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<br />. <br /> <br />. <br /> <br />. <br /> <br />Q()1951 <br /> <br />Operative Areas <br /> <br />The concept of operative areas identifies specific processes and areas where the processes are <br /> <br />operative. Some processes, such as the effects of leakage from the Arkansas River or the Fort Lyon <br /> <br />Canal may be limited to general zones. For instance, the relatively widespread occurrence of areas <br /> <br />where the depth to water is less than 5 feet and the knowledge that increases in river elevations affect <br /> <br />increases in ground-water levels leads to the question "How far-reaching can the effecAts of the river <br />/// (/ <br />be?" The depth to water map shown in figure 3 is a convenient, although generl\k:irrw~sm t(1gener- <br />// ,Y/ -"'...., "",/ ~~'_" -':\, " <br />\. ,\"," , {'-" '" <br />ally evaluate such a question. /""" \/.,~::--:::..,/ <br />\ ~:;"> "-""-"'>- ( (''''''\ \ ~~'\/ <br />The depth to water map (fig. 3) generally delineates the area, cjUdhg ~\~:hiias(\r'ek'ent~riod, <br />/ /' '\ "'~ ,." ~_ - "j '" ",,"'b'''' <br />.' __~__~.,-- \<f~<~;;rv /(::;~-:::,:::;,> <br />where the water table is within 5 feet of the land surface. In an,.e'~anlPJ(~xer~is.e,:Sut5p<;lse that the <br />\ r, "\ ) J 1\:-',,- "-""<=,,,/ <br /> <br />Arkansas River elevation increases 5 feet, compared to CP'tditio~((U::~:~~~imaOf water-level <br />, ' ")" . <br />,/----\ \ ,,/ ~ /') '--,// <br />measurements on which the depth to water map i~J:>~~"Q:'B~~s:d}'lL~~\i~ated average discharge of <br /><, {,) k:~>-~' ( () :--~~~/ <br />100 cubic feet per second during the measuri~g'R€!~> stich arf'~cf~a~e would represent an instanta- <br /> <br />/', \ """-~? //0~_",_~ '\/ <br />neous discharge of about 5,000 cubic fe~~''P~r"Sec\lnd, TI(e'lh;>'\y-duration statistics listed in table 5 indi- <br />/,,~> "',::~' -.) \/ j/ ,/ \ -"",' j / <br /> <br />cate that a daily mean discharge qf; , \ ~gpitud{pT.Qhl!:biy"~ccurs less than 1 percent of the time. <br />"'-, \ ;i;" ',- /, ~\,\/j <br />/ '^"" \ ,\ ,,- ;, <br />Assuming that the ArI\~s~S\~~~t it~~kt to affect its surface elevation in the surrounding aquifer, <br />,~ ''''''-" '\ -,,~/ -~ "", <br />,', '" ~-\'v/ /,-:.,,? _ ""-,) <br />a 5-foot increase in st!l~~~\!~J~ry~\ \~e,t}ire area on the depth to water map that is within 10 feet of <br /> <br />..." ""f // j__';:/ >/ /'->"\""",__.,_" <br />the land surface t6'b~'I!6"nlor'?'~?fe~ above the water table. In the western one-half of the study <br />{""'1 '~'" \,;' ,,'<>' '/ // <br />". ",,/ /" --,,' ',,- ~"",,- / <br />''''''<'" " 'o,,/^ ,"'^_ "> '\ ~ <br />area such a ~h~ryg~)'0~)1~a'y~i~igespread effects; in the eastern one-half of the study area, the effects <br />" ( ,/'<\, '//--; ! <br />would be liJrtile'dlll\?stlt'tptre"lativeIy narrow strip. <br />....' " <br />,,""">', "",,-w,) / <br />This e"e~ci'se illustrates that the Arkansas River has the potential to effect a large part of the study <br />\''''-- _:~:;,' <br /> <br />area. For instance;ln the example, if the land surface being within 5 feet of the water table is the crite- <br /> <br />rion used to evaluate whether or not an area is affected by the river, then the river would influence, <br /> <br />according to the frequency information in table 2, about 65 percent of the study area. <br /> <br />19 <br />