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1444 MARIPOSA ROAD <br /> WKA No. 2938.07 a <br /> . January 18, 2001 <br /> Page 2 <br /> Of the analytes examined, Tert-Butanol was the only one identified during this sampling event. <br /> It was reported at a concentration of 13 ug/l in well MW7 This is consistent with findings from <br /> the April 18, 2000 sampling event when Tert-Butanol was reported in MW7 at a concentration of <br /> 11 µg/1. Tert-Butanol was not reported above detection limits in the water sample obtained from <br /> MW2 This finding represents an apparent improvement in water quality from the April 18,2000 <br /> sampling event when Tert-Butanol was reported in MW2 at a concentration of 8.4 ug/1 and MTBE <br /> was reported at concentration of 0 78 ug/l <br /> Dunng the most recent sampling event,the depth-to-groundwater measurements in wells MW2 <br /> and MW7 were recorded at 50.40 feet and 50.34 feet below top of casing,respectively. Free <br /> product, sheen or petroleum hydrocarbon odors were not observed during groundwater <br /> monitoring and sampling activities. The measured depth to groundwater is consistent with recent <br /> measurements for the site. However,it should be noted that while well MW7 is screened at a <br /> depth suitable to intersect the soil/groundwater interface,well MW2 is not. Since screening <br /> across the soil/groundwater interface is usually considered a requirement when evaluating a <br /> petroleum hydrocarbon site,the above situation wan-ants discussion if the site is to be considered <br /> for low risk status. In light of this present situation,we will provide a bnef history before <br /> discussing any adverse possibilities related to the well construction. <br /> Wells MWl through MW3 were constructed in October of 1993 at a time when extended draught <br /> condition prevailed in California. At the time of construction,the depth to groundwater was <br /> measured at approximately 74 feet below ground surface• the screen interval was accordingly set <br /> from 64 to 84 feet below site grade This construction practice was and is considered common <br /> and in most cases provides a more-than-adequate range within which groundwater can fluctuate. <br /> r <br /> However, since 1993, the local groundwater has risen approximately 20 feet beneath the site. <br /> Because of extreme nse in groundwater,the tops of the screened interval in wells MW 1 through <br /> MW3 are presently 14 or so feet below the water surface. This means petroleum hydrocarbons <br /> that primarily float on the water surface are unlikely to be drawn through the perforated casing <br /> during well purging and sampling Under a scenario where little or no site history exists,this is a <br /> very serious consideration on which to base final closure recommendations. The case of the <br /> above site,however, is somewhat less troublesome in that almost eight years of data exists for <br /> the three"inundated"wells. <br />