Water Studies in the Colorado River Basin in Utah
Water Studies in the Colorado River Basin in Utah
The Colorado River Basin covers about 246,000 sq. miles, including parts of Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming and part of Mexico. The river supplies water to 35 million people in the United States and 3 million in Mexico. This webpage has links to stories about Colorado River Basin research done by scientists at the USGS Utah Water Science Center (UT WSC).
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Upper Colorado River Streamflow and Reservoir Contents
These reports summarize monthly data for selected rivers and reservoirs in the the Upper Colorado River Basin.
Lake Powell Coring
In response to the August 5, 2015, Gold King Mine Spill from the Bonita Peak Mining District that resulted in the release of three-million gallons of mine-impacted waters, the Utah Water Science Center, in partnership with the Utah Division of Water Quality, National Park Service, and U.S. Bureau of Reclamation, cored the San Juan and Colorado River deltas in multiple locations in Lake Powell...
Colorado Plateau Regional Groundwater Availability
Study goals This project seeks to quantify the status of groundwater as an integrated resource with surface water in the arid and semiarid region of the Colorado Plateau principal aquifer system. Surface-water resources that originate in this region are over allocated and serve 35 million people, 4.5 million acres of farmland, and are used to generate 12 billion kilowatt hours of electricity in...
Salinity
Studies of Sources and Transport of Dissolved Solids (Salt) in the Colorado River Basin using the Spatially Referenced Regressions on Watershed Attributes (SPARROW) Model The Upper Colorado River Basin (UCRB) encompasses about 112,000 mi2 and discharges more than 6 million tons of dissolved solids (salt) annually to the lower Colorado River Basin. It has been estimated that between 32 and 45...
Baseflow
The Colorado River has been identified as the most overallocated river in the world. Considering predicted future imbalances between water supply and demand and the growing recognition that base flow (a proxy for groundwater discharge to streams) is critical for sustaining flow in streams and rivers, there is a need to develop methods to better quantify present-day base flow across large regions...
Managed Aquifer Recharge
Sand Hollow Reservoir in Washington County, Utah, was completed in March 2002 and is operated for both surface-water storage and managed aquifer recharge via infiltration from surface basin spreading to the underlying Navajo Sandstone. From 2002 through 2014, about 216,000 acre-feet were diverted from the Virgin River to Sand Hollow Reservoir, and about 127,000 acre-feet of water seeped beneath...