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our�eS The re5ult5 Of the <br /> a teat to gr°unQdra on°pt4on <br /> and do not pose a feasible <br /> over time a ,spi}exca�'auon was .Lawrence <br /> lip and destud�l indicate that the S C� by pi�-g <br /> a scale pi}°t Study repared for rive the 'Cleat other sites, <br /> edtiation recently p nce length and <br /> Intrinsic Blarem the rep°� RecQm ends cans ca and expenlimit the ~,,rater <br /> d in entitled, <br /> ongoing researSU icientlY to and grO,�n dwater <br /> sions containe� androcarlanns soils in grqun <br /> the co <br /> nclu nr at�rld subsurface ascribed aerobic, <br /> even ore-11, rtial �-ab a be degradt bons in is well d attonDD�leve}s <br />,3�aerM tcr's Lea T' Gasses in `� hydrocar microbes of hioattenu <br /> o� Call or' Citation. pro etroleu Knaus, sub surface three patterns oxygen � ver~ <br /> c f the p indi& marlxed when dissolved acceptor to con <br /> ntrinsic bice b ve sum rs lls tr e depleted, angerrate <br /> ration pctenttal drocarlions Y 1RgA} ha enerai}Y °cam as ane nitrate- <br /> j)0 <br /> e radation of by �hlarlg ar}ation g s utilize oxygen O levee tar such as <br /> Biodegradation},dc�l;star an aerobic biodegr rob when D ccep to of , ttliztug the <br /> Indigenous mic biomass alive electron a cap dation occurs <br /> 1}teraturec and hYp°X water as r an alters MW b,Odegra der hypoxi s <br /> i <br /> anaerob than } to 2 m�Xide. taccu In a,aditton, oxtc <br /> reater £arban adation to resent HYP occur u alien 1 <br /> are g rbol*s to Far blodegr be, avaltable ustbeP xadation maoxic biod grad <br /> hydroca xevaiI carbanat�e muse hydreiearbo-R M Biodeg of hYp <br /> conditionrorl VIII} ar for to degra atelY ) l to 2 m p, ditional study <br /> sulfate, leGtr°r` acceV een aperoxim is available including D <br /> altexnative e are betty crept°r mechanism he,�,tcal tndicatars' and methane <br /> levels electron a this dioxide the pion'"' <br /> when D� a seconda�` lately quantify lwmerous 9, (11), Garb°n utside of <br /> pro�sided ore comp b inside and fated <br /> iron ° <br /> necessary <br /> to demonstrated-atrate, ,,fate, n be calcu <br /> ed atit�n can be alkalinitYetI at vartou biodegradation ca plical indicator <br /> btorern nate hardness, e aram for to sis of ge°che indicator <br /> Intrinsic 1 carbo of rhes peiectrori acceptor les for anal` eochemical solids, <br /> lee �n the d15tnbution of each rn t The otal isso}ved <br /> �bution venter sa p even d les were also <br /> g of the coxa round monitoring ltnity, <br /> ates C collected g dwater e alka S e collected and <br /> ed <br /> estim ,,pith D I Iigg5 groun to and bicarb rfln Gr+�urid�I sten w us <br /> were <br /> STD, in coir}unctiazr eGember 1 carboy and testa} .fP d ana'Nater samples Pale <br /> during thetD ce Do't to ph°sph° samples f°r all xound <br /> " act site <br /> parameters alyzed Duplicate llcat � 5 and <br /> nitrite, s the dup the sub! iii <br /> eters an d results for <br /> Sul nitrate, d analyse in incliidcd <br /> param total pH'T TPHg, and w►tYi detections oa apical res event <br /> sulfate of the$nI is-t e wells laboratory r Sampling <br /> fax results le for those data and ndwate <br /> analyzed ending aundv ter elevation dwater <br /> pre (A sediment fre s f�,r the most recent gx°" rout' �} <br /> of all g character °tion <br /> to analyze r l mlrieXal rhes ce of��e <br /> t is a sutxiina�`analYtica} rep coaxes �„titb the ex the sample <br /> The reified homes that el solids in n active in the <br /> t s consist ended ediatio erred <br /> appendix ed In Ta►�le eened "� susp biorem deeper sere <br /> to d deep excess <br /> Gontalri er scr iv <br /> � is due, t4 1ike15' intrinsic igher in the f the deeper <br /> both the shallow screened an that there is no htly en rich recharge o levels in the <br /> rev;eve result f°die tes were shg <br /> from b malous total it°n rntnerals DD levcls from axYg ef roundwater through and <br /> Tlie ono the general liven that the, is corning and higha ge passing <br /> >3 ect stte water y lower DQ levelsandrec <br /> distribution of the su 3 e rise in the s}ightl rouri ve ri°t <br /> groundwater at that th area shatlaw g ha <br /> anent an offsite to local acts gTE dwater <br /> wells, It IS app from lorew due s°ll imp both Tpllg and roue soil <br /> screened zone ed Its }5 lave concentration excavates, ltitO actually <br /> s°nee die remaining aver` the recent andiltarticles have <br /> shallow ding cad ar►d tinpactecl sin he results o ped In groundwa soil ent is <br /> biodegrasedding These act sedl cit+ly a <br /> UST,,were reply wells T-Id levels ,pie 5pende 5 the TP'4d highs a d is <br /> any onsite rec sarnPte via likely water <br /> ce the e <br /> Sln detected In ears that tkl roundwater ears 11 is tent <br /> g nd <br /> bMomtoring, it car carried into the g dry for many Yctian and re <br /> roil <br /> after bei gd well cQnstrix <br /> concentrations <br /> 5th damper scree <br /> 0 an artifact of <br />