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<br />- <br /> <br />~ <br /> <br />:11 <br />1 <br /> <br />( 'I" J ' <br />~~_ __~ pt\.",~:" ~L .~~_:'_ _ <br /> <br />_""_"__b~_ '.....___ <br />_-.: ,.~!'.Yz~ " _::}~;it - ~.;:~--.... <br />,~"'" -- <br /> <br /> <br />Ground water (above)~Where shallow water <br />tables develop as a result of deep percolation <br />of excess water, evaporation directlv from <br />the soil surface can cause salt to accumulate <br />on the surface as in this irrigated field near <br />Grand Junction, Colorado. <br /> <br />St6ZvO <br /> <br />an IFlFlIQ~TECI L~nCl:, <br /> <br />UJMEFlE CIa S~L TS camE FFlam? <br /> <br /> <br />The earth's crust <br />(Ieft)- The original source <br />of salts is in rock of the <br />earth;s crust and salts <br />deposi fed eons ago as the <br />earth's crust was reshaped. <br /> <br />I rrigation water <br />(right)-AII irrigation <br />lNaters contain salts. Plants <br />take up the water and <br />leave most of the salts <br />behind. Weathering of soil <br />material adds more salt to <br />the soil. Water passing <br />through the roo t zone <br />carries some of the <br />accumulated salts with it. <br /> <br />I II <br />;p <br /> <br />'I <br /> <br />~ <br /> <br />D <br /> <br />fr~~J%Y <br />i{ ~ ~..' <br /> <br />III <br /> <br />;, <br />~";"""'''~:''''~ <br />nm~~-: :"""..", . -":~ "~. <br />.}~.'n"',. <br />'" .. ',' ",.",~t " <br />"""~'r'" <br />- .. -~ ' ~.. <br />- "'Y\.' ...... \",," <br />.,../~'~.~~. "?L>._."" <br />:"~~1<,_i',1--',~~~;,> '. <br />tt~";~'~'.)',. ,_ (~:..': <br /> <br /> <br />Much of the water can be removed by flow <br />into tile drains... <br /> <br />... and/or open ditch drains. <br />