Effects of the Paradox Valley Unit on Dissolved Solids, Sodium, and Chloride in the Dolores River Ne

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Effects of the Paradox Valley Unit on Dissolved Solids, Sodium, and Chloride in the Dolores River Near Bedrock, Colorado, Etc., U.S. Geological Survey, WRIR 00-4011, July 2000

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Published : 2000
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Number of Pages : 8 Pages
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Results Effects of the Paradox Valley Unit on Dissolved Solids, Sodium, and Chloride in the Dolores River Near Bedrock, Colorado, Etc., U.S. Geological Survey, WRIR 00-4011, July 2000

Effects of the Paradox Valley Unit on dissolved solids, sodium, and - During 1999, a study was conducted by the Geological Survey (USGS) in cooperation with the Bureau of Reclamation to evaluate the effect of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River downstream from the Paradox Valley Unit. This report describes this evaluation and presents the results from this study
USGS Water-Resources Investigations Report 00-4011: Effects of the - During 1999, a study was conducted by the Geological Survey (USGS) in cooperation with the Bureau of Reclamation to evaluate the effect of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River downstream from the Paradox Valley Unit. This report describes this evaluation and presents the results from this
PDF This is the Title for Fact SheetEffect of the Paradox Valley Unit on - of the Paradox Valley Unit reduced the dissolved-solids load to the Dolores River by about 32 percent, the dissolved-sodium load by about 36 percent, and the dissolved-chloride load by about 37 percent. Since 1998, BOR modified operation of the Paradox Valley Unit to optimize interception of brine flowing into the Dolores River. Early in 2002, BOR
Effects of the Paradox Valley Unit on dissolved solids, sodium, and - The Resource Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98, [by Kenneth R. Watts] ; prepared in cooperation with the Bureau of Reclamation
Effect of the Paradox Valley Unit on the dissolved-solids load of the - Discharge of brine with an average dissolved-solids concentration of about 256,000 milligrams per liter from alluvium in Paradox Valley, a collapsed salt anticline, substantially increases the dissolved-solids load of the Dolores River. In 1996, the Bureau of Reclamation began operation of the Paradox Valley Unit, a series of brine-withdrawal wells completed in alluvium along the Dolores River
Ionic Strength | US EPA - Chafin DT (2003) Effect of the Paradox Valley Unit on the Dissolved Solids Load of the Dolores River near Bedrock, Colorado, 1988-2001. Geological Survey, Grand Junction CO. Water Resources Investigation Report 02-4275
Effects of the Paradox Valley Unit on dissolved solids, sodium, and - Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98 by Kenneth R. Watts, 2000, Department of the Interior, Geological Survey edition, in English
Holdings: Effect of the Paradox Valley Unit on the dissolved-solids - Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98 / by: Watts, Kenneth R. Published: (2000) Dolores River instream flow assessment : project report / Published: (1990)
Paradox Valley Unit | Upper Colorado Basin | Bureau of Reclamation - The Paradox Valley Unit was constructed to assist in meeting the objectives and standards of the Federal Water Pollution Control Act of 1948 ( 80-845) and the Colorado River Basin Salinity Control Act of 1974, as amended and supplemented ( 93-320). The Salinity Control Act authorizes the construction, operations, and maintenance of
Effect of the Paradox Valley Unit on the dissolved-solids load of the - Discharge of brine with an average dissolvedsolids concentration of about 256,000 milligrams per liter from alluvium in Paradox Valley, a collapsed salt anticline, substantially increases the dissolved-solids load of the Dolores River. In 1996, the Bureau of Reclamation began operation of the Paradox Valley Unit, a series of brine-withdrawal wells completed in alluvium along the Dolores River
Effect of the Paradox Valley Unit on the dissolved-solids load of the - Effect of the Paradox Valley Unit on the dissolved-solids load of the Dolores River near Bedrock, Colorado, 1988-2001 by Daniel T. Chafin, 2003, Dept. of the Interior, Geological Survey edition, in English
Figure 5 from Effect of the Paradox Valley Unit on the dissolved-solids - Figure 5. Daily dissolved-solids load at gaging stations 09169500 (upstream) and 09171100 (downstream), January 1988-September 2001. - "Effect of the Paradox Valley Unit on the dissolved-solids load of the Dolores River near Bedrock, Colorado, 1988-2001"
Effects of the Paradox Valley Unit on dissolved solids ... - WorldCat - Get this from a library! Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98. [Kenneth R Watts; United States. Bureau of Reclamation.; Geological Survey ()]
Effect of the Paradox Valley Unit on the dissolved-solids load of the - Author Chafin, Daniel T. Title Effect of the Paradox Valley Unit on the dissolved-solids load of the Dolores River near Bedrock, Colorado, 1988-2001 / by Daniel T. Chafin ; prepared in cooperation with the Bureau of Reclamation
Effect of the Paradox Valley Unit on the dissolved-solids load of the - Discharge of brine with an average dissolved-solids concentration of about 256,000 milligrams per liter from alluvium in Paradox Valley, a collapsed salt anticline, substantially increases the dissolved-solids load of the Dolores River. In 1996, the Bureau of Reclamation began operation of the Paradox Valley Unit, a series of brine-withdrawal wells completed in alluvium along the Dolores River and
Estimation of salt loads for the Dolores River in the Paradox Valley - Regression models that relate total dissolved solids (TDS) concentrations to specific conductance were used to estimate salt loads for two sites on the Dolores River in the Paradox Valley in western Colorado. The salt-load estimates will be used by the Bureau of Reclamation to evaluate salt loading to the river coming from the Paradox Valley and the effect of the Paradox Valley Unit (PVU), a
Holdings: Effects of the Paradox Valley Unit on dissolved solids - Effect of the Paradox Valley Unit on the dissolved-solids load of the Dolores River near Bedrock, Colorado, 1988-2001 / by: Chafin, Daniel T. Published: (2003) Controls on spatial and temporal variations of brine discharge to the Dolores River in the Paradox Valley, Colorado, 2016-18 / by: Mast, M. Alisa Published: (2019)
Effect of The Paradox Valley Unit on Dissolved-solids Load of The - Daily dissolved-solids load of brine withdrawn by the Paradox Valley Unit (fig. 4) was estimated from monthly brine-withdrawal volumes (Andrew Nicholas, Bureau of Reclamation, written commun., 2000) and the average dissolved-solids concentration for brine (256,000 mg/L, based on samples collected from brine-withdrawal wells in December 1997
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Paradox Valley Total Dissolved Solids (TDS) Regression - During 1999, a study was conducted by the Geological Survey (USGS) in cooperation with the Bureau of Reclamation to evaluate the effect of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River downstream from the Paradox Valley Unit
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EFFECT OF THE PARADOX VALLEY UNIT ON DISSOLVED-SOLIDS ... - USGS - EFFECT OF THE PARADOX VALLEY UNIT ON DISSOLVED-SOLIDS LOAD OF THE DOLORES RIVER SUMMARY REFERENCES CITED Abstract Discharge of brine with an average dissolved-solids concentration of about 256,000 milligrams per liter from alluvium in Paradox Valley, a collapsed salt anticline, substantially increases the dissolved-solids load of the Dolores River
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Effects of the Paradox Valley Unit on dissolved solids - Title: Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98 Author: Kenneth R Watts; United States. Bureau of Reclamation; Geological Survey () Publisher: Grand Junction, CO : Dept. of the Interior, Geological Survey, [2000] OCLC:45005528
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Effects of the Paradox Valley Unit on dissolved solids - An edition of Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98 (2000) Effects of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River near Bedrock, Colorado, water years 1988-98
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- Watts (2000) estimated that operation of the Paradox Valley Unit reduced the dissolved- solids load to the Dolores River by about 32 percent, the dissolved-sodium load by about 36 percent, and the dissolved-chloride load by about 37 percent
- Watts (2000) estimated that operation of the Paradox Valley Unit reduced the dissolved- solids load to the Dolores River by about 32 percent, the dissolved-sodium load by about 36 percent, and the dissolved-chloride load by about 37 percent
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Effects of the Paradox Valley Unit on dissolved solids - December 7, 2010. During 1999, a study was conducted by the Geological Survey (USGS) in cooperation with the Bureau of Reclamation to evaluate the effect of the Paradox Valley Unit on dissolved solids, sodium, and chloride in the Dolores River downstream from the Paradox Valley Unit
Effect of the Paradox Valley Unit on the dissolved-solids - Discharge of brine with an average dissolved-solids concentration of about 256,000 milligrams per liter from alluvium in Paradox Valley, a collapsed salt anticline, substantially increases the dissolved-solids load of the Dolores River. In 1996, the Bureau of Reclamation began operation of the Paradox Valley Unit, a series of brine-withdrawal