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ARCHIVED REPORTS_XR0004256
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0541913
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ARCHIVED REPORTS_XR0004256
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Last modified
2/13/2020 5:26:28 PM
Creation date
2/13/2020 1:21:32 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004256
RECORD_ID
PR0541913
PE
2960
FACILITY_ID
FA0024043
FACILITY_NAME
FRONTIER TRANSPORTATION FACILITY
STREET_NUMBER
425
STREET_NAME
LARCH
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
21220009
CURRENT_STATUS
01
SITE_LOCATION
425 LARCH RD
P_LOCATION
03
QC Status
Approved
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EHD - Public
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Quarterly Groundwater Monitoring Report <br /> i Frontier Transportation <br /> 0899-139 <br /> August 13, 1999 <br /> Site Layout Map). Soil samples were collected every five feet. Laboratory analysis of soil <br /> samples identified no detectable concentrations of TPH-g, BTEX, or MTBE. Groundwater <br /> samples were subsequently collected. Results are tabulated in Table 1. <br /> 3.0) SITE GEOLOGY/HYDROGEOLOGY <br /> The site is located on the boundary of the Sacramento Valley and the San Joaquin Valley <br /> within the west-central portion of the Great Valley Geomorphic province of California. The <br /> Great Valley has been filled with a sequence of older to younger alluvium of Pliocene to <br /> Holocene age which overlay sedimentary rocks of Cretaceous to Tertiary age. These <br /> sedimentary units, in turn, overlay a crystalline basement of Paleozoic and Mesozoic <br /> metamorphic and igneous rocks. The shallow subsurface geology in the site vicinity is a <br /> Iheterogeneous mix of gravel, sand, silt, and clay (Reference; Site Characterization Report, <br /> Twining Laboratories, October 16, 1996). BEII encountered clay and a heterogeneous mix of <br /> clay from 0'to 25' bg in January of 1998. Two cross sectional depictions of the site are provided <br /> as Figure 3 and Figure 4. <br /> First subsurface water was encountered at depths from 11'to 12' bg during tank removal <br /> and monitoring well installation at this site in 1995 and 1996. Since then, shallow subsurface <br /> water has been encountered between G and 10'bg. Data collected in July of 1999identified the <br /> 1 flow of groundwater in a generally western direction beneath the site (See Figure 5, Groundwater <br /> Gradient Map). Previous groundwater gradients were identified in the southwest direction <br /> indicating a modulating gradient beneath the site. <br /> 4,0) QUARTERLY GROUNDWATER SAMPLE RESULTS <br /> On July 13, 1999, BEII contracted Del-Tech to collect groundwater samples from <br /> monitoring wells MW-1 through MW-7 for laboratory analysis. Groundwater parameters(pH, <br /> temperature, and conductivity)were measured before, during, and after well purging(See <br /> Appendix A for Groundwater Parameters). Groundwater samples were analyzed for TPH-d, <br /> TPH-g, TPH-m (total petroleum hydrocarbons as motor oil), BTEX, and MTBE using EPA <br /> methods 8015 modified for diesel, 8015 modified for gasoline, 8015 modified for motor oil, <br /> 8020, and 8260, respectively. Laboratory analysis results for all monitoring episodes are <br /> presented in Table 1. Recent analytical reports are included as Appendix B. <br /> Groundwater collected from all monitoring wells identified low level dissolved TPH-d <br /> and TPH-m concentrations(:5260 µg/L) using EPA method 8015. In addition, laboratory <br /> analytical results identified no detectable dissolved concentrations of TPH-g above 50 pg/L from <br /> groundwater samples collected from MW-2, MW4, MW-5, MW-6, and MW-7 using EPA <br /> • 2 <br />
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