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L <br /> i <br /> FI <br /> 1 <br /> May 10, 1987 AGS 86103-2 <br /> cardlock Station #27 - Stockton, California <br /> After subjective sampling, the wells were developed by air <br /> surging and pumping. Approximately 25 gallons of water ( five to <br /> x <br /> six well volumes) was pumped from each of the wells prior to <br /> r sample collection for laboratory analysis . After development <br /> r pumping and well recovery, ground water samples were collected <br /> using a teflon bailer cleaned with acetone and rinsed with <br /> deionized water. The bailer was lowered through the air/water <br /> interface in order to retrieve a sample representative of the <br /> ,{ rr formation water, <br /> a <br /> -k Two laboratory-cleaned 40 ml glass sample vials and one 1 liter <br /> glass sample container were rinsed with water collected with the <br /> _ , <br /> bailer from each well. The water sample was then slowly <br /> � - transferred to the containers, which were then sealed with <br /> +_ - teflon-lined caps and placed in iced storage for transport to the <br /> analytical laboratory for testing. � L <br /> ANALYTICAL RESULTS <br /> W Soil and water samples collected during this study from each of <br /> h <br /> the soil borings and monitoring wells were selected for <br /> r - <br /> laboratory analysis. All samples were tested for total volatile <br /> { hydrocarbons, total extractable bydrocarbons, and volatile <br /> M <br /> 4 <br /> 8 <br /> BQ010999 <br />