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ARCHIVED REPORTS XR0006812
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544639
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ARCHIVED REPORTS XR0006812
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Last modified
7/9/2019 4:30:15 PM
Creation date
7/9/2019 3:24:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006812
RECORD_ID
PR0544639
PE
3528
FACILITY_ID
FA0005076
FACILITY_NAME
DICKS EXXON
STREET_NUMBER
2360
STREET_NAME
EAST
STREET_TYPE
ST
City
TRACY
Zip
95376
APN
23346001
CURRENT_STATUS
02
SITE_LOCATION
2360 EAST ST
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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F <br /> Perimeter and downgradient of the former gasoline/diesel tank pit (TP1) Soil contamination in <br /> these areas extends vertically to the shallow water table. Vertical migration of contaminants <br /> ' appears to have been fairly rapid with little lateral spreading (Figure 5). <br /> 6.2 Groundwater Impact <br /> The lateral extent of groundwater contamination has been defined in most sectors of the site. <br /> Analysis of groundwater samples collected from the monitoring wells, and soil samples collected <br /> from the capillary fringe in the borings and wells, has provided constraints on the limits of <br /> ' contamination in the following areas: the product lune area; the waste oil pit area; and the <br /> western, southern and eastern sides of the gasoline/diesel tank pit (TPl) These appear to <br /> ' comprise three discrete areas of groundwater contamination (Figure 5) The downgradient limit <br /> of affected groundwater emanating from the tank pit has not been defined. <br /> The validity of utilizing soil samples collected from the capillary fringe as indicators of <br /> underlying groundwater contamination is supported by the analytical results of samples collected <br /> from the monitoring wells Soil samples collected from monitoring wells MWl and MW2 were <br /> found to be significantly impacted, as was groundwater. The soil sample collected from MW3 <br /> contained no detectable contaminants and the groundwater in this well was clean. The lateral <br />' distance of the wells from the source of the leaks (especially MW 1) confirm that the soil <br /> contamination detected therein is truly due to capillary phenomena and not simply a result of <br />' previous vertical transport. The reasonable inference from the data is that, at this site, capillary <br /> fringe soils serve as reliable indicators of groundwater impact <br /> The lack of appreciable downgradient migration of contaminated groundwater may be due to the <br />' recent vintage of the leak combined with the low velocity silt/clay aquifer. <br /> R-012792 LF 7 <br />
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