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jll is 1 - w l li[�1 �,., 1 t• e . ' c .F r. a - o + s,- .+ <br /> i I ,ji T• a r « I + N' f ,ti i t F I , I° al n `; <br /> I <br /> il ; <br />�1IfF ri Y � .� I t Fly -.N ' - ••r r £ ; ,; , ' p F k' I 14''•i!}I!i{flrynl��!� <br /> 1I�' �I;t <br /> VOW,"!i "' s f iµ <br /> »�r9��20.November-1998 3 ' , , ' •,,' , ; 4 ,? t , .� 4 y t,j ` .,: y , ,F }' r l4'A'.''r. <br /> , <br /> ojedtNo. 95-0124 - <br /> ,F -AGE NC.,Pr <br /> r • 1 r <br /> S G NI F - ,. .1 f I. I i' ' ' i 1�•''. <br /> 12.2 �LOLL-ECTION`OF.GROUND�WATER SAMPLES <br /> I f <br /> Dunn .both sampling events <br /> g p g. ground water samples were:collected `from each'' well:using,new <br /> ii disposable baileis. Ground water samples were'collected directly nfollowing the purging of each well <br /> 4 I < <br /> r 0 r F § <br /> in an attempt to sample while the'recharge water was within the screened interval of the moriitoring7 <br /> we-, <br /> ` r .s I1S. _I .I r- , .. . - '. r'' •' ', t r' t i i l , <br /> 4mrnediately;upon retneval,,the samples were transferred into 40=rill'EPA=approved"VOA'vials;' r <br /> # containing 0S In of hydrochloric acid,(18%)'as a.sample preservative,' and'were-`labeled: The ' <br /> ' samples were transported iri a chilled'containerunder:chain:Of-custody.to McCampbell Analytjcal, , <br /> -Inc.,-(IvIAI)a state-certified laboratory�in.Pacheco,California. Samples were,analyzed iri accordance' <br /> i i � with •' ' . - ; . . , _.,.V�. -• ,,; ',f•: <br /> Ia <br /> EPA,Method,801.541 for total petroleum hydrocarbons quantified as Stoddard solvents(TPH-.' r <br /> ^ `ss),° j i <br /> EPA Method 8020 for volatile aromatics x ' <br /> (benzene;toluene, ethylbenzene and total xylenes: <br /> BTEX) and <br /> • EP,A.Method'8010•for volatile halocarbons (chloririated.hydrocarbons): <br /> 3.U. FINDINGS <br /> 3:1. .GROILND'WATER GRADIENT AND DIRECTION <br /> The groundwater elevations were calculated by subtracting the measured depth to groundwater <br /> from the•surveyed casing elevations{Table l). Ground water'elevations were plotted:and"contoured tr <br /> on a scaled site•map: <br /> The average relative ground water elevaiion'at the site increased approximately 4.5 feet between the <br /> 4' <br /> •December 1'997-and ihe.March I998-sampiingevents:During the March 1998 sampling,,theldepth <br /> . , <br /> to ground water at the site' 'ranged from 23.17 to 24:41 feet beiow,tops of ihe'.we11 casings.. aY ' <br /> During the July 1998 said liri the depth to-ground water at the site ran ed from 21'.681to 22:39 feet <br /> P g, g <br /> below cops ofae well casings: The average-relative.ground-water elevation"at the site increased <br /> approximately 1.6 feet since the the March and Jul •19 <br /> = Y. 98 sampling event <br /> a r 1, .hq . . , r -• _' • '• '. "" �::: •-- .' . ',; '', .• ? , .. '.+ r.i' ��, <br /> Theacreened intervals in wells MW-f and MW-2 lie between 34 and 54 feet bsg, and the.screened <br /> intervals in wells MW-3R,MW-4 and MW75 lie between 0-and SO feet bsg,`thus,groundwater is 3 ;. <br /> �F r I Ar Yanmd.GeoEavirorimenial,In G <br />