The role of baseflow in dissolved solids delivery to streams in the Upper Colorado River Basin

• Published in: Hydrological processes 2017-12, Vol.31 (26), p.4705-4718
• Main Authors: Rumsey, Christine A., Miller, Matthew P., Schwarz, Gregory E., Hirsch, Robert M., Susong, David D.
• Format: Article
• Language: English
• Subjects: baseflow; Beverage industry; Climate change; Creeks & streams; Discharge; Dissolved solids; Groundwater; groundwater discharge to streams; Irrigation; Landscape; Loads (forces); Measuring instruments; Mitigation; Regression analysis; River basins; Rivers; Salinity; Salinity effects; Stream discharge; Stream flow; Streams; Total dissolved solids; Transport processes; Trend analysis; Trends; Upper Colorado River Basin; Water consumption; water quality; Water users
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.11390

Salinity has a major effect on water users in the Colorado River Basin, estimated to cause almost $300 million per year in economic damages. The Colorado River Basin Salinity Control Program implements and manages projects to reduce salinity loads, investing millions of dollars per year in irrigation upgrades, canal projects, and other mitigation strategies. To inform and improve mitigation efforts, there is a need to better understand sources of salinity to streams and how salinity has changed over time. This study explores salinity in the baseflow fraction of streamflow, assessing whether groundwater is a significant contributor of dissolved solids to streams in the Upper Colorado River Basin (UCRB). Chemical hydrograph separation was used to estimate baseflow discharge and baseflow dissolved solids loads at stream gages (n = 69) across the UCRB. On average, it is estimated that 89% of dissolved solids loads originate from the baseflow fraction of streamflow, indicating that subsurface transport processes play a dominant role in delivering dissolved solids to streams in the UCRB. A statistical trend analysis using weighted regressions on time, discharge, and season was used to evaluate changes in baseflow dissolved solids loads in streams (n = 27) from 1986 to 2011. Decreasing trends in baseflow dissolved solids loads were observed at 63% of streams. At the three most downstream sites, Green River at Green River, UT, Colorado River at Cisco, UT, and the San Juan River near Bluff, UT, baseflow dissolved solids loads decreased by a combined 823,000 metric tons (mT), which is approximately 69% of projected basin‐scale decreases in total dissolved solids loads as a result of salinity control efforts. Decreasing trends in baseflow dissolved solids loads suggest that salinity mitigation projects, landscape changes, and/or climate are reducing dissolved solids transported to streams through the subsurface. Notably, the pace and extent of decreases in baseflow dissolved solids loads declined during the most recent decade; average decreasing loads during the 2000s (28,200 mT) were only 54% of average decreasing loads in the 1990s (51,700 mT).