Redox behavior of magnetite in the environment: moving towards a semiconductor model
Magnetite (Fe3O4) is a commonly found in the environment and can form via several pathways, including biotic and abiotic reduction of Fe3+ oxides and the oxidation of Fe2+ and Fe0. Despite extensive research, the redox behavior of magnetite is poorly understood. In previous work, the extent and kine...
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| Format: | Others |
| Language: | English |
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University of Iowa
2009
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| Online Access: | https://ir.uiowa.edu/etd/365 https://ir.uiowa.edu/cgi/viewcontent.cgi?article=1550&context=etd |