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KEI-P88-1013 .QR5 <br /> August 9 , 1993 <br /> Page 2 <br /> Water samples were collected by KEI from all of the Unocal wells <br /> (except MW6) on June 28, 1993 . Prior to sampling, the wells were <br /> each purged of between 6 . 5 and 8 gallons of water by the use of a <br /> surface pump. During purging operations, the field parameters pH, <br /> temperature, and electrical conductivity were recorded and are <br /> presented in Table 3 . Once the field parameters were observed to <br /> stabilize and a minimum of approximately three casing volumes had <br /> been removed from each well, samples were then collected by the use <br /> of a clean Teflon bailer. The samples were decanted into clean VOA <br /> vials that were then sealed with Teflon-lined screw caps and stored <br /> in a cooler, on ice, until delivery to a state-certified labora- <br /> tory. <br /> On June 28 , 1993 , a joint monitoring and sampling event was also <br /> conducted with the nearby Montgomery Ward site (the site of a <br /> former service station) . Monitoring data from the Montgomery Ward <br /> site are summarized in Table 2 . <br /> HYDROLOGY <br /> The measured depth to ground water at the former Unocal site on <br /> June 28, 1993 , ranged between 56. 66 and 57 . 73 feet below grade. <br /> The water levels in all of the wells have shown net decreases <br /> ranging from 3 . 16 to 4 . 50 feet since March 25 , 1993 . <br /> Based on the water level data gathered during the joint monitoring <br /> event conducted on June 28, 1993 , the ground water flow direction <br /> over the majority of the site vicinity was to the south, varying <br /> from the south-southeast to the south-southwest, as shown on the <br /> attached Potentzometric Surface Map, Figure 1. Based on the water <br /> level data gathered during the May 27 , 1993 , and April 26, 1993 , <br /> monitoring events, the ground water flow direction at the Unocal <br /> site appeared to be to the southeast, as shown on the attached <br /> Potentiometric Surface Maps, Figures 2 and 3 , respectively. The <br /> ground water flow direction at the Unocal site has varied from the <br /> southwest to the east-northeast since July of 1992 . The average <br /> hydraulic gradient over the ma3ority of the site vicinity on June <br /> 28, 1993 , was approximately 0. 008 . <br /> ANALYTICAL RESULTS <br /> The ground water samples collected from all of the existing Unocal <br /> monitoring wells this quarter were analyzed at Sequoia Analytical <br /> Laboratory and were accompanied by properly executed Chain of <br /> Custody documentation. The samples were analyzed for total <br /> petroleum hydrocarbons (TPH) as gasoline by EPA method 5030/modi- <br /> fied 8015 , benzene, toluene, ethylbenzene, and xylenes by EPA <br /> method 8020 , and for EPA method 8010 constituents. <br />