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PR0524190
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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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REGIONAL BOARD RESPONSE (SWRCB/OCC FILE A-1483) -4- <br /> PETITION FOR REVIEW OF WASTE DISCHARGE REQUIREMENTS <br /> ORDER NOS. R5-2002-0083 AND R5-2002-0084 <br /> CITY OF STOCKTON REGIONAL WASTEWATER CONTROL FACILITY <br /> Regional Board in Cease and Desist Order No. R5-2002-0084, as suggested by the State Board in Order <br /> WQ 96-09. Stockton has filed a petition for review of these Orders, and the State Board again must <br /> determine if the permit limitations and Cease and Desist Order are appropriate. <br /> FIRST BASIS: DENIAL OF DILUTION CREDIT/DENIAL OF MIXING ZONE <br /> Stockton requests that the State Board direct the Regional Board to allow dilution credits and <br /> mixing zones and rescind Cease and Desist Order No. R5-2002-0084. <br /> Dilution is a key issue. Without dilution credits, Stockton must meet stringent effluent limitations to <br /> protect the beneficial uses of the SJR. Despite more than a decade of study, there is no agreementon <br /> how to determine the dilution available for Stockton's discharge. The SJR system is complex. Channels <br /> have been rebuilt. Natural flows are stored and diverted. Pumping in the South Delta by the Central <br /> Valley Project and State Water Project actually can make the net river flow go backwards. Tides flow in <br /> and out, often reversing the direction of the river four times daily so wastes are dumped into the same <br /> parcel of water as it moves back and forth, sometimes for days and weeks at a time. <br /> Dilution may exist for many pollutants much of the time. However, pollutants combine together in <br /> complex ways to increase environmental impact over the impact found for single pollutants. The <br /> assimilative capacity of the lower SJR is already diminished due to the stress of low oxygen,high <br /> temperature, and pollutants from other sources. Based on a thorough review of actual receiving water <br /> flow data, there are critical times when net flows are minimal resulting in little or no dilution. The <br /> available flow data are from wet years, so the flows and resulting dilution would be less during critically <br /> dry years, for which the NPDES permit must provide protection. For these reasons, the Regional Board <br /> determined that no dilution credit be granted for almost all constituents. <br /> The City's petition contains substantial information regarding their evaluation of dilution, including <br /> water quality models. The Regional Board considered this information and concluded that actual flow <br /> data,with reasonable assumptions for critical dry rainfall years, should be used in determining dilution <br /> rather than the water quality models prepared by the City. This Response contains a summary of the <br /> technical bases for the Regional Board's conclusions, and the administrative record, including the <br /> permit, fact sheet, and response to comments contain much more detail explaining the Regional Board's <br /> conclusions. <br /> The 1994 Permit allowed a long-term average dilution credit of 4:1 based on model predictions, since <br /> site-specific river flow data were not available at the time. In August 1995, the US Geological Survey <br /> (USGS) installed a flow monitoring station near Stockton's outfall and began collecting flow data. <br /> Since installation of the flow monitoring station, a critically dry rainfall year has not occurred. In fact, <br /> the years of record were above average wet years for the San Joaquin Basin. Extensive flow data are <br /> available from a USGS flow monitoring station upstream at Vernalis. That flow data is helpful, <br /> however, because a large fraction of the SJR flow measured at Vernalis is diverted into Old River and <br /> other Delta channels, the SJR flow at Stockton is much less than at Vemalis. Table 1 shows the actual <br /> lowest flow measurements at Stockton during specific averaging periods, as well as the corresponding <br /> flow at Vernalis. <br />
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