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ARCHIVED REPORTS_1988_4
Environmental Health - Public
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ARCHIVED REPORTS_1988_4
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Last modified
7/17/2020 3:52:56 PM
Creation date
7/3/2020 11:04:10 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1988_4
RECORD_ID
PR0440003
PE
4434
FACILITY_ID
FA0003698
FACILITY_NAME
CORRAL HOLLOW LANDFILL
STREET_NUMBER
31130
STREET_NAME
CORRAL HOLLOW
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
25303010
CURRENT_STATUS
01
SITE_LOCATION
31130 CORRAL HOLLOW RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\SW\SW_4434_PR0440003_31130 CORRAL HOLLOW_1988_4.tif
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EHD - Public
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0 <br />0 <br />J. H. KLEINFELDER & ASSOCIATES <br />File: W-2022-1/11:312 <br />June 19, 1986 <br />Page 4 <br />Ground Water <br />It is our opinion that wells may be developed on the site <br />which would supply ground water of sufficient quantity, the <br />desired production of 3,500 gallons per minute. Deep wells <br />drilled along the northeast border of the site would have the <br />best potential for providing the desired supply. This <br />conclusion is based on data obtained from the Department of <br />Water Resources; Water and Power Resources Service, San <br />Joaquin County; landowners and developers in the site area; <br />and laboratory tests performed on water samples obtained in <br />the area. <br />In order to produce sufficient quantities of water, wells <br />would most likely penetrate the Plio-Pleistocene Corcoron <br />clay layer, which generally separates more saline water above <br />from less saline water below. Well depths on the order of <br />600 to 900 feet should be anticipated. <br />It is doubtful that a dependable ground -water supply can be <br />obtained from wells drilled in the western hills of the site. <br />These hills are located in the rainshadow of the Coast Ranges <br />and receive approximately 10 inches or less of rain annually. <br />In addition, the rock formations of the eastern Coast Ranges <br />are considered non-waterbearing. Rainwater drains off the <br />hills in the form of surface runoff and small springs, into <br />q <br />the basins and ultimately into the valley auifers. It is <br />probable that small quantities of water are trapped within <br />the Corral Hollow drainage, however, there would not be <br />sufficient quantities or recharge to supply the proposed <br />community for the long term. <br />It appears that the quantity and quality of available ground <br />water on and around the northeast portion of the site varies <br />greatly. The major sources of recharge for the aquifers <br />along the northeast side of the site are from deep ground <br />water inflow from the south and southeast. Minor amounts are <br />contributed from surface runoff of the Coast Ranges. <br />We understand that during well development for Lone Star <br />Industries, Granite Construction and Country Estates <br />Subdivision dry wells were drilled before encountering <br />sufficient quantities. Lone Star Industries and Granite <br />Construction are located approximately 3\4 to one mile north <br />of the site and Country Estates Subdivision is located on the <br />east end of the site. A landowner to the west of the site <br />informed us that he had attempted several 500 to 600 -foot <br />deep wells with no significant ground water encountered. In <br />our opinion, the relatively shallow depth of these wells is <br />probably the main reason for their failure. <br />
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