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SITE INFORMATION AND CORRESPONDENCE
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Last modified
4/3/2020 2:10:20 PM
Creation date
4/3/2020 1:50:02 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE INFORMATION AND CORRESPONDENCE
RECORD_ID
PR0524190
PE
2965
FACILITY_ID
FA0016241
FACILITY_NAME
STOCKTON REGIONAL WATER CONTROL FAC
STREET_NUMBER
2500
STREET_NAME
NAVY
STREET_TYPE
DR
City
STOCKTON
Zip
95206
APN
16333003
CURRENT_STATUS
01
SITE_LOCATION
2500 NAVY DR
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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Attachment A - 3- <br /> Comments <br /> 3- <br /> Comments on Evaluation of San Joaquin River Flows at Stockton <br /> April 2001 <br /> 5. As mentioned in item 1, the Report uses Equation [1], above, to estimate the StocktonNemalis <br /> ratio during the winter months. The equation contains the constant, C, which was derived using <br /> data from 1996 through 2000, which were above average wet years. Slight changes in the constant <br /> create substantial changes in the estimated Stockton flow. The only information in the Report to <br /> support the estimation of C, is a statement on page 18, `The accuracy of the predicted Stockton <br /> flows using the value C = 0.05 is not known for certain. However, this scenario predicts Stockton <br /> flows that correspond with the historical fractions of RWCF effluent concentrations in the San <br /> Joaquin River during January 1988." One month of data was used to substantiate the coefficient. <br /> It is not clear how much receiving water data was available or where in the river the samples were <br /> taken. <br /> 6. As mentioned above, the Report uses receiving water ammonia concentrations to substantiate the <br /> selection of the constant, C. Based on the receiving water ammonia concentration, effluent flow, <br /> and effluent ammonia concentration, an expected monthly Stockton SJR flow is calculated. The <br /> Report discounts higher C values (lower Stockton SJR flows) because the values predict extended <br /> periods of zero flow. For some reason, the bottom limit of flow is set to zero (see figures 14, 15, <br /> 16, and 17). The Report does not consider the possibility of daily net flow reversals (negative <br /> flow),which may be caused by low SJR flow and high export pumping and which have been <br /> presumed to occur in other flow models. In addition, it is not clear where or how often the <br /> ammonia samples were collected. <br /> 7. In the estimates of 1991 and 1992 Stockton flow (page 27), the Report states there were a few <br /> instances where ammonia concentrations in the San Joaquin River reached 60%to 100% (meaning <br /> very little to no dilution). The Report discounts this by stating, "...these instances were rare." It is <br /> not clear when, where, or how often the samples were collected, or how often the high <br /> concentrations occurred. This time period is important, because critical flow was measured at <br /> Vernalis during this time. The Report suggests the possibility that there are periods of limited or <br /> no dilution every year. <br /> 8. The Report does not provide information that would change the Regional Board's estimation of <br /> critical flows for the RWCF discharge. The Report asks to make considerations for future flows <br /> by stating that new tidal gates will be installed for each of the four barrier locations as part of the <br /> South Delta Improvement Program. The Report claims the tidal gates will be operational within <br /> the next 7 years, but does not provide any information about the implementing agency or the <br /> funding source. The flows in the SJR will be continually changing; and some may or may not ever <br /> come about. Use of real flow data with conservative assumptions for critical receiving water <br /> conditions remains the most accurate and reasonable approach to evaluate dilution. <br />
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