A THERMODYNAMIC MODEL FOR EXTRACTION OF RARE EARTH ELEMENTS (REE) FROM PHOSPHATE-BEARING RESOURCES
In this study, we develop a thermodynamic model to describe interactions of phosporous species with REE and impurities in phosphate rocks. As calcium is the dominant impurity, the decomposition of phosphate rocks in reaction with H3PO4, H2SO4, HCl, and HNO3, will result in the following solution systems: (1) H3PO4—Ca(H2PO4)2, (2) H3PO4—H2SO4—Ca(H2PO4)2, (3) H3PO4—HCl—Ca(H2PO4)2, and (4) H3PO4—HNO3—Ca(H2PO4)2, respectively. Therefore, the interactions of REEs with phosphorous species in the above solution systems are systematically modelled. In the modeling, we use the Pitzer equations for activity coefficient calculations. In this presentation, we will focus on the interactions of REEs with phosphorous species in the first solution system. In addition, as apatite [Ca5(PO4)3(Cl, F, OH)] is an important phase for REEs and a waste-form for actinides in high level nuclear waste disposal, our experimental and modeling studies also include apatite.
Sandia National Laboratories is a multi-mission laboratory operated by National Technology and Engineering Solutions of Sandia, LLC., a wholly owned subsidiary of Honeywell International, Inc., for the U.S. Department of Energy’s National Nuclear Security Administration under contract DE-NA-0003525. This research is funded by an LDRD project (Project Number 222400), and the SFWST programs administered by the Office of Nuclear Energy (NE) of the U.S. Department of Energy. SAND2023-06802A.