Fe(II) reduction of pyrolusite (β-MnO2) and secondary mineral evolution
Abstract Iron (Fe) and manganese (Mn) are the two most common redox-active elements in the Earth’s crust and are well known to influence mineral formation and dissolution, trace metal sequestration, and contaminant transformations in soils and sediments. Here, we characterized the reaction of aqueou...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
BMC
2017-12-01
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| Series: | Geochemical Transactions |
| Subjects: | |
| Online Access: | http://link.springer.com/article/10.1186/s12932-017-0045-0 |