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ARCHIVED REPORTS XR0001828
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3500 - Local Oversight Program
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PR0544430
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ARCHIVED REPORTS XR0001828
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Last modified
5/7/2019 2:28:30 PM
Creation date
5/7/2019 2:16:43 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001828
RECORD_ID
PR0544430
PE
3526
FACILITY_ID
FA0005370
FACILITY_NAME
PARMAR TEXACO
STREET_NUMBER
521
Direction
N
STREET_NAME
CHEROKEE
STREET_TYPE
LN
City
LODI
Zip
95240
CURRENT_STATUS
02
SITE_LOCATION
521 N CHEROKEE LN
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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' 3.0 INVESTIGATIVE RESULTS <br /> 3.1 Groundwater Monitoring Results <br /> The s <br /> hallowest groundwater in this portion of the city of Lodi is reported to occur under unconfined <br />' conditions (Environmental Forensic Investigations, 2002) On September 30, 2004, the highest point <br /> measured from the monitoring wells was 6 66 feet (msl)and occurred m monitoring well PT-MW4 The <br /> lowest elevation of the groundwater surface measured from the monitoring wells was 6 17 feet (msl)and <br /> occurred in monitoring well PT-MW6 A summary hydrograph for monitoring well PT-MWI is <br /> presented as Figure 5 <br /> The average depth to groundwater surface in the six monitoring wells was approximately 46 5 feet below <br /> Iground surface(bgs) The groundwater surface has fallen about 0 5 foot since the last monitoring event <br /> (September, 2004) <br />' Electrical conductivity concentrations in the monitoring well water samples were determined to range from <br /> 152 to 265 µmhos/cm This low-conductivity value is typical of reported electrical conductivity values of <br /> local groundwaters found near the Mokelumne River(Figure 2) Concentrations of electrical conductivity <br /> in waters from the Mokelumne River are reported to range from 200 to 350 µmhos/cm because the relative <br /> short distance from the watershed source in the Sierra Nevada and Quaternary alluvial terrain the waters <br /> traverse(Page, 1986) <br /> Temperature and pH concentrations in the monitoring well waters is typical of 1'groundwater encountered <br /> in the Lodi area(Environmental Forensics Inc, 2002) <br /> lie <br /> 3^2 Groundwater AnabAi al Results <br /> No groundwater analytical results are available for this quarterly monitoring period <br /> 3.3 Local Groundwater Flow Direction and Gradient <br /> The groundwater surface undulates slightly but has a gentle slope toward S50W with a gradient of 0 001 <br /> (Figure 4) This flow direction and gradient are consistent with published groundwater data from the City <br /> of Lodi(Environmental Forensic Investigations, Inc , 2002)and San Joaquin County Department of Public <br /> Works(2004) groundwater surface elevations for the North San Joaquin Water Conservation District <br /> 3_4 Petroleum Hydrocarbon Groundwater Plume <br /> No information is available for the petroleum hydrocarbon groundwater plume for this monitoring event <br /> 4.0 PLANNED FUTURE WORK <br /> The next planned operation for this site will include additional Quarterly Status Report(QSR) and <br /> quarterly monitoring report(QMR)for the period ending December 31, 2004 A sensitive receptor survey <br /> of the nearby water supply wells will be completed during the I'quarter of 2005 <br /> MainlDWnvironmeniallParmarTexacoWepons1093004QMR wo 4 <br />
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