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LIAR-24-99 16 35 From WOODWARD CLYDE + T-735 P 02/34 Job-492 <br /> EMCCICY TeStlngA FMd 09 MO <br /> [ASIS SOM099nu mas W Kabrs,BSG Douglas S Hodge,Ph D J Graydon Martz,BAG <br /> ASsTRACT <br /> Groundwater monitoring and sampling has bacorne ars integral part of site assessment and remodial efforts at <br /> facilities with chemically impacted groundwater significant efforts in boot the assessment and romedial arenas are <br /> being undertaken based on the Information generated during groundwater monitoring events Therefore, it becomes <br /> Imperative that the most reliable and accurate groundwater information be generated <br /> The reliability of groundwater sampling devices boars dimly on the reliability of groundwater monitoring data. <br /> Sampling deeviceo have boon evaluated for their capacity to provido roliabie samples(ltroalona, M J , et al , 1984) <br /> for laboratory analysts.The most reliable,to date,have boon the check-valve bailor and the gas-operati;d bladder <br /> pump These devices have their draw-backs,primarily by the targe amount of contaminated purge water croatod and <br /> the trate necessary to purge the well pnor to obtaining the sample The KABIS Sampler was tested against the <br /> check-valve bailor for over-ail accuracy in two ways The KABiS Sampler was shaven to be superior to the <br /> Check-valve Beller in all categories of the test. <br /> INTRODUCTION <br /> Until recently, groundwater sampling was performed using a handful of groundwater sampling devices,each with its <br /> individual set of sampling errors and sampling idiosyncrasies A large amount of purged groundwater was produced <br /> from each sampled well under the presumption that a sample representative of formational conditions could be <br /> collected <br /> The presumable reason for purging is to refresh the stagnant borehole water with representative formational water <br /> This Is boat-out by the early data, but is a potential misnomer because thore is widely varying scientific ovidence and <br /> opinion on the number of stagnant borehole volumes to purge.There are even varying opinions on exactly what <br />® constitutes a borehole or well volume <br /> The most reliable sampling devices were identified by screening fourteen different devices from five mechanistic <br /> categories(Barcelona,et a, 1954) The results of Barcolona's scresining have become the equipment protocol <br /> (TEGD)basis for nearly SM/6 of currently recommended sampling activities The KAKIS Sampler is a new adjunct to <br /> that list <br /> LITERATURE REVIEW <br /> Many articles have been published on the pmblern of obtaining representative groundwater samples from rapidly <br /> recovering ground-water monitoring wells Scan, et al I reported In a 1981 paper that bacterial activity can <br /> dramatically affect VOG analysis results Dissolved VOCs can effervesce in as little as 2 hours after sample <br /> acquisition Seanor and BrannaW note(%in their 1853 paper that water in ground water monitoring wells standing <br /> considerably above the screened interval and not in communication with formational water is stagnant This standing <br /> water is subject to dmerent chemical equilibria and often has different pH,EC,temperature, and dissolved solids <br /> Wilson and Dworkins reported in their 1984 paper that rust and scale from ground-water monitoring wells may <br /> interfere with laboratory analyses,as may the proseince of colloids and clay platelets <br /> Barcelona and Helfrich4 concluded.in 1986,that no or improper purging of a ground-water monitoring well was a <br /> greater cause for sampling error than was sampling method,well construction materials,or sampler matenals They <br /> went so far as to state that improper purging was the dominant error factor in groundwater sampling <br /> WB Puroina <br /> The universal goal of well purging is to remove°stagnant"water from the well,creating very little disturbance to the <br /> groundwater flow regime Recommended purge volumes range from one(1)to twenty(20)well bore volumos, <br /> • <br /> 1 of 14 3124199 4.21 PM <br />