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ARCHIVED REPORTS_XR0005381
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ARCHIVED REPORTS_XR0005381
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Last modified
9/24/2020 12:09:10 AM
Creation date
3/17/2020 4:23:03 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0005381
RECORD_ID
PR0545561
PE
3528
FACILITY_ID
FA0009490
FACILITY_NAME
KENTS OIL SVC INC
STREET_NUMBER
3310
Direction
E
STREET_NAME
MINER
STREET_TYPE
AVE
City
STOCKTON
Zip
95205
APN
14339005
CURRENT_STATUS
02
SITE_LOCATION
3310 E MINER AVE
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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• <br /> 1 FIELD ACTIVITIES <br /> On September 25, 1998, Kleinfelder collected groundwater samples from three monitoring wells <br /> at the site. Mr. Doug Heard of our Stockton office did the sampling. <br /> 1.2 Measurement of Groundwater Levels <br /> Upon arrival onsite, all wells were opened and allowed to equilibrate. After approximately 30 <br /> minutes, the depth to groundwater was measured in the three wells using a conductivity-based <br /> water level indicator. The water level indicator was cleaned prior to use in each well to reduce <br /> the potential for cross-contamination. Measurements were made to the surveyed mark on the <br /> north rim of the monitoring well PVC casings. Groundwater depth measurements were <br /> converted to groundwater elevations. These elevations were plotted as shown on Plate 1, <br /> Groundwater Elevation Map. Table 1 presents a summary of water level measurements. <br /> The groundwater gradient and flow direction were calculated from the groundwater elevation <br /> data and indicates the groundwater is flowing in a southerly direction with a gradient of 0.031. <br /> Previous groundwater gradients and directions were plotted graphically and presented in a Rose <br /> Diagram as shown on Plate 2. This plot shows the overall direction and magnitude of the <br /> gradient and a mean groundwater direction. <br /> i <br /> 1.3 Collection of Groundwater Samples <br /> Following obtaining groundwater depth measurements, Kleinfelder collected samples from the <br /> three wells at the site. During the purging, field parameters such as temperature, pH, and <br /> conductivity were monitored. Copies of the Purge Characterization and Sample Log Sheets are <br /> presented in Appendix A. Groundwater samples were collected from these wells, and the <br /> sampling protocol for each monitoring well was as follows: <br /> + The volume of water in gallons standing in the well was calculated by subtracting the <br /> depth-to-groundwater measurement from the known depth to the well bottom and <br /> multiplying by the cross-sectional inside area of the well casing. <br /> • A transparent single-use disposable bailer was lowered approximately half-way into the <br /> surface of the water standing in the well and then withdrawn to check for a petroleum <br /> layer or sheen on the water. <br /> • A minimum of three well volumes of water was then purged from each well using a <br /> submersible pump. The pump was decontaminated between each well and new tubing <br /> was used for each well. <br /> Samples were collected after purging by decanting samples from the disposable <br /> disposable bailer directly into bottles provided by the analytical laboratory. <br /> s <br /> 40-327301/4018RO51 3 <br /> Copyright 1998 Kleinfelder,Inc. <br /> KLEINEELDER 790 Chadbourne Road, Suite D. Fairfield CA 94,585-964 3 (707)429-4{70 (707) 429-4162 fax <br />
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