Quality of groundwater used for public supply in principal aquifers of the Southwestern U.S.
Tuesday, February 27, 2018: 8:50 a.m.
In 2013, the National Water-Quality Assessment (NAWQA) Project of the U.S. Geological Survey began a sampling effort focused on the quality of groundwater used for public supply in 20 principal aquifers across the Nation. Portions of four of these nationally identified principal aquifers─the Basin and Range basin-fill aquifer, the Basin and Range carbonate-rock aquifer, the Rio Grande aquifer and the High Plains aquifer─are located within the Southwestern U.S. NAWQA sampled 238 public supply wells from these four aquifers during 2013 to 2016. Samples were analyzed for a comprehensive suite of water-quality constituents, including major and trace elements (including hexavalent chromium), nutrients, pesticides, volatile organic compounds (VOCs), radionuclides, microbial indicators, pharmaceuticals, hormones, and groundwater age tracers. No exceedances of human-health benchmarks for drinking water were present in the samples collected for pesticides or VOCs. The most common exceedances frequencies of water-quality benchmarks relative to secondary standards were for salinity-related constituents: 30% of samples had high concentrations of dissolved solids, whereas exceedances of chloride, sulfate, and fluoride, ranged from 8% to 13%. The most common exceedance of a human-health benchmark for drinking water was for arsenic (12%). Exceedances for uranium (4%) and nitrate (0%) were low; these results contrast with previous NAWQA studies of shallow groundwater in these aquifers, where exceedances of human-health benchmarks for constituents such as arsenic, uranium, and nitrate occurred more frequently. Results are being evaluated to assess the relation of groundwater quality with natural and human-related factors. Most constituents that have exceedances of water-quality or human-health benchmarks in the four identified principal aquifers are derived chiefly from geologic sources, and generally are observed at higher concentrations in older, more geochemically evolved groundwater.