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ARCHIVED REPORTS_XR0012626
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0543041
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ARCHIVED REPORTS_XR0012626
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Last modified
5/18/2020 3:03:14 PM
Creation date
5/18/2020 2:45:25 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012626
RECORD_ID
PR0543041
PE
2960
FACILITY_ID
FA0024604
FACILITY_NAME
HUMAN SERVICES AGENCY
STREET_NUMBER
145
Direction
S
STREET_NAME
SUTTER
STREET_TYPE
ST
City
STOCKTON
Zip
95202
APN
14912016
CURRENT_STATUS
01
SITE_LOCATION
145 S SUTTER ST
P_LOCATION
01
QC Status
Approved
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EHD - Public
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�.a <br /> I <br /> As was the case with the soil action levels the <br /> groundwater <br /> cleanup concentrations vary in a case by case scenario based on <br /> the site characteristics. <br /> 5.0 SITE CONDITIONS <br /> 5.1. Site Geology <br /> The subsurface geology at the site is characterized by unconsoli- <br /> dated sands, silts and clays exhibiting little lateral continui- <br /> ty. Although no continuous beds were discernible, a medium to <br /> coarse sand with variable silt content was observed at all well <br /> locations beginning approximately 20 feet below ground surface <br /> (BGS) . This coarser zone extended to at least 35 feet BGS at all <br /> well locations. <br /> At monitor wells location MW-1 and MW-S, the saturated formation <br /> was typified by coarse materials (medium to coarse sands and, at <br /> MW--1, fine to medium gravels) . The saturated zones for wells <br /> MW-1 and MW-3 were encountered at 28 feet BGS and 26 feet BGS <br /> respectively. At MW-2, however, the saturated material was a <br /> sandy clay encountered at a depth of approximately 36 feet BGS. <br /> in general, the soil observed at all depths at MW-2 was much <br /> finer than at the other well locations, with the dominate soil <br /> encountered being a silty clay. <br /> 5.2 Groundwater Gradient s. <br /> Upon completion of the well development the depth to water and <br /> top of casing measurements were obtained. This information was <br /> used to determine the site groundwater gradient. From this data, <br /> it was found that the site gradient (groundwater flow direction) <br /> p, is primarily northeast (Figure 4) . <br /> 6.0 CONCLUSIONS AND RECOMMENDATIONS <br /> Based on the analytical data, hydrocarbon compounds exist within <br /> the soils and shallow groundwater at the site in excess of <br /> typical cleanup levels. The chemical concentrations present <br /> within the soils and groundwater suggest that site cleanup can be <br /> accomplished via limited activities based on the following; <br /> o For conducting an evaluation of remedial actions at u:_a <br /> subject site, the L.U.F.T. field manual ri: .% assessment and <br /> [. decision tree flow chart methodologies can be utilized. <br /> Figure 5 presents the decision tree flow chart and graphi- <br /> cally presents the path followed for the evaluation of the <br /> Human Services building site. As can be seen by following <br /> the path; soil cleanup .is recommended. <br /> o The hydrocarbon presence within the soils appears to be <br /> limited to a relatively small area centered around borehole <br /> #3. <br /> - 10 - <br />
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