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<br />C,#J <br />N <br />00 <br />00 <br /> <br />((Ii <br /> <br />1 II <br /> <br />!nporalion <br /> <br />QlIorideSlnd <br />",",le50' <br />sodium,maeneslurn <br />akium. Ind <br />potassiumClrried <br />with w.ternpor <br /> <br />I I I <br /> <br />00", <br /> <br />CondtllSition <br />Nitropn.Olnen. <br />ClrtIondioltde <br />dissolved <br /> <br /> <br />. <br /> <br />Precipitation <br /> <br />- <br /> <br />1 <br /> <br /> <br />Tempaf.ryrdentioninmaunl.in <br />arusassoil..ter <br />I. CO2 dissolved in soil, Ca, Mg, N. <br />bitarbonllesadded ta wilt!' <br />2. 504 dmolved in nus where olidllion <br />of sulfides 1$ Ottllrfinl <br />3. Connate w.teror $Oluble compounds 01 <br />m.rinesedim~ts.dded <br /> <br />+-- Outllow10 ocun <br />Clrriesminmlm.tterbiid <br /> <br />+- Subsurface outflow ta otQn <br /> <br />- <br /> <br />! <br /> <br />Runoff <br /> <br /> <br />~, <br /> <br />r <br /> <br /> <br />r <br /> <br />! <br /> <br />! <br /> <br />! <br /> <br />- <br /> <br />I <br />Wlllent <br />- <br />Steplgt <br /> <br />- <br /> <br />I <br /> <br />:::;..0: <br /> <br />1 <br /> <br />I <br /> <br />I <br /> <br />:::::-: <br /> <br />1 <br /> <br />1 <br /> <br />1 <br /> <br />Evlpor.tion <br />Miner.lm.tler <br />rtt.intd in soil <br /> <br />T'.nspirJlion <br />Minenllnlttuwply <br />rebinediasoil.Plrtty <br />carriedoffinCfOP~ <br />t <br />J <br /> <br />1 <br /> <br /> <br />Soil wiler <br />I. C02.dded.fGfmingurbonitatid <br />2. RmlHln cl soil minerals wilh <br />urbonitacidtotormsoluble <br />bicarbonlles <br />3. PrecipitatiGn of colloidal iron. <br />.Iuminum, Ind siliu; of <br />tlrbon.lu 1$ solubility limit <br />isreadM!d <br />4, Cltionmhan,e <br /> <br />--+ <br /> <br />r <br /> <br />D <br />'" <br />I <br />i <br /> <br />! I <br /> <br />-11 <br /> <br /> <br />Ground water <br />I. Calion tlthan,e <br />2. Sulf'lt reduction by .naerobic <br />blcltri'.subslilutin, <br />biurbonatefor tile sulfatt <br /> <br />FIGURE 1 -Geochemical eycle of surface and ground waters, <br /> <br />3 <br /> <br />