Title: SJR DWSC DO Modeling HydroQual, Inc' Andy Thuman, P'E' Laurie De Rosa
1SJR DWSC DO ModelingHydroQual, Inc.Andy
Thuman, P.E.Laurie De Rosa
SJR Technical Working GroupMay 16, 2006
2SJR Models Study Area
- Downstream
- DSM2-delta
- ECOMSED/RCA
- Tidal portion from Vernalis to Jersey Island
- Upstream
- DSM2-sjr
- Free-flowing portion from Stevinson to Vernalis
Source Kratzer, et al. (2004) USGS WRI-03-4127
3Model Grid
R1
4Modeling Effort
- Models calibrated/validated from 2000-2001 on a
continuous basis - Hydrodynamic model includes tidal transport and
calculation of temperature - Water quality model uses tidal transport and
includes the following parameters - EC, BOD, DO, eutrophication (nutrients
phytoplankton), TSS
5Model Calibration Period Flows
1923-2002
Annual Average
2001
Summer Average (J-S)
Model Period
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8DWSC Hydrodynamic Modeling
- Hydrodynamic model calibration
- Model output compared to observed stage, flow
temperature - Compares well with data and DSM2 output
- Reproduces daily temperature stratification
- Further work may be needed in the Turning Basin
near Old River/Mossdale
9Temperature Calibration
10Temperature Calibration
2002 Data near R5
2001 Model near R5
11Flow Calibration
Increased Old River flow between Jun-Aug by 530
cfs
12DWSC Water Quality Modeling
- Water quality model calibration
- Model output compared to observed DO, BOD,
nutrients, chl-a, TSS EC - Focus on reproducing low DO events,
stratification algal dynamics - Includes a sediment flux submodel
- Post-processor to view output (HIMS)
- Including web-based viewer
13Light Extinction(Lehman, 2005)
- Ideally light data with depth
- Determine Ke using
- I Io e -KeH
- Actuality secchi depth data
- Determine Ke using
- Ke 1.8/secchi
14Light Extinction Relationship
- Used coupled secchi, TSS chla data to develop
relationship (Di Toro, 1978) - Ke 0.052NVSS 0.174VSS 0.031Chla
- VSS 0.2TSS (based on Vernalis data)
- Ke 0.0764TSS 0.031Chla
- Model calculates Ke as a function of modeled TSS
and Chla
15Spatial Variation
- Secchi depth increases in DWC (lower chla TSS)
- Decreased Ke in DWSC vs upstream SJR
16Algal Stoichiometry
- Data from Vernalis
- Limited POC data in DWSC
- Redfield ratios
- C/N 5.7 (Data 3.1)
- C/P 41 (Data - 32)
- C/Chl Range 20-100
- Data 37, Lehman 40
- Used Redfield C/Chl40
17Other Model Inputs
- Solar radiation CIMIS Lodi West
- 100-700 ly/d, variations due to weather events
- Boundary Conditions
- Upstream based on Vernalis
- Downstream based on Jersey Potato Pt
- Internal sloughs based on river data
- Atmospheric Reaeration
- Based on wind speed formula (Banks, 1975 Banks
Herrera, 1977)
18Hourly Wind Speed and KL at RR Island Source DWR
2000
2001
19Model Settling/Deposition
- Water column settling 2.5 m/d
- Deposition to sediment variable
- DWSC 0.25-0.5 m/d (higher in TB)
- SJR 0-0.05 m/d w/ adjustments to assist in TSS
chla calibration - Settling rates set based on calibration
20Model Parameters
21Stockton RWCF Effluent
22DWSC SOD Data Model Output(Litton, 2003)
23DO Chla Calibration
Vernalis (BC)
Mossdale
24R1
R2
25R3
R4
26R5
R6
27R7
R8
28Spatial DO Chla Transects(June-October Average)
2000
2001
29Spatial Nutrient Transects
2000
2001
30DO Deficit Components (R5)
Sink
Sink
Source
Sink
Ka Source SOD - Sink
31Summary
- DWSC WQ Model calibration completed final
report issued (Task 4 May 2006) - Provides finer temporal vertical resolution
than previous modeling studies - Stratification, diurnal variation, DO components
- Can be used to assess DO aeration device impacts
(e.g., location, spreading, benefit) - Links upstream downstream water quality for
assessing management alternatives
32Recommendations
- Further testing of models to more recent DWSC
data (hydro WQ) - Different flow regimes, DO levels, etc.
- More detailed data/modeling of the Mossdale/Old
River area of the SJR - Algal growth between Vernalis Mossdale
- More information on carbon dynamics
- POC/DOC data, internal loads, DO effects
33Recommendations
- Investigate algal dynamics (2 species)
- Studies have shown different algal species
- Include more than 1 species in model with
different algal growth dynamics - May help Vernalis-Mossdale algal growth
- Use models in adaptive management approach
- Use models (as currently calibrated) to
investigate potential controls while still
collecting data completing modeling to improve
the effective use of the DWSC model as a
management tool
34Questions Answers
Contact info Andy Thuman Laurie De
Rosa HydroQual, Inc. Mahwah, NJ (201) 529-5151
x7184 athuman_at_hydroqual.com lderosa_at_hydroqual.com
35Light Extinction Comparison