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ARCHIVED REPORTS_XR0004414
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PR0539293
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ARCHIVED REPORTS_XR0004414
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Last modified
11/20/2019 3:31:01 PM
Creation date
11/20/2019 3:23:44 PM
Metadata
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EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004414
RECORD_ID
PR0539293
PE
2957
FACILITY_ID
FA0022465
FACILITY_NAME
VALLEY MOTORS
STREET_NUMBER
800
Direction
E
STREET_NAME
MAIN
City
STOCKTON
Zip
95202
CURRENT_STATUS
01
SITE_LOCATION
800 E MAIN
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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u <br /> 7.0 CONCLUSIONS AND RECOMMENDATIONS <br /> Synthesizing all of the data that have been gathered in the past four years of investigation, several <br /> conclusions can now be drawn These are listed below <br /> • Petroleum hydrocarbon concentrations in the soil beneath this site are very low Gasoline <br /> oxygenates (MTBE, etc) are either below detection limits or present at very low <br /> concentrations in all of the samples that have been collected, and total hydrocarbons have <br /> only been detected above 100 ppm in two samples, both from VM-1 Volatile aromataic <br /> hydrocarbons (BTEX), because of their mobility in groundwater, have spread somewhat <br /> farther than TPH and have been detected in several borings, but usually at concentrations less <br /> than 1 ppm Neither diesel nor ox to are important contaminants at this site We <br /> �in <br /> mmend that the sampling protocol a amended to eliminate analysis for these compounds <br /> ny uture samples <br /> • The stratigraphy beneath the site is complicated by the lenticularity of several sandy channel <br /> deposits that channel into and grade laterally into overbank silt beds These variations affect <br /> the direction of groundwater flow as well as the direction of migration of hydrocarbons due <br /> to differences in permeability <br /> • In general, the hydraulic conductivity of the near-surface strata is fair No high-permeability <br /> beds have been encountered, but some of the sand beds have conductivities in the range of <br /> 104 cm/sec Thus, groundwater flow beneath the site is anticipated to be relatively slow, <br /> especially below a depth of 40 feet <br /> • The vertical and lateral extent�ofa�scon matronin the soil have been reasonably <br /> well de ineated The plume is wlliptical in shape, with a long axis following the <br /> probable trace of the former pipeline from the dispenser to the USTs Contamination extends <br /> under the sidewalk on the Grant Street side of the property, but does not extend under the <br /> sidewalk on the Main Street side Contamination does not extend below the base of the <br /> channel sand that lies at a depth of 20-35 feet below the northwestern part of the site <br /> • Groundwater in the northwestern part of the site has been impacted, and contamination <br /> extends off site north of HP-4 and west of VM-1 Accurate delineation of the extent in those <br /> directions would be very difficult, because of subsurface obstructions and drilling restrictions <br /> in the streets Delineation of the eastern extent should be possible by completing VM-4 in the✓ <br /> shallow aquifer, as originally planned We recommend constructing a monitoring is <br /> boring, with screen from 35 feet to the present ottom of thehole, which we estimate to be 55 <br /> Data on bacterial activity and nutrient availability suggest that natural bioremediation of the <br /> contaminants at the site will be slow in the vadose zone above 35 feet, and negligible below <br /> that depth The low concentrations of contaminants also means that the food source for <br /> hydrocarbon-degrading bacteria is minimal <br /> 10 <br />
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