Solution equilibria of uranyl minerals: Role of the common groundwater ions calcium and carbonate.

ABSTRACT: Understanding the factors that govern aqueous solubility of uranyl minerals is important for predicting uranium mobility in groundwater and for designing effective remediation strategies. The uranyl-containing minerals metaschoepite [UO3?(2H2O)] and uranophane [Ca(UO2)2(SiO3OH)2·5H2O] were synthesized and evaluated in batch solubility experiments conducted in the presence of common groundwater ions: calcium, bicarbonate/carbonate, and dissolved silica. Solid-phase characterization revealed the expected structural and thermogravimetric properties of metaschoepite and uranophane. Metaschoepite solubility in carbonate-free water followed a u-shaped pH dependency with minimum solubility near pH 8.5; uranium concentrations at pH ? 8.5 were approximately equivalent to the reference value for safe drinking water established by the EPA (30??g/L). With increasing bicarbonate/carbonate concentration (1?mM?-?50?mM) the solubility of metaschoepite increased, presumably due to the formation of uranyl-carbonate complexes. However, the experimental concentrations of uranium were lower than concentrations predicted from accepted complexation constants. For uranophane, equilibrium uranium concentrations were < 75??g/L at typical groundwater concentrations of calcium and dissolved silica (pH?>?7). The diversity of uranyl minerals that possibly form in the presence of common groundwater species: Ca-Mg-Na-K-Si-bicarbonate/carbonate-sulfate-chloride, has not been fully explored with respect to understanding potential mineral transformations and impacts on uranium solubility and mobility.

SUBMITTER: Stanley DM 

PROVIDER: S-EPMC7369140 | biostudies-literature | 2019 Sep

REPOSITORIES: biostudies-literature