2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 65-10
Presentation Time: 4:20 PM

SOLUBILITY AND CALORIMETRY STUDIES OF K-ZIPPEITE: DETERMINATION OF STANDARD STATE THERMODYNAMIC PROPERTIES


SHARIFIRONIZI, Melika, Civil and Environmental Engineering and Earth Science, Uni of Notre Dame, 301 Stinson Remick Hall, Notre Dame, IN 46637, BURNS, Peter C., Department of Civil and Environmental Engineering and Earth Sciences, University of Notre Dame, 301 Stinson Remick Hall, Notre Dame, IN 46556, FEIN, Jeremy B., Civil & Environmental Engineering & Earth Sciences, University of Notre Dame, 156 Fitzpatrick Hall, Notre Dame, IN 46556 and SZYMANOWSKI, Jennifer, Civil and Environmental Engineering and Earth Science, Uni of Notre Dame, 301 Stinson Remick Hall, Notre Dame, IN 46556, msharifi@nd.edu

Zippeite is a uranyl sulfate mineral that is widespread in U deposits that contain sulfides and are oxidized, and is a common constituent of mine wastes. The stability of different uranyl mineral phases plays an important role in determining geologic nuclear waste repository performance. In this study, we synthesized K-zippeite, K3(H2O)[(UO2)4(SO4)2O3(OH)], and completed solubility and calorimetric studies. The enthalpy of formation of zippeite was calculated from the enthalpy of dissolution in a high-temperature oxide melt solution calorimeter. Solubility measurements were conducted both from undersaturation and from supersaturation in order to demonstrate and constrain equilibrium. Using the log solubility product that was calculated from the solubility measurements(log Ksp), the standard state Gibbs-free energy was determined at T=297K. The Gibbs free energy of formation of zippeite, coupled with its enthalpy of formation, was then used to calculate the standard entropy of formation.