USE OF RADIUM ISOTOPES TO EVALUATE NATURALLY-OCCURRING URANIUM AND RADIUM SOURCES AND BEHAVIOR IN NEW MEXICO GROUNDWATERS: EXAMPLES FROM THREE SITES
Trends in Ra isotope ratios (224Ra/228Ra and 228Ra/226Ra) provide insights into the sources and mobility of U and Ra in these wells, and can influence decisions about water treatment vs. obtaining alternative water sources to meet drinking water standards. The Glorieta waters are oxic, with variable 228Ra/226Ra values, indicating a variable degree of U enrichment in the aquifer sandstones, while 224Ra/228Ra ratios close to one suggest that Ra is labile, sorbing and desorbing rapidly relative to the half-life of 224Ra (3.6 days). In reducing groundwaters near the Zuni Mountains, U concentrations are low. Ra is low in one well but highly elevated in a nearby well, and 228Ra/226Ra values are very low (<0.25), implying enrichment of U in the aquifer sediments. Although U concentrations were low in reducing groundwaters from the Laguna area, low 228Ra/226Ra values (<0.4) suggest enrichment of U relative to Th in the clastic sedimentary aquifer units. 224Ra/228Ra values are variable but overall close to 1. This study used an innovative low-cost method for 226Ra analyses. Radium was concentrated onto Mn oxide coated fibers and counted via decay products after a 20 day incubation period using an inexpensive radon-in-air detector. This technique could be used for low-cost long-term monitoring of water sources or pilot tests for radium treatment.
Sandia National Laboratories is a multi-program laboratory managed and operated by Sandia Corporation, a wholly owned subsidiary of Lockheed Martin Corporation, for the U.S. Department of Energy's National Nuclear Security Administration under contract DE-AC04-94AL85000.