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SU0004094
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SU0004094
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Last modified
10/27/2020 1:02:10 PM
Creation date
9/6/2019 10:43:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004094
FACILITY_NAME
QX-01-0002
STREET_NUMBER
36736
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36736 S KOSTER RD
RECEIVED_DATE
1/8/2002 12:00:00 AM
QC Status
Approved
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\MIGRATIONS\K\KOSTER\36736\QX-01-02_PA-0200065\SU0004094\EIR 2004.PDF
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EHD - Public
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4. ENVIRONMENTAL ANALYSIS <br /> 4.8 HYDROLOGY AND WATER QUALITY i <br /> Groundwater Extraction and Land Subsidence <br /> Significant land subsidence in the San Joaquin Valley has occurred in areas where the Corcoran <br /> Clay confines the lower aquifer. In these areas,pressure changes caused by groundwater <br /> pumping promote greater compressive stress than in the unconfined zone(DWR, 1977). The <br /> maximum land subsidence levels recorded in the Central Valley occurred in the 2,600 square- <br /> mile Los Banos-Kettleman City area. Because of the slow drainage of the fine-grained deposits, <br /> subsidence at a particular time is more closely related to past water-level change than to current <br /> change. For example,in the San Joaquin Valley,groundwater withdrawals increased greatly until <br /> large imports of surface water through various canals occurred;but even though water levels in _ <br /> the area started to rise, the rate of subsidence began to decrease three years later. The rate of <br /> ground subsidence can be reduced or arrested by a rise in the artesian head and water levels,but <br /> restoration of water levels has not caused any restoration of land surface heights (i.e., once the — <br /> physical compaction and subsidence occur, they are essentially permanent). Significant land <br /> subsidence has been detected in the San Joaquin Valley due to increased groundwater pumping <br /> associated with the drought of 1987-1992(USGS,2003). The areas of subsidence are primarily — <br /> south of the Merced River and no subsidence has been reported in the Vernalis Area(Williamson <br /> and others, 1989). <br /> Groundwater Quality <br /> On a regional scale,the water quality in the upper,unconfined aquifer is,for the most part, <br /> relatively poor and of variable quality. Water within the lower,confined aquifer is of better <br /> quality and is more commonly used as a water supply source. <br /> The agricultural pesticide dibromochloro-propane(DBCP) is a potential carcinogen found in <br /> groundwater throughout San Joaquin Valley. DBCP has been detected in 30 percent of the <br /> private and public-supply wells from 1979 through 1984 and since 1977. California has since — <br /> outlawed its use. At least 50 other pesticides, including 1,2—dichloropropane and ethylene <br /> dibromide had been detected in ground water in the Central Valley by 1984(USGS,2003). <br /> REGULATORY FRAMEWORK <br /> Water Quality Regulations <br /> The major federal legislation governing the water quality aspects of the project is the CWA as <br /> amended by the Water Quality Act of 1987. The objective of the CWA is "to restore and <br /> maintain the chemical, physical, and biological integrity of the Nation's waters"(U.S. <br /> Government Printing Office, 1988). The State of California's Porter-Cologne Water Quality _ <br /> Control Act(Division 7 of the California Water Code)provides the basis for water quality <br /> regulation within California. The State Water Resources Control Board(SWRCB)administers <br /> water rights, water pollution control, and water quality functions throughout the state, while the — <br /> RWQCB conducts planning,permitting,and enforcement activities. The project would be <br /> subject to review under provisions of the RWQCB. The project area lies within the jurisdiction <br /> of the CVRWQCB. The California Department of Fish and Game has jurisdiction over any <br /> RMC Pacific Vernalis Qaany Mining and Reclamation Project 4.8-16 ESA/203015 <br /> Adminis¢ativ Dnfl IDt March 2004 <br />
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