In this article, we will thoroughly explore the impact of Uranyl carbonate on our lives. From its origins to its relevance today, Uranyl carbonate has become a topic of great interest to researchers, academics and the general public. Over the years, Uranyl carbonate has generated debates, discussions and different perspectives that have enriched our understanding of this phenomenon. Through this comprehensive analysis, we will seek to shed light on the various aspects of Uranyl carbonate and how it has shaped our lives on different levels. This article will be a complete guide for those who wish to delve into the fascinating world of Uranyl carbonate and understand its importance in our contemporary society.
Uranyl carbonate refers to the inorganic compound with the formula UO2CO3. Also known by its mineral name rutherfordine, this material consists of uranyl (UO2+2) and carbonate (CO2−3). Like most uranyl salts, the compound is a polymeric, each uranium(VI) center being bonded to eight oxygen atoms.[1] Hydrolysis products of rutherfordine are also found in both the mineral and organic fractions of coal and its fly ash and is the main component of uranium in mine tailing seepage water.[2]
Uranyl carbonates as a class of materials
Many uranyl carbonates exist, rutherfordine being the simplest stoichiometry. Most uranyl carbonates contain additional components including water and diverse anions and cations.[3]
A common method for concentrating uranium from a solution uses solutions of uranyl carbonates, which are passed through a resin bed where the complex ions are transferred to the resin by ion exchange with a negative ion like chloride. After build-up of the uranium complex on the resin, the uranium is eluted with a salt solution and the uranium is precipitated in another process.[citation needed]
^Finch, R. J.; Cooper, M. A.; Hawthorne, F. C.; Ewing, R. C. (1999). "Refinement of the Crystal Structure of Rutherfordine". The Canadian Mineralogist. 37 (4): 929–938.
^Ivanovich, M.; Fröhlich, K.; Hendry, M.J. (1991). "Uranium-series radionuclides in fluids and solids, Milk River aquifer, Alberta, Canada". Applied Geochemistry. 6 (4): 405–418. Bibcode:1991ApGC....6..405I. doi:10.1016/0883-2927(91)90040-V.
^Amayri, Samer; Reich, Tobias; Arnold, Thuro; Geipel, Gerhard; Bernhard, Gert (2005). "Spectroscopic Characterization of Alkaline Earth Uranyl Carbonates". Journal of Solid State Chemistry. 178 (2): 567–577. Bibcode:2005JSSCh.178..567A. doi:10.1016/j.jssc.2004.07.050.
"Ion-exchange". U.S. Nuclear Regulatory Commission. 6 October 2011. Retrieved 22 November 2011.
Flury, Markus; Harsh, James B. (2000). "Remediation of Uranium Contaminated Mine Waste"(PDF). State of Washington Water Research Center Report WRR-04. State of Washington Water Research Center. Archived from the original(PDF) on 3 October 2011. Retrieved 22 November 2011.