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4Wt4gXA1 Tecluucs 1XC Page 7 <br />Groundwater Monitonng Report <br />' Project No 724 2 <br />February 13, 2006 <br />' 3.0 CONCLUSIONS & RECOMIIMNDATIONS <br />t Based on our interpretation of the data collected over the course of this subsurface <br />investigation, GTI has reached several conclusions These conclusions assume that the <br />premise that the data we considered, although incomplete, are representative of actual site <br />' conditions We acknowledge that there may be undiscovered conditions, which would upon <br />their consideration, change our interpretation and thus our conclusions <br />' Conclusions <br />The groundwater plume does not display a typical "core" but exhibits wide variations <br />in contaminant concentration in both vertical and lateral planes as shown in Figures 6 <br />- 12 Generally the plume has migrated down gradient of the source and is displaced <br />east of the former UST <br />o The highest MTBE concentrations detected in the intermediate and deep aquifers <br />' were in wells MW -106 (25 lig/1) and MW -209 (8 4 tAg/1), respectively <br />o Water table well MW -7 contains 2 2 ug/]L MTBE <br />o The contaminated shallow, intermediate and deep wells are down gradient from <br />' the former UST and dispenser locations areas in the predominant groundwater <br />direction to the east <br />o The highest TPH-G concentrations were detected to the east of the site in wells <br />MW -106 and MW -208, and the highest Benzene concentrations were detected to <br />the east and northeast in wells MW -106 and MW -109 in the intermediate wells, <br />' and MW -208 in the deep wells, respectively <br />o The presence of 53 ug/1 TPH-G in deep well MW -210 is the first contaminant <br />detection recorded for this well <br />' r In their correspondence dated September 3, 2002, the San Joaquin County <br />Environmental Health Department (SJC/EHD) identified two LUFT sites (701 E <br />Charter Way and 749 E Charter Way) as being up gradient of the subject site The <br />' contamination detected in the MW -108/208 location may be partly or entirely <br />originated from an offsite source <br />• The SJC/EHD also stated in their above letter that a sandy interval at 70 — 80 bgs <br />' could be acting as lateral conduit for contaminant migration The presence of <br />contamination in deep wells MW -208 and MW -209 support this theory However, <br />GTI still suggests that the low concentrations of TPH-G & MTBE in these wells do <br />' not warrant an engineered clean up <br />4 The data shows that a relatively stable, wide spread, low concentration plume of <br />' petroleum hydrocarbon compounds is present in the groundwater at this site The <br />deeper TPH-G plume is not defined to the north and the deeper MTBE plume is not <br />defined to the east <br />