Iron (II) and Silicate Effects on Mineralization and Immobilzation of Actinides [electronic resource]

Abstract - The unique composition of the Yucca Mountain repository site, which contains large concentrations of silicate in an oxidative environment, has required extensive research into compound formation involving uranium and iron(II) under such conditions. The possibility of uranium leakage from...

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Bibliographic Details
Online Access: Online Access
Corporate Author: Harry Reid Center for Environmental Studies (Researcher)
Format: Government Document Electronic eBook
Language:English
Published: Washington, D.C. : Oak Ridge, Tenn. : United States. Dept. of Energy. Office of Civilian Radioactive Waste Management ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 2006.
Subjects:

MARC

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245 0 0 |a Iron (II) and Silicate Effects on Mineralization and Immobilzation of Actinides  |h [electronic resource] 
260 |a Washington, D.C. :  |b United States. Dept. of Energy. Office of Civilian Radioactive Waste Management ;  |a Oak Ridge, Tenn. :  |b distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy,  |c 2006. 
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500 |a 01/01/2006. 
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500 |a FT. 
500 |a ANS 2006 International High Level Radioactive Waste Management Conference, Las Vegas, NV, April 30th-May 4th. 
500 |a Tyler A. Sullens; Cynthia-May S. Gong; Kenneth R. Szerwinski. 
520 3 |a Abstract - The unique composition of the Yucca Mountain repository site, which contains large concentrations of silicate in an oxidative environment, has required extensive research into compound formation involving uranium and iron(II) under such conditions. The possibility of uranium leakage from within the containment vessels into the near-field ground water, as well as iron leaching from the vessel itself, necessitates study of the individual contributions of these elements for compound formation. By mimicking the known silicate concentration found in surrounding ground water and varying concentrations of both uranyl and iron(II), subsequent precipitation of uranyl silicate phases has shown evidence of iron(II) sorption to the available sites on the mineral surface. The mineralization seems to be driven by the formation of uranyl silicate, in contrast to iron(III)-control of precipitation in the oxidated system. Characterization of this system presented includes ICP-AES analysis as well as preliminary EDAX, XRD, and FT-IR. 
520 0 |a Actinides, Iron (ii), Silicates. 
536 |b FC28-04RW12237. 
650 7 |a X-ray Diffraction.  |2 local. 
650 7 |a Uranium.  |2 local. 
650 7 |a Actinides.  |2 local. 
650 7 |a Radioactive Waste Management.  |2 local. 
650 7 |a Ground Water.  |2 local. 
650 7 |a Precipitation.  |2 local. 
650 7 |a Mineralization.  |2 local. 
650 7 |a Silicates.  |2 local. 
650 7 |a Leaching.  |2 local. 
650 7 |a Containment.  |2 local. 
650 7 |a Sorption.  |2 local. 
650 7 |a Uranyl Silicates.  |2 local. 
650 7 |a Yucca Mountain.  |2 local. 
650 7 |a Iron.  |2 local. 
650 7 |a Management Of Radioactive And Non-radioactive Wastes From Nuclear Facilities.  |2 edbsc. 
710 2 |a Harry Reid Center for Environmental Studies.  |4 res. 
710 1 |a United States.  |b Department of Energy.  |b Office of Civilian Radioactive Waste Management.  |4 spn. 
710 1 |a United States.  |b Department of Energy.  |b Office of Scientific and Technical Information.  |4 dst. 
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