Laserfiche WebLink
''I �'y'. .n .'" - T .1. .. ,.. ,..:f- r`a+ '�•'.3-1,- w' ,- ......y✓ '.5., k...,^«. «.f.S..Y. ,,,. ,�'.: <br /> {,1.28 April 1997 Y '. i.-_ ,,11, f R'1• ,.f <br /> A6&,Project'No 6'0232 <br /> F Page 4 of 9 ; <br /> . 11 <br /> oil <br /> Jurassic complex of igneous and inetamorpluc basement rock <br /> 7: GROUND WATER DEPTH AN 'FLOW DIRECTION "" x <br /> Review of Lines'of Equalb'th`of Water-Wells.Fall 1993 published by the"San Joaqurn'CountyS< r i. <br /> Flood Control'and Water:Consezvation District suggests that the wer-'table surfa6e Beneath the site <br /> I 'occurs at a depth of approximately 15 feet bsg'. The uppermost ground.water flows in a unconfined I ;51a; <br /> f av0r.`With increasing dep'k the aquifer becomes semi-confined' <br /> ',,due,ta the`presence of f ne-grimed <br /> F 4 ' • <br /> 5edimenfs. i <br /> i. <br /> - <br /> ,, ;< Base _ 4 _ <br /> d-upon.informd6ji obtained-from� the:PHS,EHD; the prevailing ground'water flow.direct on-fin <br /> - the area of-the 'site is generally toward the north ,However, ,groundwater mon.iforin& events <br /> performed'at the site iri July and August 1996 'that aground water flow direction is <br /> 'ei n rally ; <br /> `toward the south. <br /> ADDITIONAL SUBSURFACE INVESTIGATION ' <br /> 3.I. DRILLING AND SA1\ZPLING'' .. <br /> 4n16•July I996 . .- ; , . ,. . `- , . • ,� - ' - � ; • 4. <br /> e <br /> on „soil'boring (MW-4) was adva.nced at the site to a depth ofapproximately 25. <br /> feet b_sg utilizing'a CME-75 truck mounted'drill-rig equipped!with'eight-inch'diameter,'hollow stem <br /> au ers Cuttings and `roseate enerated'durin drillin activities.were laced in ro erl` �ylabeled <br /> g . Ig,l , g g' g p ; P. .P. ..Y `."':.. <br /> ' D:O:T. model 17H 55-gallon'. .!dhims'and were,stored on site �n an.area lacking.pu�lic access .The <br /> location'of soil boring M'W=4 is depicted"oi Figure'-2. <br /> Discrete soil samP les were collected at-five-fobfintervals be"'' ata de th.,of'S feet'bs <br /> , <br /> g g• P g, utilizing <br /> a Califorl id-split-spoon saliipler and:brass'sle'eves. The sampler'wa's driven by dropping'a 140-pound <br /> r r <br /> Iweight from a.lieight of 30 inches:The number'of blows required,to'advan' each 6= nch;leilgth of <br /> the sampler.;(blovv counts) was recorded on boring Iogs by-an AGE-staffgeologist(Appendix B) <br /> a <br /> }. <br /> Upon-sample retrieval,.•the,middlebrass,sleeve was removed from the.sampler Both ends of the r <br /> r <br /> sleeve were`cover-ed`With-TeIIon-sheets;capped'and sealed;with tape:.Each.sample was labeled with ; <br /> E <br /> the.f boring location,.;depth tame `date' and sampler's'in'itials. The samples were;placed in <br /> If r` a chilled container and•transported,under chain of-'custody' toa.Castle''Analytical, Laboratory, a <br /> California"state-certified';•laboratory.•.Selected soil.'samples -were 'analyzed for total-,petroleum. <br /> hydrocarbons quantified as gasoline and diesel (TPH=g and TPH-d),''volatile aromatics (BTE&X) ' <br /> with'methyl-tertiary;butyl'ether(MTBE)in accordancewith'EPA Methods 8015M, $0.15M:and'8020. <br /> . I <br />