Abstract
Boltwoodite and uranophane are uranyl silicates common in oxidized zones of uranium ore deposits. An understanding of processes that impact uranium transport in the environment, especially pertaining to the distribution of uranium between solid phases and aqueous solutions, ultimately requires determination of thermodynamic parameters for such crystalline materials. We measured formation enthalpies of synthetic boltwoodites, K(UO2)(HSiO4)·H2O and Na(UO2)(HSiO4)·H2O, and uranophane, Ca(UO2)2(HSiO4)2·5H2O, by high temperature oxide melt solution calorimetry. We also studied the aqueous solubility of these phases from both saturated and undersaturated conditions at a variety of pH. The combined data permit the determination of standard enthalpies, entropies and Gibbs free energies of formation for each phase and analysis of its potential geological impact from a thermodynamic point of view.
| Original language | English |
|---|---|
| Pages (from-to) | 5269-5282 |
| Number of pages | 14 |
| Journal | Geochimica et Cosmochimica Acta |
| Volume | 75 |
| Issue number | 18 |
| DOIs | |
| State | Published - Sep 15 2011 |
| Externally published | Yes |
Funding
This material is based upon work supported as part of the Materials Science of Actinides, an Energy Frontier Research Center funded by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences under Award Number DE-SC0001089. Funding for the beginning stages of this project (prior to EFRC) was provided by a U.S. Department of Energy, Office of Science and Technology and International (OST&I) grant under the Source Term Thrust program.
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