Laserfiche WebLink
<br />Salinity Control Opportunities <br /> <br />'" <br />UI <br />.... <br />.... <br /> <br />emerges asspringflow where the canyon has penetrated the Redwall and <br />Mauve Umestones below the regional water table, There are many spring <br />openings along two relatively well-defined reaches. A full scale feasibility <br />study of It he project is not planned due to the high capital cost of building <br />the projE!ct and the historical and religious value of the area to the Hopi <br />Indians, <br /> <br />Dirty Devil River Unit <br /> <br />The Dirty Devil River study area was located in Emery and Wayne Counties <br />in southern Utah. The study area included the Muddy Creek, the Fremont <br />and Dirty Devil Rivers, and the tributaries of Muddy Creek, Hanksville Salt <br />Wash, aIld Emery South Salt Wash. The Dirty Devil River drainage <br />contribu$s approximately 150,000 tons of salt each year to the Colorado <br />River. TlJ.e Muddy Creek tributary contributes an average of 86,000 tons of <br />salt annually. No significant sources of salt or potential alternatives were <br />identifieq on the Fremont River or its tributaries, Approximately 28 percent <br />of the Mdddy Creek salt load (24,200 tons per year) comes from springs in <br />HanksvilJe Salt Wash and Emery South Salt Wash, <br /> <br />Reclamation evaluated reducing the salinity of the Dirty Devil and Colorado <br />Rivers by collecting saline spring water in Hanksville Salt Wash and Emery <br />South Salt Wash and disposing of it by deep well injection. This means of <br />disposal would reduce the salt contribution to the Colorado River by <br />20,900 tons annually. The unit was thought not to be cost effective, <br /> <br />Glenwood-Dotsero Springs Unit <br /> <br />Glenwood..Dotsero Springs is located along the Colorado River in Eagle, <br />Garfield, ~nd Mesa Counties in west-central Colorado, The springs are <br />located nElar the town of Glenwood Springs and the rural community of <br />Dotsero. The combined annual discharge of the springs is 25,000 acre-feet <br />of water Which contain about 440,000 tons of salt, About half of the salt <br />contribution comes from 20 surface springs; the remainder enters as seeps <br />and undetiwater springs within the river channel. <br /> <br />Reclamatii>n started its planning investigations in 1980, The most cost- <br />effective plan at the time consisted of collecting both surface and subsurface <br />salt water:at Dotsero and transporting the salt water in a gravity flow pres- <br />sure line tP Glenwood Springs where additional surface and subsurface salt <br />water would be collected and added to the Dotsero salt water, The water <br />would then be piped to evaporation ponds at the Colorado-Utah border, At <br />$126 per ton, this plan could not compete with alternatives available in <br />other unit~. Plans were deferred until a more cost-effective alternative, <br />possibly aIj. industrial use, could be found. A planning report concluding the <br />evaporatiop. pond alternative was completed in February 1986, <br /> <br />B-3 <br /> <br />",,' '., <br /> <br />.,' , <br />,..;, <br />. <br /> <br />4 <br /> <br />, <br />q <br />A <br />'1 <br /> <br />