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ARCHIVED REPORTS_XR0004257
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PR0541913
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ARCHIVED REPORTS_XR0004257
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Last modified
2/13/2020 5:16:54 PM
Creation date
2/13/2020 1:22:50 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004257
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 /> Frontier Transportation <br /> 0399-085 <br /> April S, 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 Holocene <br /> age which overlay sedimentary rocks of Cretaceous to Tertiary age. These sedimentary units, in <br /> turn, overlay a crystalline basement of Paleozoic and Mesozoic metamorphic and igneous rocks. <br /> The shallow subsurface geology in the site vicinity is a heterogeneous mix of gravel, sand, silt, and <br /> clay (Reference, Site Characterization Report, Twining Laboratories, October 16, 1996). BEII <br /> encountered clay and a heterogeneous mix of clay from 0' to 25' bg in January of 1998. Two <br /> cross sectional depictions of the site are provided 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. BEII encountered shallow <br /> subsurface water between 6' and 10' bg. Data collected in December of 1998 identified the flow <br /> of groundwater in a generally western direction beneath the site (See Figure 5, Groundwater <br /> Gradient Map), <br /> 4.0) QUARTERLY GROUNDWATER SAMPLE RESULTS <br /> On February 23, 1999, BEII collected groundwater samples from MW-1 through MW-7 <br /> for laboratory analysis. Groundwater parameters (pH, temperature, and conductivity) were <br /> measured before, during, and after well purging (See Appendix A for Groundwater Parameters). <br /> Groundwater samples were analyzed for TPH-d, TPH-g, BTEX, and MTBE using EPA methods <br /> 8015 modified for diesel, 8015 modified for gasoline, 8020, and 8260, respectively. Laboratory <br />' analysis results for all monitoring episodes are presented in Table 1 and Table 2. Recent analytical <br /> reports are included as Appendix B. <br /> Groundwater collected from MW-1, MW-2, MW-4, MW-5, MW-6, and MW-7 identified <br /> no detectable (<500 ,ug/L) dissolved TPH-d concentrations using EPA method 8015. In <br /> monitoring well MW-3, groundwater analysis identified an increase in TPH-d concentrations from <br /> 1,300µg/L in December 1998 to 3,600µg/L in February 1999. However, TPH-d concentrations <br /> identified in MW-3 were not representative of true dissolved diesel concentrations. Laboratory <br /> analysis results reported the TPH-d concentration as a diesel and motor oil mixture in December <br />' 1998 and as a gasoline and diesel mixture in February 1999, but not as diesel exclusively. <br /> • 2 <br />
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