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Last modified
1/17/2020 5:31:32 PM
Creation date
1/17/2020 3:54:48 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0505611
PE
2951
FACILITY_ID
FA0006807
FACILITY_NAME
MORESCO PROPERTY
STREET_NUMBER
16865
STREET_NAME
GAWNE
STREET_TYPE
RD
City
STOCKTON
Zip
95205
APN
18309009
CURRENT_STATUS
01
SITE_LOCATION
16865 GAWNE RD
P_LOCATION
99
QC Status
Approved
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EHD - Public
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-, 10, CJeafngicaf?echnics Inc. Page 5 <br /> Soil Groundwater Investigation Report <br /> Moresco <br /> Project No.251.3 <br /> i„ .Tune 7, 1999 <br /> 3.1 Analytical Results <br /> 3.1.1 Soil Sample Analysis <br /> The following is a summary of the soil analytical results. The data is included in Table 1 of <br /> Appendix A and the laboratory data sheets are included in Appendix C. <br /> 1. MW-1 <br /> • The 15.5 foot sample showed the presence of very low levels of MTBE (11 ug/Kg). <br /> • The 60.5 foot sample showed the presence of low levels of MTBE and TBA (110 <br /> ug/Kg and 15 ug/Kg, respectively). <br /> • The 25.5, 45.5, 75.5, 90.5 and 110.5 foot samples were non-detect for all analytes. <br /> �• 3.1.2 Groundwater Sample Analysis <br /> After development of the monitoring well on April 5, 1999, a groundwater monitoring was <br /> conducted on April 8, 1999 and May 19, 1999. The water samples were submitted to Kiff <br /> Analytical LLC for analysis for BTEX, the gasoline fuel oxygenate compounds (MTBE, <br /> DIPE, ETRE, TAME, and TBA) and TPH-G. The results of the groundwater analysis are <br /> included in as Table 2 in Appendix A. The analytical data reports are included in Appendix <br /> C. <br /> The groundwater sample from MW-1 did not show the presence of any of the compounds <br /> tested for. <br /> LW <br /> 3.2 Site Hydrology <br /> On April 8, 1999, the depth to water was 89.70 feet bgs. On May 19, 1999, the depth to <br /> `r water was 93.72 feet bgs. The groundwater appears to show a rapid decrease in elevation at <br /> the site. This is possibly due to groundwater pumping for irrigation purposes of the <br /> surrounding farms. <br /> It is not possible to calculate a site specific groundwater gradient as there is only one <br /> monitoring well at the site. <br /> 3.3 Geology and Field Observations <br /> The following section discusses the subjective field observations and geology documented <br /> during this investigation based on the interpretations of the field geologist. <br /> The site's geology is typical for shallow valley sediments consisting of sand with varying <br /> .� amounts of silt and clay. The following specific observation were made: <br /> • At least four distinct sediment types have identified between the surface and 100 ft: <br /> - clean sand <br /> - sand with fines <br /> clayey silt/silty clay <br /> - sandy gravel <br /> • A thin gravel layer was encountered between 60 and 65 feet bgs. <br /> • From 90 feet to 110 feet in MW-1 the soil was very fine-grained materials, silts, clays and <br /> silty sands. <br /> i.• Field observations indicate that the soils below the tank pit have been effectively remediated <br /> by the vapor extraction system. Only the 10 and 15 foot samples showed field evidence (i.e., <br /> L <br />
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