期刊
APPLIED GEOCHEMISTRY
卷 23, 期 5, 页码 1094-1100出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.apgeochem.2008.01.004
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The objective of this study was to investigate the removal mechanism of U(VI) from groundwater by magnetite as the main product of anoxic steel corrosion. For this purpose, a systematic sequence of batch experiments was conducted to focus the active role of magnetite in the reduction of U under different conditions. Results indicated that under anoxic conditions U(VI) was sorbed at the magnetite surface, whereas under reducing conditions at different H-2(g) pressures, U was present in tetravalent form as amorphous UO2. (c) 2008 Elsevier Ltd. All rights reserved.
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