<br />,.-," C 1'\,
<br />(.,)v.'
<br />
<br />Stage 11, which began in 1986, involved lining about
<br />40 mi of canals and replacing about 320 mi of laterals
<br />with underground pipeline. When Stage II is com-
<br />pleted, the estimated decrease in salt load to the
<br />Colorado River would be ] 51 ,000 tons/yr (Bureau
<br />of Reclamation, 1985a, 1986). By early 1994, about
<br />two-thirds of Stage II was completed.
<br />The USDA on-farm salinity-control program
<br />was started in 1979 in the Grand Valley and has contin-
<br />ued through 1994. Once completed, the estimated
<br />decrease in dissolved-solids loading attributed to the
<br />on-farm improvements would be 132,000 tonslyr for
<br />the Grand Valley Unit (Hedlund, 1994). Approxi-
<br />mately 50 percent of the USDA salinity program in the
<br />Grand Valley was completed by early 1994 (Emory
<br />Johnson, Natural Resources Conservation Service, oral
<br />commun., ]994).
<br />
<br />Lower Gunnison Basin Unit
<br />
<br />The Lower Gunnison Basin Unit consists of the
<br />Gunnsion River Basin downstream from Blue Mesa
<br />Reservoir, including the North Fork Basin (fig. I).
<br />The primary irrigation project in this area is the
<br />Uncompahgre Project (fig. I), which supplies water
<br />for irrigation of about 86,000 acres. The BOR salinity
<br />program in the Lower Gunnison Basin Unit was
<br />focused only on the Uncompahgre Project. The BOR
<br />(1982,1984) estimated that about 360,000 tonslyr
<br />of salt came from irrigation-induced sources in
<br />the Uncompahgre Project. The estimated annual
<br />dissolved-solids loading from the entire Lower
<br />Gunnison Basin Unit was about 640,000 tons (Bureau
<br />of Reclamation, 1984). The BOR's Winter Water
<br />Replacement Program was designed to replace the
<br />practice of using winter flows in canals and laterals
<br />for livestock watering by expanding the existing rural
<br />domestic water systems in the Uncompahgre Project
<br />(Bureau of Reclamation, ] 987). The replacement pro-
<br />gram was estimated to decrease the annual dissolved-
<br />solids loading from this area by 74,000 tons. Construc-
<br />tion of the Winter Water Replacement Program began
<br />in 1990 and, by late 1994, was about 95 percent com-
<br />pleted (D.W. Crabtree, Bureau of Reclamation, oral
<br />commun., 1994).
<br />Another salinity-control feature planned for the
<br />Lower Gunnison Basin Unit is the East Side Lateral
<br />Program, which is planned to replace about 188 mi
<br />of laterals and 7 mi of small canals on the east side
<br />
<br />of the Uncompahgre Project with underground pipe-
<br />line (Bureau of Reclamation, 1994). That program
<br />would decrease dissolved-solids loading from the
<br />Uncompahgre Project by about 64,000 tons/yr. The
<br />East Side Lateral Program was scheduled to begin
<br />in 1995, but presently (1995) has been deferred
<br />(U.S. Department of the Interior, 1995).
<br />
<br />The total irrigated area in the Lower Gunnison
<br />Basin Unit that was studied by the USDA for their
<br />salinity-control work is 171,000 acres, which includes
<br />the Uncompahgre Project. Once completed, the USDA
<br />on-farm improvements were estimated to decrease
<br />dissolved-solids loading from the Lower Gunnison
<br />Basin Unit by about 166,000 tonslyr (Hedlund, 1994).
<br />The USDA on-farm improvements were initiated in
<br />1988 in the Lower Gunnison Basin Unit.
<br />
<br />Meeker Dome Unit
<br />
<br />Meeker Dome is a local uplift located east
<br />of Meeker in the White River Basin (fig. 2). The
<br />White River is a tributary of the Green River, which is
<br />tri butary to the Colorado River. The Meeker Dome
<br />Unit was a BOR project that consisted of plugging
<br />three abandoned oil wells drilled in Meeker Dome.
<br />The wells provided conduits for the vertical move-
<br />ment of saline, deep ground water into shallow
<br />aqui fers, which then discharged into the White River
<br />(CH2M Hill, ] 979, 1982). The purpose of the well
<br />plugging was to decrease discharge of the saline
<br />ground water into the White River. One well was
<br />plugged in December 1980; the other two wells were
<br />plugged by June 1981. A post-project study by
<br />CH2M Hill (1982) reported significant decreases
<br />in chloride loading with measurable decreases in
<br />dissolved-solids loading from Meeker Dome. Also,
<br />seeps and springs dried up, and water levels in observa-
<br />tion wells decreased after the wells were plugged.
<br />Detailed monitoring activities ended in 1984 and, in a
<br />concluding study, the BOR (l985b) estimated that
<br />about 19,000 tonslyr of salt was removed from the
<br />White River by the Meeker Dome Unit well plugging.
<br />The saline ground water had high chloride and sodium
<br />concentrations; the BOR (I 985b) reported marked
<br />decreases in concentrations of those constituents in the
<br />river after the well plugging.
<br />
<br />6 Trend Analysis 0' Selected Water-Ouality Data Associated With SBllnlty-Control Projects In the Grand Valley.
<br />In the Lower GunnIson River Basin, and at Meeker Dome. Western Colorado
<br />
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