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ARCHIVED REPORTS_XR0007996
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ARCHIVED REPORTS_XR0007996
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Last modified
4/14/2020 2:50:03 PM
Creation date
4/14/2020 1:05:01 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0007996
RECORD_ID
PR0541401
PE
2950
FACILITY_ID
FA0006046
FACILITY_NAME
UNION OIL STATION #5098
STREET_NUMBER
5606
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
CURRENT_STATUS
02
SITE_LOCATION
5606 PACIFIC AVE
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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Updated Site Conceptual Model and Third Quarter 2002 Monitoring and Remediation Report <br /> Cleanu and Abatement Order No 5-00-707 EAI Pro ect No 1232 <br /> 5.0 DISCUSSION <br /> 5.1 Ground Water Elevation Contour Maps <br /> Ground water beneath the sites has been segregated into shallow and deep zones hereinafter <br /> referred to Hydro-Stratigraphic Units A, and B respectively, or simply Unit A and Unit B Two <br /> deeper units, Unit C and Unit D, are also associated with the sites (see Section 2 0) The wells <br /> that are located on the former Wards site are generally screened in Unit B with the exception of <br /> well MW-81) which is screened in Unit D Figures 8 and 9 present ground water elevation <br /> contour maps for Hydra-Stratigraphic Units A and B Unit A wells extend across the water <br /> table and generally are screened from 30 to 50 feet bgs Unit B wells are generally screened <br /> between 50 and 70 feet bgs <br /> Five additional wells are screened across Hydro-Stratigraphic units deeper than Units A and B <br /> as follows Two wells are screened in Unit C (MW-23S and MW-24S) and three wells (MW- <br /> 8D, MW-23D and MW-24D) are screened in Unit D (see Section 2 0) It is EAI's opinion that <br /> Units C and D are hydraulically connected and represent the same unit <br /> 5.2 Ground Water Flow Direction and Magnitude <br /> Since the RTW was taken out of operation in August 2000, ground water flow direction in <br /> Hydro-Stratlgraphlc Units A and B has consistently been toward the east The current gradient <br /> as measured from Unit B is approximately 0 003 foot/foot <br /> 5.3 Monitoring Well Hydrographs <br /> Figures 4 through 7 present TPH-G and benzene concentration plus ground water elevation <br /> verses time for ground water monitoring wells MW-2, MW-3, MW-11 and MW-12, <br /> respectively A general decline in TPH-G and benzene concentrations has been observed since <br /> ground water monitoring was initiated One exception is TPH-G in well MW-1 i which has <br /> shown an increase during the last two quarters Ground water elevation over the same period <br /> of time has risen approximately 20 feet on average <br /> 5.4 TPH-G and Benzene Isoconcentrahon Maps <br /> Figures 10 and 11 present TPH-G isoconcentration maps for Units A and B Figure 10 <br /> indicates that three Unit A wells had a detectable TPH-G concentration above the laboratory <br /> detection limit of X50 pg/L (MW-14A, 910 pg/L, MW-19S, 280 pg/L, and MW-25S, 340 <br /> µg/L) Iii Uillt B, the hzghesi c,omentrdtion of TPH-G was in well MW-11 (49,000 }ig/L) <br /> Figures 12 and 13 present Unit A and Unit B benzene isoconcentration maps, respectively <br /> Benzene was detected in Unit A in four wells during the September 2002 sampling event (MW- <br /> 10A, 078 pg/L, MW-14A, 33 pg/L, MW-19S, 054 pg/L, and MW-25S, 45 pg/L) The <br /> highest Unit B benzene concentration was in monitoring well MW-11 at 10,000 pg/L (see <br /> Figure 13) <br /> BHM WORD 1231RO211 -8- ENVIRONMENTAL AUDIT,INC p <br />
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