Simulation of Natural Iron Oxide Alteration in Soil: Conversion of Synthetic Ferrihydrite to Hematite Without Artificial Dopants, Observed With Magnetic Methods
We present new results on the conversion of pure, undoped synthetic ferrihydrite, wet‐annealed at pH 6.56 and 90°C without stabilizing ligands, to nanophase goethite, hematite, and an intermediate magnetic phase, nanophase maghemite. Our analyses included magnetic field and temperature‐dependent pro...
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Published in | Geochemistry, geophysics, geosystems : G3 Vol. 21; no. 7 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Washington
John Wiley & Sons, Inc
01.07.2020
Wiley |
Subjects | |
Online Access | Get full text |
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