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<br /> <br />N <br /> <br />Effects of Irrigation Development <br />on the Interaction of <br />Ground Water and Surface Water <br /> <br /> <br />Nebraska ranks second among the States with respect <br />to the area of irrigated acreage and the quantity of water used <br />for irrigation. The irrigation water is derived from extensive <br />supply systems that use both surface water and ground water <br />(Figure N-l). Hydrologic conditions in different parts of <br />Nebraska provide a number of examples of the broad-scale <br />effects of irrigation development on the interactions of ground <br />water and surface water. As would be expected, irrigation <br />systems based on surface water are always located near <br />streams. In general, these streams are perennial and (or) <br />have significant flow for at least part of the year. In contrast, <br />irrigation systems based on ground water can be located <br />nearly anywhere that has an adequate ground-water <br /> <br />"'" <br /> <br />- <br /> <br />..... <br /> <br />a..ry <br /> <br />'", ',;, .. ~'~.::m <br />.",,,..., <br /> <br />..... <br /> <br /> <br />. .,-,^ <br />.;.~ /:Jj' <br /> <br />, ""I.::it,ir," '",t <br />", --...~,-_. .~. '. <br />. \. ~"<; ,::,', ,;, <br />. ,_' .~.". ":t> <br />'. . -.,. <br /> <br />... <br /> <br />.... <br /> <br />~'; ~ ~ <br /> <br />"'" <br /> <br />_.. <br /> <br />~.'" <br /> <br />~i'Iti:I <br />....,a4.;...~; ;", <br /> <br />.. """ <br />, . <br />71~~~:~ ~~~~"' <br />~,~.;\ ~.~ ,,',' , <br />:~k-.'t-,.,_,..",. <br />~~~,~~,~:;-,~:::,-;,,~_.:::. ":';.':_~! ~ <br />,<')~t~J,? '.-" <br />;,-~::",{/,;;..< ! <br /> <br />:":'~;...:._,-~, ~ <br /> <br />EXPLANATiON <br /> <br />o SurfaCEl-water <br />irrigation project <br /> <br />resource. Areas of significant rise and decline in ground-water <br />levels due to irrigation systems are shown in Figure N-2. <br />Ground-water levels rise in some areas irrigated with surface <br />water and decline in some areas irrigated with ground water. <br />Rises in ground-water levels near streams result in increased <br />ground-water inflow to gaining streams or decreased flow <br />from the stream to ground water for losing streams. In some <br />areas, it is possible that a stream that was losing water before <br />development of irrigation could become a gaining stream <br />following irrigation. This effect of surface-water irrigation prob- <br />ably caused the rises in ground-water levels in areas F and G <br />in south-central Nebraska (Figure N-2). <br /> <br />. <br />, <br />I <br /> <br />. <br /> <br />." <br />.~----- <br />t: "'ji}' <br />. -~ .. Iih>< <br />';"'ir'h' <br />,;~":-,! " ' <br />}:..:""~~, ,:"" <br /> <br />-r;.;f1t1- <br /> <br />o 20 40 MILES <br />I I I <br /> <br />Figure N-1. Nebraska is one of the most extensively irrigated States in the Nation. The irrigation water comes from <br />both ground-water and surface-water sources. Dots are irrigation wells. (Map provided by the University of Nebraska, <br />Conservation and Survey Division.) <br /> <br />58 <br />