operations on water quality in the Susitna River basin
with particular reference to state water quality standards. Predicting the potential impacts of the
dam and its proposed operations on water quality requires the development of a water quality
model. The goal of the Water Quality Modeling Study is to utilize the extensive information
collected from the Baseline Water Quality Study to develop a model(s) to evaluate the potential
impacts of the proposed Project and operations on various physical parameters within the Susitna
River watershed.
The objectives of the Water Quality Modeling Study are as follows:
Implement (with input from licensing participants) an appropriate reservoir and river water
temperature model for use with past and current monitoring data.
Using the data developed as part of the Baseline Water Quality Study, model water quality
conditions in the proposed Watana Reservoir, including (but not necessarily limited to)
temperature, dissolved oxygen (DO), fine suspended sediment and turbidity, chlorophyll-
a, nutrients, ice, and metals.
Model water quality conditions in the Susitna River from the proposed site of the Watana
Dam downstream, including (but not necessarily limited to) temperature, DO, fine
suspended sediment and turbidity, chlorophyll-a, and nutrients. Ice processes effects are
accounted for using output from the River 1D Ice Processes Model (in coordination with
the Ice Processes Study).
3. STUDY AREA
As established in RSP Section 5.6.3, the study area begins at PRM 19.9 and extends past the
proposed dam site to PRM 235.2; data collection sites are described in Table 3-1. The distribution
of data collection sites for the Susitna Basin also is shown in Figure 3-1. These data were used in
the calibration of the EFDC water quality model.
As described in Study 5.6 ISR, Part C, Section 7.1.1.1, a decision point was considered in 2014
regarding extension of the water quality modeling downstream of PRM 29.9 (AEA 2014e). On
September 30, 2014, AEA filed with FERC the Water Quality and Lower River Modeling
Technical Memorandum (AEA 2014a), which provided results of the analysis. Based on the small
difference between pre and post-Project temperatures at PRM 29.9 and similar small changes in
DO based on observed saturation, extension of the water quality model downstream of PRM 29.9
was not recommended.
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4. METHODS AND VARIANCES
4.1. Methods
4.1.1. Model Selection
During 2013, AEA selected a 3-dimensional Reservoir Water Quality Model, a 2-dimensional
River Water Quality Model, and a (2-D) River Water Quality Model with Enhanced Resolution
Focus Areas for this Project. The rationale for selection of the Reservoir and River Water Quality
models is set forth in Section 5.6.4.6 of the RSP (AEA 2012).
Section 5.6.4 in the RSP provides a detailed discussion of the model selection factors and
evaluation based on technical, regulatory, and management criteria (AEA 2012). The three
modeling systems evaluated were H2OBAL/SNTEMP/DYRESM, CE-QUAL-W2, and the
Environmental Fluid Dynamics Code (EFDC) model. The EFDC model was selected to implement
the study. It is capable of simulating both reservoir and river environments; includes
hydrodynamics, water temperature, water quality, and sediment transport modules; and considers
ice formation and breakup.
4.1.2. Reservoir and Downstream River Modeling Approaches
The reservoir and riverine modeling approaches are described in ISR Part A, Section 4.2. In 2014,
AEA continued with the modeling approaches as described in the ISR. The downstream riverine
model boundary was determined to be PRM 29.9 in the Water Quality and Lower River Modeling
Technical Memorandum (AEA 2014a).
4.1.3. Focus Area Modeling
Focus area (FA) modeling was described in ISR Part A, Sections 4.3 and 5.4 (AEA 2014c).
4.1.4. Scales for Modeling and Resolution of the Output
The scales for modeling and output resolution are discussed in ISR Part A, Section 4.4 (AEA
2014c). Model domain and spatial resolution can differ at points along the river depending on
channel width and complexity. The cell sizes for the reservoir model, river model, and FA-128
(Slough 8A) model are presented below.
Reservoir model
o Cell width: 357–2,953 feet
o Average width: 1,690 feet
o Cell length: 8–560 feet
o Average length: 230 feet
River model
o Cell width: 87–567 feet
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o Average width: 244 feet
o Cell length: 1,066–2,206 feet
o Average length: 1,599 feet
FA-128 (Slough 8A) model
o Cell width: 50–111.5 feet
o Average width: 70 feet
o Cell length: 103–229 feet
o Average length: 145 feet
4.1.5. Selection of Model State Variables and Options
The selection of model state variables and outputs is summarized in ISR Part A, Section 5.1 and
ISR Part B (AEA 2014c; AEA 2014d).
4.2. Variances from Study Plan
No variances from the established methods occurred during the implementation of this study in
2014.
5. RESULTS
5.1. Reservoir Model
The reservoir modeling is complicated because of pool level fluctuations of up to approximately
200 feet, in addition to complete drying of shallow areas of the reservoir. The outflow elevation in
the reservoir is based on movable vertical shutters to allow water withdrawals at multiple water
depths, allowing cooler water to be drawn from lower depths in the summer and warmer water to
be drawn from lower depths in the winter. The most extreme water withdrawal strategy scenario
is water being discharged from only the warmer reservoir surface where solar radiation is absorbed
during summer and early fall. Actual operation will likely differ from this scenario. The April 2014
Proof of Concept (POC) simulations of the reservoir model assumed that water withdrawn from
the entire intake elevation range resulted in discharge temperatures being lower than pre-Project
conditions during the summer months (Tetra Tech 2014a). This is not representative of planned
operations of the dam.
The POC model runs simulated reservoir discharge and temperature to show how model results
would be transferred to other study components. The results from the POC were discussed at the
April 2014 Technical Work Group meetings (Tetra Tech 2014a). The model runs simulated the
1974–1976 period (a dry period with a large pool drawdown) and the 1979–1981 period (a wet
period with a small pool drawdown). Pre-Project river flow and temperature were used as upstream
boundary conditions for the reservoir model.
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As discussed in Section 1.1 of Study 8.5 ISR, Part C Appendix N (AEA 2014b), the POC reservoir
model was robust and demonstrated that vertical resolution captures thermal stratification and
mixing processes in the reservoir model. Plots from the POC model runs are provided in Appendix
A.
5.2. River Model
The POC model runs were discussed at the April 2014 Technical Work Group meetings (Tetra
Tech 2014b). For the model runs, the pre-Project conditions upstream river temperature boundary
was based on a 3-year synthesized temperature record that correlated observed temperatures with
time of year and river flow. The upstream boundary post-Project conditions were taken from the
reservoir model. As discussed in Section 1.2 of Study 8.5 ISR, Part C Appendix N (AEA 2014b),
although the results should not be considered as representative of future conditions in the river, the
POC indicated that the river model was stable and had an acceptable run-time performance for
decadal time scale simulations. Plots from the POC model runs are provided in Appendix A. The
Baseline Water Quality Study (Study 5.5) and Water Quality Modeling Study (Study 5.6): Water
Quality and Lower River Modeling Technical Memorandum (AEA 2014a) include additional
modeling results for the river model at the dam site, PRM 125, PRM 60, and PRM 29.9.
After the POC modeling, the river model was calibrated against high-frequency temperature
monitoring data at seven stations (PRM 152.7, PRM 152.2, PRM 142.3, PRM 140, PRM 88.3,
PRM 87.8, and PRM 59.9). The locations of the monitoring sites are shown in Figure 3-1. The
monitoring data are available for different periods between July 2012 and September 2013. The
results of the model calibration versus the observed temperature data are presented in Figures 5.2-
1 and 5.2-2. The plots present the modeled and observed temperature data as a function of the days
since the model run began on December 31, 2009, with the plots starting with July 18, 2012 (Day
930) and running through October 2013.
Figures 5.2-1 and 5.2-2 indicate the model predicts the temperature well. The model is able to
represent the general magnitude and trend of observed temperature data and will be able to be used
to predict potential impacts of the proposed Project and operations. On an annual basis, the data
show that 2013 had higher water temperatures at all stations, and the model was able to predict
that pattern. The model reproduces short-term magnitude and variability of water temperature as
well.
The model determined that the simulated water temperatures in the Susitna River are sensitive to
the magnitude and timing of temperature in the boundary conditions, indicating that the uncertainty
in the boundary condition can influence the simulated temperature. Since the data available to
accurately represent the boundary conditions are limited, considerable uncertainties are present in
the simulated temperature, particularly the details in short-term behavior. In this case, the best way
to evaluate model performance is through visual comparison, which looks at identifying the pattern
and trend rather than point-to-point comparison. This process is used with hydrodynamic and water
quality models across the country.
Slight differences in model results from observed data can be attributed to uncertainty from the
model boundary conditions, as well as in the observed data. In addition, the observed data might
have specific local conditions that deviate from the general pattern. For example, the observed
temperature at PRM 88.3 is low and below 12 degrees Celsius (°C), but at PRM 87.8 (0.5 miles
downstream), the observed temperature becomes significantly higher (almost 15 °C). While the
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FERC Project No. 14241 Page 6 November 2015
model is able to reproduce the temperature at PRM 88.3 well, it cannot reproduce the higher
temperatures at PRM 87.8 during the same period. PRM 87.8 is likely under the influence of local
conditions or is not representative (e.g., the location of the Talkeetna Wastewater Treatment
Facility outfall). Similarly, the high temperature at PRM 59.9 might be partly explained by local
conditions given that with the flow rate and water volume during the period, the solar radiation
would not have the ability to increase water temperature to that degree from the previous upstream
observations.
In general, the model is adequately calibrated for temperature. Future refinement in calibration
might be possible during the water quality model calibration process.
5.3. FA-128 (Slough 8A) Model
The Focus Area models will have higher-resolution than the full river model. The FA-128 (Slough
8A) mode, located from PRM 129.7 to PRM 128.1, was configured separately from the full river
model. The full river model was used to determine the upstream and downstream boundary
conditions for FA-128.
The POC model runs were discussed at the April 2014 Technical Work Group meetings (Tetra
Tech 2014c). Section 1.3 of Study 8.5 ISR, Part C Appendix N contains a discussion of the POC
FA-128 (Slough 8A) results (AEA 2014b). Plots from the POC model runs are provided in
Appendix A of this report. No additional modeling has occurred.
6. DISCUSSION
Although the POC results should not be considered as representative of future conditions in the
reservoir and river, they indicated that the models are robust and provide physically realistic
simulation of water surface elevation, velocity, and temperature (Tetra Tech 2014a, 2014b, 2014c;
AEA 2014b). In addition, the reservoir POC model demonstrated that vertical resolution captures
thermal stratification and mixing processes in the reservoir model.
The models have been tested with potential Project flow scenarios to demonstrate stability and
acceptable run-time performance. Test data sets for water temperature generated in 2012 have been
used in both the reservoir and riverine models, which are capable of decade time scale simulations.
The same data sets were extended into 2013 to verify and further refine model calibration.
Temperature data from 2014 was not available during POC modeling.
As described in Study 5.6 ISR, Part C, Section 7.1.1.1, a decision point was considered in 2014
regarding the extension of the water quality modeling downstream of PRM 29.9 (AEA 2014e).
Based on the minor difference between pre and post-Project temperatures at PRM 29.9 and similar
minor changes in DO based on observed saturation, extension of the water quality model
downstream of PRM 29.9 was not recommended.
The Baseline Water Quality Study (Study 5.5) and Water Quality Modeling Study (Study 5.6):
Water Quality and Lower River Modeling Technical Memorandum included additional modeling
results for the river model at the dam site, PRM 125, PRM 60, and PRM 29.9 (AEA 2014a).
After the POC modeling, the river model was calibrated using temperature data from 2012 and
2013, as the 2014 temperature data was not available. The 2014 data will be used for future model
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validation. The model reproduces short-term magnitude and variability of water temperature, as
shown in Figures 5.2-1 and 5.2-2. The model is considered acceptably calibrated for temperature.
Though not part of the water quality model development, the interpretation of model results of
suspended sediment concentrations in relation to turbidity will be required to evaluate potential
Project effects. The initial evaluation of correlations between total suspended solids (TSS) and
turbidity is included as Attachment 1 of this report.
7. CONCLUSION
AEA has made extensive progress in implementing the water quality modeling study, which
provides the groundwork for completing the development of the reservoir and riverine models.
The reservoir, riverine, and FA-128 (Slough 8A) models have been configured and tested, as
shown in the POC modeling (Tetra Tech 2014a, 2014b, 2014c). The POC included spatial
configuration of each model to run a multiyear hydrodynamic and temperature simulation. Based
upon the work already completed, AEA expects to achieve the objectives for the Water Quality
Monitoring Study (Section 2), in addition to work identified in Study 5.6 ISR Part D Section 8
(AEA 2014f). No additional field work is planned or deemed necessary at this time, as the data is
sufficient to complete the modeling.
8. LITERATURE CITED
AEA (Alaska Energy Authority). 2012. Revised Study Plan: Susitna-Watana Hydroelectric Project
FERC Project No. 14241. December 2012. Prepared for the Federal Energy Regulatory
Commission by the Alaska Energy Authority, Anchorage, Alaska. http://www.susitna-
watanahydro.org/study-plan.
AEA (Alaska Energy Authority). 2014a. Baseline Water Quality Study (Study 5.5) and Water
Quality Modeling Study (Study 5.6): Water Quality and Lower River Modeling Technical
Memorandum. Prepared for the Federal Energy Regulatory Commission by the Alaska
Energy Authority, Anchorage, Alaska. http://www.susitna-watanahydro.org/wp-
content/uploads/2014/09/DRAFT-Tech-Memo_Baseline-Water-Quality-Decision-
Points.pdf
AEA (Alaska Energy Authority). 2014b. Fish and Aquatics Instream Flow Study (Study 8.5) Initial
Study Report. Part C: Appendix N. Middle River Fish Habitat and Riverine Modeling Proof
of Concept. Prepared for the Federal Energy Regulatory Commission by the Alaska Energy
Authority, Anchorage, Alaska. http://www.susitna-watanahydro.org/wp-
content/uploads/2014/06/08.5_IFS_ISR_PartC_2_of_2.pdf.
AEA (Alaska Energy Authority). 2014c. Water Quality Modeling Study, Study Plan Section 5.6.
Part A: Sections 1-6, 8-10. Prepared for the Federal Energy Regulatory Commission by the
Alaska Energy Authority, Anchorage, Alaska. http://www.susitna-watanahydro.org/wp-
content/uploads/2014/05/05.6_WQMOD_ISR_PartA.pdf.
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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AEA (Alaska Energy Authority). 2014d. Water Quality Modeling Study, Study Plan Section 5.6.
Part B: Supplemental Information (and Errata) to Part A (February 3, 2014 Draft Initial
Study Report). Prepared for the Federal Energy Regulatory Commission by the Alaska
Energy Authority, Anchorage, Alaska. http://www.susitna-watanahydro.org/wp-
content/uploads/2014/06/05.6_WQMOD_ISR_PartB.pdf.
AEA (Alaska Energy Authority). 2014e. Water Quality Modeling Study, Study Plan Section 5.6
Part C: Executive Summary and Section 7. Susitna-Watana Hydroelectric Project FERC
Project No. 14241. June 2014. Prepared for the Federal Energy Regulatory Commission
by the Alaska Energy Authority, Anchorage, Alaska. http://www.susitna-
watanahydro.org/wp-content/uploads/2014/06/05.6_WQMOD_ISR_PartC.pdf.
AEA (Alaska Energy Authority). 2014f. Water Quality Modeling Study, Study Plan Section 5.6.
Part D: Supplemental Information to June 2014 Initial Study Report. Prepared for the
Federal Energy Regulatory Commission by the Alaska Energy Authority, Anchorage,
Alaska.
Tetra Tech. 2014a. Reservoir Water Quality Modeling. PowerPoint Presentation, Riverine
Modeling Proof of Concept Meeting on April 15-17, 2014. Prepared for Alaska Energy
Authority, Anchorage, Alaska. Susitna-Watana Hydroelectric Project, FERC No. P-14241.
http://www.susitna-watanahydro.org/meetings/past-meetings/.
Tetra Tech. 2014b. Riverine Water Quality Modeling. PowerPoint Presentation, Riverine
Modeling Proof of Concept Meetings on April 15-17, 2014. Prepared for Alaska Energy
Authority, Anchorage, Alaska. Susitna-Watana Hydroelectric Project, FERC No. P-14241.
http://www.susitna-watanahydro.org/meetings/past-meetings/.
Tetra Tech. 2014c. Riverine Water Quality Modeling FA-128. PowerPoint Presentation, Riverine
Modeling Proof of Concept Meetings on April 15-17, 2014. Prepared for Alaska Energy
Authority, Anchorage, Alaska. Susitna-Watana Hydroelectric Project, FERC No. P-14241.
http://www.susitna-watanahydro.org/meetings/past-meetings/.
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9. TABLES
Table 3-1. Susitna River Basin Temperature and Water Quality Monitoring Sites.
Water Temperature Water Quality Monitoring
Historic Current Historic Current
PRM Description Latitude
(WGS84)
Longitude
(WGS84)
W S
S W S W S
W S
S W S
2012
2012
-
2013
2013
2013
-
2014
2014 2013
2013
-
2014
2014
19.9 Susitna above Alexander
Creek 61.43903 -150.48456 X X X X
29.9 Susitna Station 61.54428 -150.51556 X X X X X X X X X
32.51 Yentna River 61.587604 -150.48301 X X X X X X X X X X X
33.6 Susitna above Yentna 61.57595 -150.42741 X X X X X X X
45.11 Deshka River 61.710142 -150.32470 X X X X X X
59.9 Susitna 61.86220 -150.18463 X X X X X X X
87.8 Susitna at Parks Highway East 62.174531 -150.173677 X X X X X X X X
88.3 Susitna at Parks Highway
West 62.181096 -150.16787 X X X X X X X X X
99.2 LRX 1 62.306018 -150.108764 X X X X X
102.81 Talkeetna River 62.34243 -150.11266 X X X X X X
118.61 Chulitna River 62.567703 -150.23782 X X X X X X X X X X X
107 Talkeetna 62.39724 -150.13728 X X X X X X
116.7 LRX 18 62.526527 -150.114671 X X X X
124.2 Curry Fishwheel Camp 62.61783 -150.01373 X X X X X X
129.6 Slough 8A 62.670479 -149.903241 X X X X
129.9 LRX 29 62.673914 -149.899025 X X X
132.7 Slough 9 62.702358 -149.841895 X X X X
134.1 LRX 35 62.713854 -149.808926 X X X X
140 Susitna near Gold Creek 62.767054 -149.693532 X X X X X
140.11 Gold Creek 62.767892 -149.68978 X X X X X X X X X X
141.0 Slough 16B 62.780204 -149.68536 X X X X
142.21 Indian River 62.78635 -149.65878 X X X X X
142.3 Susitna above Indian River 62.785776 -149.64890 X X X X X X
143.6 Slough 19 62.793819 -149.614255 X X X X
143.6 LRX 53 62.79427 -149.61327 X X X X X
145.6 Slough 21 62.814667 -149.575329 X X X
152.2 Susitna below Portage Creek 62.830397 -149.382743 X X X X X
152.31 Portage Creek 62.830379 -149.380289 X X X
152.7 Susitna above Portage
Creek 62.827002 -149.
827002 X X X X X X
168.1 Susitna 62.791696 -148.993825 X X
183.1 Susitna below Tsusena Creek 62.81348 -148.656868 X X
184.81 Tsusena Creek 62.821783 -148.606809 X X X
187.2 Susitna at Watana Dam site 62.82260 -148.55300 X X X X X
196.8 Watana Creek 62.82960 -148.25900 X
209.2 Kosina Creek 62.78220 -147.94000 X X X X X
225.5 Susitna near Cantwell 62.70520 -147.53800 X
235.22 Oshetna River 62.63961 -147.383109 X X X X X X X
Notes:
PRM = Susitna River Project River Mile
W = Winter
S = Summer
* Indicates sampling location was a tributary to the Susitna River
1 indicates the Susitna River PRM at the confluence of the tributary (samples collected from the tributary)
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2 indicates an alternate monitoring location from PRM 225.5 due to river inaccessibility by helicopter during summer sample collection
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10. FIGURES
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Figure 3-1. Stream Water Quality and Temperature Data Collection Sites for the Susitna-Watana Hydroelectric Project.
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Figure 5.2-1. River Model Temperature Calibration Plots (PRM 152.7, 152.2, 142.3, 140).
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Figure 5.2-2. River Model Temperature Calibration Plots (PRM 88.3, 87.8, 59.9).
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APPENDIX A: APRIL 2014 PROOF OF CONCEPT RESULT PLOTS
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LIST OF FIGURES
Figure A-1. Proof of Concept 1974–1976 Simulation Boundary Conditions River Model
Discharge and Temperature Results at Dam Site. ................................................................... 1
Figure A-2. Proof of Concept 1979–1981 Simulation Boundary Conditions River Model
Discharge and Temperature Results at Dam Site. ................................................................... 2
Figure A-3. Proof of Concept 1974–1976 Simulation Boundary Conditions River Model
Temperature Results. ............................................................................................................... 3
Figure A-4. Proof of Concept 1974–1976 Comparison of Pre- and Post-Project Temperature at
FA-128 (Slough 8A) (RM131/RM127.8). ............................................................................... 4
Figure A-5. Proof of Concept 1976–1981 Simulation Boundary Conditions River Model
Temperature Results. ............................................................................................................... 5
Figure A-6. Proof of Concept 1979–1981 Comparison of Pre- and Post-Project Temperature at
FA-128 (Slough 8A) (RM131/RM127.8). ............................................................................... 6
Figure A-7. Proof of Concept May–October 1976 Comparison of Pre- and Post-Project
Discharge and Temperature at FA-128 (Slough 8A). .............................................................. 7
Figure A-8. Proof of Concept May–October 1981 Comparison of Pre- and Post-Project
Discharge and Temperature at FA-128 (Slough 8A). .............................................................. 8
Figure A-9. Proof of Concept 1974–1976 Simulation Boundary Conditions Reservoir Model
Discharge and Temperature Results at Dam Site. ................................................................... 9
Figure A-10. Proof of Concept 1979–1981 Simulation Boundary Conditions Reservoir Model
Discharge and Temperature Results at Dam Site. ................................................................. 10
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-1. Proof of Concept 1974–1976 Simulation Boundary Conditions River Model Discharge and
Temperature Results at Dam Site.
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-2. Proof of Concept 1979–1981 Simulation Boundary Conditions River Model Discharge and
Temperature Results at Dam Site.
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-3. Proof of Concept 1974–1976 Simulation Boundary Conditions River Model Temperature Results.
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-4. Proof of Concept 1974–1976 Comparison of Pre- and Post-Project Temperature at FA-128 (Slough
8A) (RM131/RM127.8).
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-5. Proof of Concept 1976–1981 Simulation Boundary Conditions River Model Temperature Results.
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-6. Proof of Concept 1979–1981 Comparison of Pre- and Post-Project Temperature at FA-128 (Slough
8A) (RM131/RM127.8).
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-7. Proof of Concept May–October 1976 Comparison of Pre- and Post-Project Discharge and
Temperature at FA-128 (Slough 8A).
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-8. Proof of Concept May–October 1981 Comparison of Pre- and Post-Project Discharge and
Temperature at FA-128 (Slough 8A).
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-9. Proof of Concept 1974–1976 Simulation Boundary Conditions Reservoir Model Discharge and
Temperature Results at Dam Site.
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Note: Proof of Concept model runs assumed reservoir water withdraw from the entire intake elevation range, which is not
representative of planned operation of the dam.
Figure A-10. Proof of Concept 1979–1981 Simulation Boundary Conditions Reservoir Model Discharge and
Temperature Results at Dam Site.
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Attachment 1: Relationship between Turbidity and Total Suspended Solids:
A Correlation Model Plots
Susitna-Watana Hydroelectric Project
(FERC No. 14241)
Water Quality Modeling Study
Study Plan Section 5.6
2014 Study Implementation Report
Attachment 1
Relationship between Turbidity and Total Suspended
Solids: A Correlation Model
Prepared for
Alaska Energy Authority
Prepared by
Tetra Tech, Inc.
November 2015
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TABLE OF CONTENTS
1. Introduction ....................................................................................................................... 1
2. Study Objectives................................................................................................................ 1
3. Study Area ......................................................................................................................... 1
4. Methods .............................................................................................................................. 2
4.1. Background Information ......................................................................................... 2
4.2. Existing Models of Turbidity and TSS Relationships ............................................ 2
4.3. Method for Relationship Development ................................................................... 3
5. Results ................................................................................................................................ 3
6. Summary and Discussion ................................................................................................. 4
7. Literature Cited ................................................................................................................ 5
8. Figures ................................................................................................................................ 7
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LIST OF FIGURES
Figure 3-1. Susitna River Study Area and Large-scale River Segments. ...................................... 7
Figure 5-1a. Distribution of turbidity at cross-sectional sampling sites throughout the Susitna
River. ....................................................................................................................................... 8
Figure 5-1b. Distribution of TSS at cross-sectional sites throughout the Susitna River. ............... 9
Figure 5-2a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River,
Summer 2013 – Winter 2014 (using full turbidity range). .................................................... 10
Figure 5-2b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River,
Summer 2013 – Winter 2014 (using full turbidity range). .................................................... 10
Figure 5-2c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River,
Summer 2013 – Winter 2014 (using full turbidity range) ..................................................... 11
Figure 5-3a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, on a
log-log scale, compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
............................................................................................................................................... 12
Figure 5-3b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, on a
log-log scale, compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
............................................................................................................................................... 12
Figure 5-3c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, on a
log-log scale, compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
............................................................................................................................................... 13
Figure 5-4a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). ........................... 14
Figure 5-4b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). ........................... 14
Figure 5-4c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). ........................... 15
Figure 5-5a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, on a
log-log scale, Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). .... 16
Figure 5-5b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, on a
log-log scale, Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). .... 16
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Figure 5-5c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, on a
log-log scale, Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs). .... 17
Figure 6-1. Power relationships (log-log) developed for the three Susitna River Segments. ....... 18
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LIST OF ACRONYMS, ABBREVIATIONS, AND DEFINITIONS
Abbreviation Definition
AEA Alaska Energy Authority
EFDC Environmental Fluid Dynamics Code
FERC Federal Energy Regulatory Commission
ILP Integrated Licensing Process
mg/L Milligrams per Liter
NTU Nephelometric Turbidity Unit
PRM Project River Mile
Project Susitna-Watana Hydroelectric Project
RSP Revised Study Plan
SPD Study Plan Determination
SSC SSC Suspended Sediment Concentration
TSS Total Suspended Solids
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1. INTRODUCTION
The Alaska Energy Authority (AEA) is preparing a License Application that will be submitted to
the Federal Energy Regulatory Commission (FERC) for the Susitna-Watana Hydroelectric Project
(Project) using the Integrated Licensing Process (ILP). The Project is located on the Susitna River,
an approximately 300-mile-long river in Southcentral Alaska. The Project’s dam site would be
located at Project River Mile (PRM) 187.1.
On December 14, 2012, AEA filed its Revised Study Plan (RSP) with the FERC for the Susitna-
Watana Hydroelectric Project (FERC Project No. 14241), which included 58 individual study
plans (AEA 2012). Included with the RSP are the Baseline Water Quality Study (RSP Study 5.5)
and the Water Quality Modeling Study (RSP Study 5.6). The collective goal of the water quality
studies is to assess the effects of the proposed Project and its operations on water quality in the
Susitna River basin, which will inform development of any appropriate conditions for inclusion in
the Project license. Study 5.5 focuses on data collection and documenting physical water quality
along the Susitna River. Predicting the potential impacts of the dam and its proposed operations
on water quality requires the development of a water quality model. The goal of Study 5.6 is to
utilize the extensive information collected from the Baseline Water Quality Study to develop a
model(s) to evaluate the potential impacts of the proposed Project and operations on various
physical parameters within the Susitna River watershed.
On April 1, 2013 FERC issued its study determination (April 1 SPD) for the Revised Study Plan
(RSP) Section 5.6 with modifications.
This technical memorandum describes the development of the relationships between total
suspended solids (TSS) concentrations and turbidity in the Susitna River that will be applied to
TSS model results to estimate turbidity.
2. STUDY OBJECTIVES
The objective of this technical memorandum is to describe the development of a relationship(s)
that estimates turbidity from total suspended solids (TSS) concentrations. This relationship will be
used to convert TSS results from the EFDC (Tetra Tech 2007a, b and c) model to turbidity as part
of the Water Quality Modeling Study (Study 5.6).
3. STUDY AREA
As established by RSP Section 5.5.3, the study area for water quality monitoring includes the
Susitna River from PRM 29.9 to PRM 235.2 (Oshetna River), and selected tributaries within the
proposed transmission lines and access corridors. The study area is shown in Figure 3-1.
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4. METHODS
4.1. Background Information
Total suspended solids (TSS) are particles in the water column larger than 2 μm (smaller particles
are considered dissolved). TSS therefore, refers to that portion of the total sediment load of rivers
that is carried in suspension in the water column. This portion can include a wide variety of
particles – such as, sand, silt, clay, and algae – that settle at varying rates depending on the water
velocity as well as the size and weight of the particles. Turbidity is an optical measurement of the
quantity of light absorbed or scattered by particles in a sample of water, and is measured in
nephelometric turbidity units (NTUs, Duchrow and Everhart 1971; McCluney 1975). Turbidity
and TSS are typically generated by the re-suspension of bottom sediments and the erosion and
transport of inorganic particles from the surrounding watershed to rivers and streams (Wetzel
2001). However, in the Susitna River turbidity is also due in large part to the presence of glacial
rock flour (Peratrovich et al. 1982). Even small quantities of suspended sediment can substantially
affect turbidity in water (Duchrow and Everhart 1971). Because of the numerous factors that affect
turbidity there is no universal relationship between TSS and turbidity (Davies-Colley and Smith
2001). As a result, river-specific relationships have to be developed (e.g., Lloyd et al. 1987).
4.2. Existing Models of Turbidity and TSS Relationships
Although turbidity and TSS are strongly related, and turbidity is often used to indicate changes in
TSS concentration in water, the two parameters are not typically related by a 1:1 ratio. This may
be due to variation in sediment types (Duchrow and Everhart 1971) and size fractions, and the fact
that turbidity does not include settled solids, and, conversely, TSS does not include colored
dissolved organic matter (Davies-Colley and Smith 2001; Chen et al. 2006; Wood 2014).
Lloyd et al. (1987) described relationships between suspended sediment concentration (total non-
filterable residue) and resulting turbidity from Alaskan streams. The authors developed three
relationships to determine if turbidity criteria could provide reasonable approximations of water
quality criteria based on suspended sediment concentrations. Using data from 34 Alaskan rivers
(including the Susitna River) that was compiled by the U.S. Geological Survey during the period
1976-1983 (May-October), they found a significant correlation between suspended sediment
concentration (SSC) and turbidity (r2 = 0.83) as shown by Equation (1). The data were log/log
transformed. A similar relationship was developed specifically for the Susitna River
(Peratrovich et al. 1982) as shown by Equation (2). Another example of a river-specific
relationship was developed by Barrett et al. (1992), as shown by Equation (3) (r2 = 0.94; P<0.001)
using experimental sample data. This third relationship was used in a study investigating reactive
distance and pursuit speed of fish during foraging.
T = 0.44(SSC)0.858 (1)
T = 0.185(SSC)0.998 (2)
SSC = 3.399(T) - 5.603 (3)
Where, T = turbidity (NTU) and SSC = suspended sediment concentration (mg/L)
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4.3. Method for Relationship Development
Geologic formations with distinct ages and structures have a major effect on water quality
conditions along all three of the defined river segments. The morphologic characteristics of the
Upper Susitna River (above PRM 187.1) are dominated by the products of Quaternary-age
glaciation. The Middle Susitna River segment (from PRM 187.1 to PRM 102.4) is heavily
influenced by bedrock outcrops as well as Quaternary-age glaciations. The Lower Susitna River
segment (below PRM 102.4) is dominated by sediment loading from the major tributaries
(Chulitna and Talkeetna Rivers) and variable resistance to erosion of the Pleistocene-age,
glacially-derived materials including tills (moraines), glacio-fluvial sediments in various elevation
outwash-surfaces and glacio-lacustrine sediments that control the width of the valley. Therefore,
this analysis considers the three Susitna River segments separately.
Another consideration for developing the relationships is whether to segregate the data by open-
water flow periods versus winter conditions. There is a significant difference in both TSS and
turbidity between winter and summer because the supply of glacially-derived sediments is
drastically reduced during the winter. Because the relationships will be used to evaluate potential
Project effects, it was decided that ice-covered and open-water data would be combined. This is
because the reservoir would retain, mix, and release water year-round and the release flows would
include upstream flow from each flow period.
The procedure for developing the relationships is a simple correlation of the paired TSS and
turbidity samples collected in the three Susitna River segments. As illustrated by Equations 1, 2,
and 3, linear and power relationships will be considered.
5. RESULTS
As part of the Baseline Water Quality Study (Study 5.5), turbidity (NTU) and total suspended
solids (TSS) concentrations were measured monthly at 17 sampling locations within the study area
in 2013 and 2014, resulting in 281 observations of each parameter. Using these data, significant
relationships were determined with data from the Upper (n=57), Middle (n=119) and Lower
(n=105) River segments. This section details the correlation models relating turbidity (NTU) and
total suspended solids (mg/L), as measured in water samples collected throughout the Susitna
Basin during field sampling in 2013 and during winter 2014.
The range in turbidity and TSS values in the main Susitna River in 2013 and 2014 was large.
Observed turbidity levels ranged from 1.5-4 NTU (in the very clear waters of the Deshka River)
to more than 1,000 NTU in the mainstem (Figure 5-1a), and the observed range in TSS
concentrations was similar and also exceeded 1,000 mg/L (Figure 5-1b).
The Susitna data for summer 2013 and winter 2014 were separated among the Lower River (data
collected between PRM 29.1 to 101.8), Middle River (data collected between PRM 103.9 to 187.1)
and the Upper River segments (data collected above PRM 187.1). All data for both summer and
winter periods are included because the winter data provide the lower end of the TSS/Turbidity
range and the open water flows provide the high end and because the relationships will be used for
with-Project conditions that will consist of water sourced throughout the year.
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The linear relationships between TSS and turbidity were stronger (r² > 0.9) in the Middle and
Upper River segments than in the Lower River (r2<0.8) (Figure 5-2a, b, c). The estimate of
turbidity NTUs from TSS was nearly 1:1 for all three Susitna River segments. For Upper and
Middle River data (Figures 5-2c and 5-2b) the relationships tend to be slightly, though consistently
higher than the observed turbidity when the observations are less than 200 NTU. This trend was
even more exaggerated in the Lower River (Figure 5-2a).
The strength of the relationship between TSS and turbidity for all three river sections increased if
data were log transformed (Figure 5-3a, b, c). With the log transformation, the coefficients of
determination (r²) were about 0.97 for Upper and Middle River data and 0.95 for the Lower River
data. These figures illustrate that turbidity and TSS approach zero together and that there is an
approximate 1:1 relationship between TSS and turbidity in the three segments with coefficients
ranging from 0.62 to 1.04 and exponents ranging from 0.97 to 1.07. The relationship for the Lower
Susitna River (Figure 5-3a) segment still shows general under-prediction of turbidity in the 100 to
200 NTU range but this is not readily evident for the other segments.
Previous models (Equations 1 and 2) that were developed with data from Alaskan rivers (Equation
1 data from several Alaska rivers; Equation 2 data from the Susitna River basin) appear to
substantially underestimate turbidities predicted from observed TSS values when compared to the
present models for the 3 river segments (Figure 5-3a, b, c).
Relationships were also developed for data only in the 0 to 200 NTU range because of the tendency
of the relationships to over-predict in that range, especially for the Lower River. The linear
equations of Lower and Middle river data with 0 – 200 NTU had relatively high r²s of 0.88 and
0.95, respectively (Figure 5-4a and 5-4b). A couple of outlying data points produced a weaker fit
for the Upper River model, which had an r² of 0.67 (Figure 5-4c). Log-log transformations
improved the relationship between turbidity and TSS for turbidities between 0 and 200 NTU for
both the Upper and Lower river data, but not for the Middle River data (Figures 5-5a, 5-5b, 5-5c).
6. DISCUSSION
The correlations developed from the 2013 and 2014 data collected by the Baseline Water Quality
Study (5.5) between TSS and turbidity are quite strong and will allow accurate predictions of
turbidity over a large range of suspended solid concentrations. Separate regression models were
constructed for turbidity versus TSS for each of the river segments: Lower River, Middle River,
and Upper River. The Lower River linear regression model showed greater variation in the TSS-
turbidity relationship in the mid-range (400 – 1,000) of the set of observations (Figure 5-2a). This
was in contrast to the Middle River and Upper River models (Figure 5-2b and Figure 5-2c,
respectively) both of which had higher r2 values (amount of variation explained by the regression
model).
For all segments, observed variability in turbidity levels increased above TSS concentrations of
100 mg/L, with the greatest variability between predicted and observed turbidity values occurring
in the Lower River. This is expected based on there being three distinct sources (Middle Susitna,
Chulitna, and Talkeetna Rivers) of suspended sediment in the Lower River.
There is actually very little difference in the resulting equations. As illustrated in Figure 6-1, the
six power relationships (the three river segments using the complete data sets and the three river
segments using only <200 NTU data), only the Lower River equation for lower NTUs differs. The
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selection of the final equation or equations will consider combining data from the Middle and
Upper Susitna River segments and whether a greater emphasis should be placed on the lower
turbidity data because this will likely be the range most frequently encountered under with-Project
conditions and because this range is likely to be important for habitat analysis. Therefore, final
selection will be made in coordination with the Study 8.5 (Fish and Aquatics Instream Flow Study).
7. LITERATURE CITED
Alaska Energy Authority (AEA). 2012. Revised Study Plan: Susitna-Watana Hydroelectric
Project FERC Project No. 14241. December 2012. Prepared for the Federal Energy
Regulatory Commission by the Alaska Energy Authority, Anchorage,
Alaska. http://www.susitna-watanahydro.org/study-plan.
Barrett J.D., G.D. Grossman, and J. Rosenfeld. 1992. Turbidity-induced changes in reactive
distance in rainbow trout. Transactions of the American Fisheries Society 121:437-443.
Chen, Z., Hu, C., and Muller-Karger, F. 2006. Monitoring turbidity in Tampa Bay using
MODIS/Aqua 250-m imagery. Remote Sensing of Environment 109(2): 207-220.
Davies-Colley, R. J., and D. G. Smith. 2001. Turbidity, suspended sediment, and water clarity: a
review. Journal of the American Water Resources Association 37(5):1085-1101.
Duchrow, R.M. and W.H. Everhart. 1971. Turbidity measurements. Transactions of the American
Fisheries Society 100: 682-690.
Lloyd, Denby S., Jeffery P. Koenings, and Jacqueline D. LaPerriere. 1987. Effects of turbidity in
fresh waters of Alaska. North American Journal of Fisheries Management 7: 18-33.
McCluney, W.R. 1975. Radiometry of water turbidity measurements. Journal of the Water
Pollution Control Federation 47: 252-266.
Peratrovich, Nottingham, and Drage. 1982. Susitna reservoir sedimentation and water clarity
study. Susitna Hydroelectric Project, Alaska Power Authority. Anchorage, AK.
Tetra Tech, Inc. 2007a. The Environmental Fluid Dynamics Computer Code Theory and
Computation: Volume 1 Hydrodynamic and Mass Transport. Tetra Tech, Inc., Fairfax,
VA.61 pp.
Tetra Tech, Inc. 2007b. The Environmental Fluid Dynamics Computer Code Theory and
Computation: Volume 2 Sediment and Contaminant Transport and Fate. Tetra Tech, Inc.,
Fairfax, VA.96 pp.
Tetra Tech. 2007c. The Environmental Fluid Dynamics Computer Code, Theory and Computation:
Volume 3: Water Quality and Eutrophication. Tetra Tech, Inc., Fairfax, VA.
Wetzel, R.G. 2001. Limnology: Lake and River Ecosystems, 3rd Edition. Academic Press, New
York, NY. 1006 pp.
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Susitna-Watana Hydroelectric Project Alaska Energy Authority
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Wood, M.S., 2014, Estimating suspended sediment in rivers using acoustic Doppler meters: U.S.
Geological Survey Fact Sheet 2014-3038, 4 p. Available at:
http://dx.doi.org/10.3133/fs20143038.
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
Susitna-Watana Hydroelectric Project Alaska Energy Authority
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8. FIGURES
Figure 3-1. Susitna River Study Area and Large-scale River Segments.
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
Susitna-Watana Hydroelectric Project Alaska Energy Authority
FERC Project No. 14241 Attachment 1 - Page 8 November 2015
Figure 5-1a. Distribution of turbidity at cross-sectional sampling sites throughout the Susitna River.
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
0
5
10
15
20
25
30
35
40
45
50
10701301902503103704304905506106707307908509109701030109011501210127013301390MoreFrequencyTurbdity (NTU)
Histogram
Frequency Cumulative %
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
Susitna-Watana Hydroelectric Project Alaska Energy Authority
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Figure 5-1b. Distribution of TSS at cross-sectional sites throughout the Susitna River.
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
0
5
10
15
20
25
30
0408012016020024028032036040044048052056060064068072076080084088092096010001040108011201160120012401280132013601400MoreFrequencySuspended Sediment (mg/L)
Histogram
Frequency Cumulative %
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-2a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, Summer 2013 –
Winter 2014 (using full turbidity range).
Figure 5-2b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, Summer 2013 –
Winter 2014 (using full turbidity range).
y = 0.7996x + 67.792
R² = 0.7818
0
200
400
600
800
1000
1200
1400
0 200 400 600 800 1000 1200 1400 1600Turbidity (NTUs)Total Suspended Sediment (mg/L)
y = 0.8781x + 29.906
R² = 0.943
0
200
400
600
800
1000
1200
0 200 400 600 800 1000 1200 1400Turbidity (NTUs)Total Suspended Sediment (mg/L)
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-2c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, Summer 2013 –
Winter 2014 (using full turbidity range)
y = 0.9726x + 2.4071
R² = 0.9643
0
100
200
300
400
500
600
700
0 100 200 300 400 500 600 700Turbidity (NTUs)Total Suspended Sediment (mg/L)
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-3a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, on a log-log scale,
compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
Figure 5-3b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, on a log-log scale,
compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
y = 1.0487x0.9735
R² = 0.9507
0.1
1
10
100
1000
10000
0.1 1 10 100 1000 10000Turbidity (NTUs)Total Suspended Sediment (mg/L)
Lower River Equation 1 Equation 2
y = 0.8581x1.0204
R² = 0.9671
0.1
1
10
100
1000
10000
0.1 1 10 100 1000 10000Turbidity (NTUs)Total Suspended Sediment (mg/L)
Middle River Equation 1 Equation 2
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Figure 5-3c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, on a log-log scale,
compared to turbidity predicted from Equation 1 and Equation 2 (Section 4.2).
y = 0.6215x1.0737
R² = 0.9702
0.1
1
10
100
1000
1 10 100 1000Turbidity (NTUs)Total Suspended Sediment (mg/L)
Upper River Equation 1 Equation 2
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-4a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, Summer 2013 –
Winter 2014 (using turbidity between 0 and 200 NTUs).
Figure 5-4b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, Summer 2013 –
Winter 2014 (using turbidity between 0 and 200 NTUs).
y = 0.564x + 8.4217
R² = 0.8797
0
20
40
60
80
100
120
140
160
180
200
0 50 100 150 200 250 300Turbidity (NTUs)Total Suspended Sediment (mg/L)
y = 0.7298x + 17.91
R² = 0.9485
0
20
40
60
80
100
120
140
160
180
200
0 50 100 150 200 250 300Turbidity (NTUs)Total Suspended Sediment (mg/L)
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-4c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, Summer 2013 –
Winter 2014 (using turbidity between 0 and 200 NTUs).
y = 0.7604x + 6.563
R² = 0.6715
0
20
40
60
80
100
120
140
160
180
200
0 20 40 60 80 100 120 140 160Turbidity (NTUs)Total Suspended Sediment (mg/L)
2014 STUDY IMPLEMENTATION REPORT WATER QUALITY MODELING STUDY (STUDY 5.6)
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Figure 5-5a. Relationship between TSS and Turbidity (NTUs) in the Lower Susitna River, on a log-log scale,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs).
Figure 5-5b. Relationship between TSS and Turbidity (NTUs) in the Middle Susitna River, on a log-log scale,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs).
y = 1.3896x0.8422
R² = 0.9831
0.1
1
10
100
1000
0.1 1 10 100 1000Turbidity (NTUs)Total Suspended Sediment (mg/L)
y = 0.8195x1.0217
R² = 0.9523
0.1
1
10
100
1000
0.1 1 10 100 1000Turbidity (NTUs)Total Suspended Sediment (mg/L)
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Figure 5-5c. Relationship between TSS and Turbidity (NTUs) in the Upper Susitna River, on a log-log scale,
Summer 2013 – Winter 2014 (using turbidity between 0 and 200 NTUs).
y = 0.664x1.0442
R² = 0.9323
0.1
1
10
100
1000
1 10 100 1000Turbidity (NTUs)Total Suspended Sediment (mg/L)
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Figure 6-1. Power relationships (log-log) developed for the three Susitna River Segments.