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ARCHIVED REPORTS_XR0002956
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0545250
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ARCHIVED REPORTS_XR0002956
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Last modified
1/30/2020 5:40:08 PM
Creation date
1/30/2020 4:30:46 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0002956
RECORD_ID
PR0545250
PE
3528
FACILITY_ID
FA0001817
FACILITY_NAME
7-ELEVEN INC #35355
STREET_NUMBER
3202
Direction
W
STREET_NAME
HAMMER
STREET_TYPE
Ln
City
Stockton
Zip
95209
CURRENT_STATUS
02
SITE_LOCATION
3202 W Hammer Ln
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
Scanner
SJGOV\sballwahn
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EHD - Public
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. ALISTO ENGINEERING GROUP <br /> 4/0 RJ\J� <br /> February 21, 1995 <br /> Mr. Scott Hooton <br /> BP Oil Company JUS <br /> Environmental Resources Management 1995 <br /> 295 S.W. 41st Street �1vVj <br /> Building 13, Suite N ��5 HyCl H - -t�4401 <br /> Renton, Washington 98055 <br /> Subject: Baildown Test Results <br /> BP Oil Company Service Station No. 11193 <br /> 3202 West Hammer Lane <br /> Stockton, California <br /> Dear Mr. Hooton: <br /> In accordance with BP Oil Company Contract Release No. G489719, Alisto Engineering <br /> Group performed baildown testing at BP Oil Company Service Station <br /> No. 11193, 3202 West Hammer Lane, Stockton, California on February 16, 1995. <br /> The testing involved extracting groundwater using a submersible pump until a portion of the <br /> available drawdown in the well was depleted. Pumping was discontinued and the <br /> drawdown of the water column in the wells was then allowed to recover to a minimum of 90 <br /> percent of the initial water column. Recovery of drawdown in the wells was recorded using <br /> pressure-sensitive transducers and a data logger. <br /> The test data were then used in an analytical computer program (Agtesoly, Geraghty and <br /> Miller, 1991) to estimate the hydraulic conductivity (K) of the shallow water-bearing zone <br /> using techniques developed by Bower-Rice (1976). The estimates of hydrogeologic properties <br /> are summarized in Table 1. <br /> The transmissivity (T) was calculated using the equation T=Kb, where b is the saturated <br /> thickness of the water-bearing zone. For purposes of this calculation, the measured water <br /> column in each well was assumed to be the saturated thickness of the water-bearing zone. <br /> The graphical analysis for each well from the baildown test is included for reference. <br /> Based on review of the boring logs, the predominant soil types of the water-bearing zone are <br /> silt and silty sand underlain by fine to medium sand, which generally have K values ranging <br /> from approximately 1 to 1 x 105 cm/s (Freeze and Cherry, 1979). The values of the aquifer <br /> parameters calculated from the baildown tests are comparable and consistent with the <br /> characteristics of subsurface soils encountered at the site. <br /> The submersible pump was only capable of drawing down 1.5 feet of groundwater in MW-1 <br /> at a maximum pumping rate of 6 gallons per iinute. The rapid recovery is consistent with. <br /> the silty sand and sand encountered in the well's water-bearing zone. <br /> 1777 OAKLAND BOULEVARD, SUITE 200 •WALNUT CREEK. CA 94596 • (510) 295=1650 • FAX (510) 295-1823 <br /> CONTRACTORS LICENSE NO. A-652544 <br />
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