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3 All_ <br /> Quarterly Monitoring Report, First Quarter 1990 September 17, 1990 <br /> AGS 38012-2 <br /> Former Unocal Station No. 2859 <br /> In lune 1988, we observed the drilling of three soil borings (B-1 through B-3) and <br /> installation of three groundwater monitoring wells (MW-1 through MW-3) in the borings <br /> (Plate P-2). Soil samples were collected from the borings and groundwater samples were <br /> collected from the monitoring wells for laboratory analysis of hydrocarbons. In August 1989, <br /> we observed Spectrum Explorati-}n, Inc. of Stockton, California, drill borings B-4 through <br /> +" B-6 (Plate P-2). Soil and ground-water samples were collected from the borings and wells <br /> for laboratory analyses. Hydrocarbons were detected in sail and groundwater samples <br /> collected during both site visits. <br /> In response to the detection of hydrocarbons in soil and ground water,Applied Geoiystems <br /> began periodic monitoring of the ground water in June 1988. Results of previous <br /> monitoring hlt ty5tected in 5 <br /> ells <br /> W-2anMWt3lowereels have been detected n wells xjW-1, -4 were Band M � . <br /> Present uarter! <br /> Monitoring Event <br /> A geologist visited the site on March 1, 1990,to measure the depth to water and subjectively <br /> analyze ground water in monitoring wells MW-1 through MW-5 and to sample the ground <br /> water for laboratory analyses. The depth to the groundwater surface was meafrom <br /> the top of the well casing to the nearest 0.01 foot with a Solinst water riodendicator. <br /> r <br /> Y, Depth-to-ground-water data were combined with the elevation of the top of the well casing, <br /> previously surveyed by Moldenhauer Engineering Company(a licensed land st!rveyur frc-1 <br /> Davis, California) an September 21, 1989, to compile a Potentiometric Map (Plate i?-3). <br /> he G&�Con <br /> Data used to compile Platt are shown in Tt and the averagebg adient to be 0.0024.le 1. We evaluate6f The:c data arae <br /> groundwater flow to be no <br /> consistent with the flow direction and gradient previously evaluated. <br /> Samples of ground water were taken from the monitoring wells for subjective analysis using <br /> the methods described in the attachment to this report. The geologista exinno cd he sa celes <br /> for floating product, sheen, and other subjective evidence of by <br /> of <br /> hydrocarbons was noted. Results of subjective analyses are presented in Table 2. <br /> The geologist purged approximately 3 well volumes (30 gallons) of ground water from the <br /> five wells using a submersible pump. The wells were allowed to recover to near static water <br /> levels. The geologist then collected groundwater samples from each well for laboratory <br /> analyses. The methods of ground-water sampling are discussed in an attachment to this <br /> beled 17-E see <br /> ending te <br /> report. The purge water Se star ewater was subsequenily remnsite in properl oedtbylA mourdrumspPetro!uhm <br /> results of laboratory analyses. <br /> of Fairfield, California, and recycled. <br /> -- 2 <br /> Applied GOOSYStOMS <br />