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2900 - Site Mitigation Program
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Last modified
5/17/2019 9:45:35 AM
Creation date
5/16/2019 2:23:25 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0505363
PE
2960
FACILITY_ID
FA0005584
FACILITY_NAME
VALLEY PACIFIC LODI PLANT & CARDLOCK
STREET_NUMBER
930
Direction
E
STREET_NAME
VICTOR
STREET_TYPE
RD
City
LODI
Zip
95240
APN
04905023
CURRENT_STATUS
01
SITE_LOCATION
930 E VICTOR RD
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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AMeuangkhoth
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EHD - Public
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Roberts Oil Company May 23, 1988 <br />Project No. 1628G Page 3 <br />and benzene, toluene, and total xylenes (BTX) following the appropriate EPA <br />methods. All samples were placed in a refrigerated chest and were transported <br />under chain -of -custody documentation to a state -certified laboratory for <br />chemical analysis. <br />4.0 ANALYTICAL RESULTS <br />All three ground -water samples (MW -2, MW -3, MW -4), were analyzed for TVH, <br />BTX, and TEH. Results of the analyses revealed no detectable concentrations of <br />TVH or BTX in any of the samples. Ground -water sample results from wells <br />MW -2 and MW -3 revealed no detectable concentrations of TEH; however, the <br />results for the well MW -4 sample revealed a TEH concentration of 240 parts <br />per billion (ppb). The results of the laboratory analyses are presented in <br />Table 1. <br />5.0 DISCUSSION <br />The ground -water surface as measured on March 31, 1988 is presented in <br />Figure 2. The ground -water flow direction as shown is toward the southwest <br />at an average calculated gradient of 0.0005 feet per foot. This flow direction <br />is approximately 90 degrees different from the April, 1987 southeast direction <br />reported by J.H. Kleinfelder and Associates (Kleinfelder, 1987). The most <br />recent data indicates that the local ground -water surface has apparently <br />changed over time. Due to the very low inclination of the ground -water <br />surface, minor variations in water levels can drastically alter the apparent <br />flow direction. Because the local ground -water surface is nearly flat the <br />contamination migration is therefore surmised to be slow. These conditions <br />make it difficult to determine the prevailing local ground -water flow <br />direction. <br />While no state action levels currently exist for TVH and TEH, the TEH value <br />observed in well MW -4 and the free -product in well MW -1 indicate that the <br />ground -water on site has been impacted. <br />
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