Stephanie J. Moore1, R.L. Bassett, Ph.D.
2, Beiling Liu, Ph.D.
3, Christopher P. Wolf
1 and Dale Doremus
4, (1)Daniel B. Stephens & Associates Inc., (2)Geochemical Technologies Corp, (3)New Mexico Interstate Stream Commission, (4)New Mexico Environment Dept.
Water quality in the Lower Rio Grande (LRG) Valley (San Marcial, NM, to El Paso, TX) has been extensively studied and observed salinization has been attributed to various mechanisms, including agricultural practices and inflow of deep saline and geothermal groundwater. We evaluate historical chloride and streamflow data (1905 to 2003), review previous investigations, and consider the most recent hydrogeologic interpretations of the study area (including Palomas, Mesilla, and Jornada del Muerto Basins). Based on the conceptual model of the system, we identified the various sources of water and, therefore, salinity to the LRG and designed a sampling plan to characterize these sources. Finally, we conducted two synoptic sampling events to test for geochemical and environmental tracers. Results of geochemical and isotopic analyses and a chloride mass balance assessment confirm that natural sources of salinity are the principal contributors to the salinization of the Rio Grande. Specifically, a combination of geothermal and deep saline groundwater inflow to the Rio Grande is primarily responsible for the observed salinization of the LRG. These analyses indicate that it is not possible to reproduce the observed salinization by evapotranspiration and agricultural processes alone.
The 2007 Ground Water Summit