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ranged from 6.70 in MW-1 to 7.06 in MW-3. Groundwater temperature ranged from 18.9 <br /> degrees Celsius in MW-3 to 22.3 degrees Celsius in MW-2. Conductivity ranged from <br />' 1090 micro ohms in MW-2 to 2530 micro ohms in MW-3. The wells were allowed to <br /> recharge a minimum of 80% before sampling. Samples were collected from each <br /> monitoring well along with a blind duplicate. Water samples were collected by lowering a <br />' disposable bailer below the static water level, and raising the bailer slowly in order to <br /> minimize agitation of the water sample in the bailer. <br /> Water was discharged from the bailer through a bottom discharge valve. Discharge to the <br />' sample container was at a rate slow enough to minimize bubbling or significant agitation of <br /> the liquid. The sample container was filled to the top (from the bottom up) and overfilled <br /> leaving no headspace. <br />' The samples were collected in laboratory-approved glass vials and bottles. Following <br /> collection of the samples,they were placed in an ice chest cooled with ice to a temperature <br /> of approximately 40°to 50°F. <br /> Samples were then delivered to the laboratory within 24 hours of collection. Sample <br /> handling, transport and delivery to the laboratory were documented using chain-of-custody <br />' procedures, including the use of chain-of-custody forms. <br /> Quality Assurance/Quality Control <br />' To increase the confidence levels in the data obtained and minimize the likelihood that <br /> judgments were made from potentially erroneous data, a quality assurance/quality control <br /> (QA/QC)program was implemented. <br /> The program includes formal procedures for drilling, sampling, decontamination, <br /> instrument calibration, documentation of field activities and calculations, and peer review. <br />' Routine QC procedures were performed by the laboratory,and included daily calibration of <br /> instruments, percent surrogate recoveries, and analysis of matrix spikes and matrix spike <br /> duplicates. The laboratory reported the results to be within acceptable percent error with no <br /> results exceeding the laboratory-established control limits. <br /> Decontamination <br />' The hollow-stem augers were decontaminated prior to the advancing of each boring. The <br /> sampler was decontaminated between sampling intervals, using a bristle brush, with a <br /> trisodium phosphate (TSP) solution; this was followed by two tapwater rinses. The <br /> sampler was dried by air prior to use. <br />' Waste Disposal <br />' The soil cuttings and purge water produced during the site investigation were placed in <br /> DOT drums and stored on site pending analytical result. The soil cuttings and purge water <br /> will be transported and recycled/disposed of by a licensed hauler in accordance will <br />' appropriate regulations. <br /> FIELD OBSERVATIONS <br /> Soils beneath the site consisted primarily of silty clays, silty sand and silts. Groundwater <br /> was encountered at approximately 55 feet bgs during drilling activities. Elevated PID <br /> 8 197046a - Stockton <br />