Abstract
The dissolution of uranium dioxide under oxidative alkaline conditions is critically influenced by iron pyrite (FeS2), which is a gangue mineral commonly found in uranium ores. This paper makes an effort in understanding the kinetics of dissolution of UO2 in a co-existing system of UO2 and FeS2 under the lixiviant combination of Na2CO3 and NaHCO3–O2 at elevated temperature and pressure. Dissolution experiments were carried out in a laboratory batch autoclave reactor using synthetic mixtures of minerals consisting of UO2, FeS2 (reactive gangue—varied from 1 to 6 %), silica (inert gangue) and calcite (inert gangue). The kinetic profiles indicated that the rate of dissolution of UO2 increased with initial increase in FeS2 content in the feed and decreased when the FeS2 weight increased beyond 3 %. The dissolution phenomenon was analysed using scanning electron microscopy and X-ray diffraction studies.
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Acknowledgments
The authors convey their sincere thanks to their colleagues in chemical laboratory of Mineral Processing Division and Shri Bhaskar Paul of Material Processing Division of Bhabha Atomic Research Centre for the wet chemical analyses and scanning electron microscopy respectively. They also acknowledge the services of the XRD Laboratory of Atomic Minerals Directorate for Exploration and Research in carrying out XRD analyses. The authors also thank Dr. J.K. Chakravartty, Director, Materials Group, Bhabha Atomic Research Centre for his encouragement during the investigations. The authors are thankful for the valuable suggestions from two anonymous reviewers.
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Anand Rao, K., Sreenivas, T., Vinjamur, M. et al. Kinetics of Alkaline Leaching of UO2 and FeS2 in Co-existing System. Trans Indian Inst Met 69, 23–31 (2016). https://doi.org/10.1007/s12666-015-0615-8
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DOI: https://doi.org/10.1007/s12666-015-0615-8