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<br />.... <br />l\) <br /> <br />---.-.... ~- -'---"--J' -- - --.--r---- ------ <br />wide problem that is becoming important to users of Colorado River <br />water. Increased concern and a Sense of urgency co halt the salinity <br />increase have been e~pressed by Federal and State water resource <br />agencies. <br /> <br />Data collected to the present time indicates that approximately two. <br />t~irJ5 of tric tot~l salt ~urci~n at lioovcr Dam comeS iroln natural <br />sourceS. Of this load approximately 82 percent comes from diffuse <br />nourccs such as overland runoff and ground water inflow, and about <br />IS percent originates from point sources including mineral springs, <br />seeps, and abandoned wells. <br /> <br />The larGest point source contributors of dissolved solids to the <br />Upper Colorado River arc in the reach of the river between the mouth <br />of the Roarin3 Fork River at Glenwood Springs and the mouth of the <br />Eagle River near Dotsero. These contributions arc from thermal <br />sp~ing5 rising in or nea~ the bed of the riVer and irom ground vater <br />entcrinll tilts reach of the river. Inflow-outflow I:IeasurementS indicate <br />this reach of the river contributes approximately 25,000 acre-feet of <br />water containing over 500,000 tons of dissolved solids annually. <br /> <br /> <br />.-....., <br /> <br />"""""- <br /> <br />~ <br /> <br />~~~- <br /> <br />PIZ44-4Z7-l4~A Colorado River ~ater Quality Improvement Program-Colorado <br />Hot I:I"ncral springs in the Dotsero area: View showing the flow frolD <br />sampling stations dot ZO, 30 and 40. <br />USSR Piloto by V. Jer:;ley February 22, 1973 <br /> <br />I <br />'.'1 <br />u 1 <br />::.1 <br />",:i,'1 <br />:,)1 <br />';~:~':I <br /> <br />",1 <br />>j <br />I <br />I <br />I <br />'I <br />...1 <br />"1 <br />I <br /> <br />".~-'-~": <br /> <br />f~.;~::::.; <br />>1) <br />