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ARCHIVED REPORTS XR0001011
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ARCHIVED REPORTS XR0001011
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Last modified
3/6/2019 7:46:40 PM
Creation date
3/6/2019 4:04:38 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001011
RECORD_ID
PR0544236
PE
3526
FACILITY_ID
FA0024238
FACILITY_NAME
JM EQUIPMENT COMPANY
STREET_NUMBER
1245
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323034
CURRENT_STATUS
02
SITE_LOCATION
1245 W CHARTER WAY
P_LOCATION
01
QC Status
Approved
Scanner
WNg
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EHD - Public
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Gealogual Technics tmc Page 5 <br /> ' V Quarter 2002 Groundwater Monitoring Report <br /> Project No 507 2 <br /> March 7,2003 <br /> • Deep well MW-109 continues to intennittently contain trace amounts of (at or dust <br /> ' above the laboratory reporting limits) BTEX contamination The reduction in <br /> contaminant concentrations from the first sampling event is noted, however sufficient <br /> monitoring has been performed to conclude that it is probably a drilling artifact or the <br /> bottom of the groundwater plume <br /> 0 Figures 4 and 5 indicate a previously inverse relationship between groundwater <br /> elevation and contaminant concentrations in wells MW-9 and MW-5 respectively <br /> ' These two parameters have demonstrated parallel slopes for recent events In Figure 4, <br /> the inverse trend was consistent for well MW-9 for the first four monitoring events, but <br /> since the March 2001 event the relationship has been predominantly parallel In Figure <br /> r5, the inverse trend was constant for MW-5 for the first five monitoring events, but since <br /> the January 2001 event the relationship has been parallel <br /> Trend lines added to the data in Figures 4 & 5 show that as the groundwater elevation <br /> has lowered since 1999 that the concentration of TAH-G has increased Suggesting that <br /> concentration is directly related to groundwater level <br /> ' 0 Figure 6 indicates an inconsistent relationship between groundwater elevation and <br /> contaminant concentrations in well MW-6 No data is included for the December event <br /> due to the well's inaccessibility <br /> o The groundwater gradient is relatively flat and the direction of groundwater flow has <br /> varied during the course of the investigation <br /> ' C Oxidation-Reduction Potential (ORP) was measured (Table 4) and the results suggest <br /> that with the exception of MW-2, all of the wells sampled are either in the core of the <br /> contamination plume or are immediately down gradient from the plume and within the <br /> ' halo of reaction depleted water caused by biodegradation of the contaminants <br /> s Figure 7 is a contour map indicating the TPH-G concentrations on December 20, 2002 <br /> The groundwater plume is localized in the vicinity of the former UST excavation The <br /> bulls-eye pattern to the TPH-G contour map in Figure 7 shows that the center of the <br /> plume has not moved from its source and suggests that contaminant migration may be <br /> occurring primarily by diffusion with a slight influence by advection <br /> r <br /> ' 3.0 CONCLUSIONS AND RECOMMENDATIONS _— <br /> Conclusions <br /> ' 1 Elevated concentrations of BTEX, TPH-G and MTBE are present in a laterally limited <br /> groundwater plume that is centered on MW-9 <br /> 2 The MTBE and previously monitored 1,2-DCA plumes are insignificant in comparison <br /> ' to the BTEX and TPH-G plumes <br /> 3 The lateral extent of the contamination plume is defined to the east, northeast and <br /> southeast by wells MW-3, MW-2 and MW-1 respectively <br />
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