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SITE INFORMATION AND CORRESPONDENCE
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3500 - Local Oversight Program
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PR0544799
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SITE INFORMATION AND CORRESPONDENCE
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Last modified
11/19/2024 10:19:51 AM
Creation date
9/3/2019 3:24:19 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
SITE INFORMATION AND CORRESPONDENCE
RECORD_ID
PR0544799
PE
3528
FACILITY_ID
FA0003872
FACILITY_NAME
DISCOVERY CHEVROLET
STREET_NUMBER
1615
Direction
W
STREET_NAME
ELEVENTH
STREET_TYPE
ST
City
TRACY
Zip
95376
APN
23227019
CURRENT_STATUS
02
SITE_LOCATION
1615 W ELEVENTH ST
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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Former Discovery Chevrolet June 17, 1998 <br /> Tracy,California SWRCB Closure Anneal Letter <br /> In September 1994, GeoStrategies installed three groundwater monitoring wells (MW-1, MW- <br /> 2 and MW-3) at the site, and in April 1997, Horizon installed two downgradient groundwater <br /> monitoring wells (MW-4 and MW-5) to evaluate for the presence of hydrocarbons in the soil <br /> and groundwater beneath the site. Groundwater samples from wells MW-1 and MW-2 have <br /> been found to contain concentrations of TPHg up to 17,000 parts per billion(ppb), and benzene <br /> up to 3,100 ppb; however, the recent trend has shown a significant decrease in these <br /> concentrations. Groundwater samples from well MW-3 have been found to contain no <br /> detectable concentrations of TPHg, BTEX, MTBE or TOG, and concentrations of TPHd up to <br /> 200 ppb. Groundwater samples from downgradient wells MW-4 and MW-5 have been found <br /> to contain no detectable concentrations of TPHg and BTEX since the initial well sampling. <br /> Confirmation testing by EPA Method 8260 have indicated that MTBE detected in groundwater <br /> by EPA Method 8020 were false positive results. <br /> In 1997, groundwater samples collected and analyzed from wells MW-I and MW-2, located <br /> within the dissolved hydrocarbon plume, indicated lower concentrations of nitrate, sulfate, and <br /> ferric iron than the concentrations detected in perimeter wells MW-3, MW-4 and MW-5. The <br /> bioparameters indicated that intrinsic bioremediation is a viable and active method of natural <br /> remediation occurring beneath the site. The overall historical trend has been a reduction in <br /> hydrocarbon concentrations in the groundwater beneath the site. <br /> Additional sampling and delineation work was performed in April 1997 and February 1998. In <br /> April 1997, hand borings SA through SK were drilled around and in the former UST <br /> excavation to a depth of approximately 8 feet bsg. Selected soil samples collected from the <br /> hand borings were analyzed for TPHg and BTEX. The highest concentrations of TPHg and <br /> BTEX in soil were reported in the vicinity of the former product lines adjacent to the southwest <br /> corner of the former UST excavation. In February 1998, soil borings GP-1 through GP-10 <br /> were advanced and sampled using a truck-mounted Geoprobe® direct push rig. At the request <br /> of the SJC PHS/EHD, 26 soil samples and 10 water collected from the soil borings were <br /> analyzed for TPHg, BTEX, MTBE, and fuel oxygenates. Again, the highest concentrations in <br /> soil were reported in the vicinity of the former product lines adjacent to the southwest comer of <br /> the former UST excavation. The highest concentrations of TPHg, BTEX, and MTBE in <br /> groundwater were reported in the vicinity of the former product lines adjacent to the southwest <br /> corner of the former UST excavation, and along the west side of the excavation area. Based on <br /> the soil and groundwater sample analytical results, the TPHg- and benzene-impacted soil and <br /> groundwater have been defined vertically to a depth of 15 feet and laterally beneath the site. <br /> Based on mass balance calculations, the amount of gasoline hydrocarbons in the subsurface <br /> soil and water were estimated to be approximately 40 gallons. Historical laboratory analytical <br /> +� soil and groundwater results are included in Appendices #2 and #3 included with this letter. <br /> The shallow groundwater being monitored beneath the site is within the uppermost water- <br /> bearing or water table zone, is generally present between approximately 9 to 11 feet bgs, and <br /> generally has a flow direction toward the north-northwest beneath the site. Reported <br /> subsurface materials encountered during drilling at the site consisted primarily of fine-grained <br /> soils such as silty to sandy clay, clayey silt, and clayey sand. Because of the generally fine- <br /> grained nature of the shallow water-bearing materials and poor historical land-use practices, <br /> 0617jmun.wrb 2 HORIZON ENVIRONMENTAL INC. <br />
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