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` III <br /> oints <br /> sampling P <br /> fest. Therefore,the spatial frequency of l <br /> signed. <br /> 1) Questions of Scale should be carefully selected and de <br /> f Sampling Point Design <br /> A sampling plan designed to collect representative 2) Flexibility o , <br /> samples must take into account the pace tenand time as well as In most cases well-point al scale Of diametersof submer5 b g f t 7` <br /> changes in site conditions through sp inches will permit the use of most types <br /> the chemical associations and behavior of the parameters <br /> pumping devices far tow-flaw (minimal drawdown}sampling <br /> that are targeted for investigation.ln subsurface ernes aver time or P is suggested that short(e.g.,less than i.fi m}screens be <br /> physical(i.e.,aquifer)and chemlcat <br /> properties <br /> rit. In fact, incorporated into the monitoring design where Possible so <br /> space are not statistically iendeNp nd distances of samples ewmeters) that mparable results from one device to an,other gvertVcal <br /> taken in close Proxim ty{ is relative to the deg <br /> expected. Short,of course,expected at site. <br /> or within short time periods(tela,more frequently man water quality variability expo <br /> monthly)are highly auto-corrslated. This monthly)or deneans that se <br /> in frequency( .g., lin Point <br /> empial mg high-samPf' g 3) Equilibration of Sam¢ g <br /> spatial monitoring designs run the risk of 1`8 $��a'ia <br /> collection and misleading'inferences regardingactice, contaminant Time should be allowed for equilibration of the wet! <br /> values that aren't ststisticalVy valid. In rarely suffer or sampling point with the formation after installationPlace- <br /> detection <br /> `lies- <br /> detection and assessment monitoring eprogramsmerit of well or sampling points in the subsurface Produces <br /> c1•iniq s <br /> these over-sampling concerns. in corrective-action evaluation <br /> some disturbance of ambient enc ia6�y Drilling <br /> ie ed to cause <br /> Programs,ft is also Possible that too little data may be e. auger, rotary,etc.)are g <br /> Coll over space or time. In these cases,false interprets- more disturbance than direct-push technologies-s)deither;er <br /> kion of the spatial extent of contamination esus underestimation ( g there may be a period(i.e.,days different <br /> of temporal concentration variability may case, be distin Of <br /> Sam- <br /> which water quality near the point may <br /> 2) 'Target Parameters from that in the formation.Proper development of the <br /> lin Dint and adjacent formation to remove fins5 created <br /> e ov� <br /> Parameter selection in monitoring Program design is piing p <br /> during emplacement wilt shorten this water Reality <br /> most often dictated by <br /> the regulatory status of the site. period. <br /> However,background water quallty constituents8SQr9i nt targets <br /> Procedures used in and Sampling <br /> indicator parameters,and c S. <br /> Theitoo s and P11 p ticable Ill, Definition of Low-Flow Purging <br /> for data cottectlon programs. <br /> In these programs should be equally r�beneeded o deter- tt!s generally accepted that water in the well casing <br /> to atl categor.05 of data,since all may <br /> mine or support regulatory action, is non-repreSto colt a of the formation water and needs However,e <br /> pnstructi°n purged prior to collection of ground-wa 9ndeed ble represerita- <br /> C. Sarnpf1ng point Design and C the water in the screened interval may <br /> central to all five of the formation.depending purged well mnextent for the <br /> site hydrogeotogY• Welts are purg <br /> Detailed site characterization is following reasons:the presence of the air interface ra the top <br /> and the basis for this characterize- en concentration <br /> decision-making purposes <br /> 4e of the water column resulting in an OX) <br /> tion resides}i$'identificationral hniis. Fundamentalu �� dot po re p gradient with depth,loss of volatiles up the it er pack`chemical <br /> major hyd head-differences 9 <br /> point location include: subsurface lithology, tin int teaching from of sorpeeaVs orhbafilnd surface infiltration. <br /> and background geochemical conditions. Each sampling P° changes due to clay <br /> tow-flow purging,whether using portable or dedi- <br /> has a proper use or uses which should <br /> program documented a a using pump-intake located in <br /> level which!s appropriate for the program's not always be be <br /> objectives. Individual sampling points may rated systems,shouldabovsahe middle ai the screened <br /> detection. the middle or slightly <br /> able to fulfill rriultl,fe rmonitorsng objectives(e•g. interval. Placement of the pump <br /> too close to the bottom of the <br /> assessment, corrective action). well will cause increased entrainment of solids which have <br /> with Monitoring,ingrain and Data collected in the well over time.a result onor purging and sampling re present as <br /> 1) <br /> Compatibility f well development,p <br /> Quality Fjb4eotives events,and natural colloidal transport and deposition. <br /> int location and design will in the middle or toward the <br /> specifics of sampling Po 'therefore, placement of the pump suggested <br /> Placement of the <br /> be dictated by the complexity of subsurface lithology and top of the screened interval is <br /> variability in contaminant andlor geochemical conditions. It pump atQ�ede�p�of <br /> e water <br /> aquifers,ers, screenedcolumn for gacross <br /> the <br /> raund•water sam- recommended Point <br /> should <br /> Low- <br /> should be noted that, Low- <br /> regardless (e.g.,wells, drive-points, <br /> a roach, few sampling p water tabte,where this is the desired sampling P <br /> ,ling pp have zones of influence in excess of a few <br /> screened augers) <br /> 4 <br />