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USA 65 - QTR RPT 12/94 <br /> north, northeast from MW3 to MW2 , see Figure 4D Unlike the <br /> previous ground water gauging period (Figure 4C) the hydraulic <br /> gradient across the site is less stable, indicating that this may <br /> reflect a condition of flux between the inflow and outflow of <br /> water to the local aquifer and is represented by a variation or <br /> differences of hydraulic conductivities from well to well, this <br /> is expressed at the site by a 'high water ridge' from MW5 and MW3 <br /> and a ' ground water low' from MW3 to MW2 <br /> SITE INVESTIGATION <br /> Ground water sampling was conducted on December 28, 1994 in <br /> compliance with the quarterly monitoring requirements for this <br /> site The various ground water parameters were determined by 1) <br /> recording depth to water (by use of a resistivity meter) at each <br /> monitor well , 2) purging and containment of ground water from the <br /> wells, 3) collecting water samples from the wells, 4 ) submitting <br /> these water samples to a State Certified Analytical testing <br /> laboratory via established "chain of custody" procedures <br /> The water samples were analyzed for Total Fuel Hydrocarbons (TFH) <br /> as gasoline and Volatile Aromatic Hydrocarbons (BTEX) using EPA <br /> Methods 5030 and 602 , respectively Laboratory detection limits <br /> are as follows TFH is 0 02 mg/L and BTEX is 0 5 �tg/L <br /> Methods and Procedures <br /> The ground water was sampled in eight monitoring wells (MW1 , MW2 , <br /> MW3 , MW4 , MW5, MW6 , MW7 and MW8) by a Western Geo-Engineers <br /> (WEGE) geotechnician working directly under the supervision of <br /> California Registered Geologist ##3037 Prior to sampling each <br /> well , the WEGE geotechnician measured the depth to ground water <br /> using a resistance probe A ground water contour surface was <br /> later plotted from these depth-to-water measurements, ground <br /> water flow directions at the site were then inferred from the <br /> contour gradients This information is presented in Figure 4D <br /> Each well was purged before collecting water samples Purging <br /> was completed only after water temperature, pH, and conductivity <br /> had stabilized Purged water was contained in a labeled, secured <br /> 55 gallon drum on site <br /> The wells were allowed to recover after purging A water sample <br /> was then collected with a fresh bailer Each sample was divided <br /> among three 40-m1 VOA vials The vials are supplied pre-cleaned <br /> to exact EPA protocols and contain the appropriate preservative <br /> The sample vials were labeled as to station, well, time, and <br /> sampler, and documented on the chain-of-custody sheet, they were <br /> then placed into an ice chest with a travel blank and cooled to <br /> 40C with ice The samples were delivered to a California State <br /> 3 <br /> i <br />