Uranium Co-Precipitation with Iron Oxide Minerals

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In oxidizing environments, the toxic and radioactive element uranium is most soluble and mobile in the hexavalent oxidation state. These processes also affect the biological availability of U(VI) species toward reduction and precipitation as the less soluble U(IV) species by metal-reducing bacteria. The results provide compelling evidence of U incorporation within the hematite structure.

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Duff, M.C. May 22, 2002.

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This article is part of the collection entitled: Office of Scientific & Technical Information Technical Reports and was provided by UNT Libraries Government Documents Department to Digital Library, a digital repository hosted by the UNT Libraries. It has been viewed 51 times . More information about this article can be viewed below.

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Description

In oxidizing environments, the toxic and radioactive element uranium is most soluble and mobile in the hexavalent oxidation state. These processes also affect the biological availability of U(VI) species toward reduction and precipitation as the less soluble U(IV) species by metal-reducing bacteria. The results provide compelling evidence of U incorporation within the hematite structure.

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  • Journal Name: Geochimica et Cosmochimica Acta

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  • Report No.: WSRC-MS-2002-00322
  • Grant Number: AC09-96SR18500
  • Office of Scientific & Technical Information Report Number: 799444
  • Archival Resource Key: ark:/67531/metadc736199

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Creation Date

  • May 22, 2002

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  • Oct. 19, 2015, 7:39 p.m.

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  • May 5, 2016, 5:57 p.m.

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Duff, M.C. Uranium Co-Precipitation with Iron Oxide Minerals, article, May 22, 2002; South Carolina. (digital.library.unt.edu/ark:/67531/metadc736199/: accessed August 18, 2017), University of North Texas Libraries, Digital Library, digital.library.unt.edu; crediting UNT Libraries Government Documents Department.