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Ferrihydrite: Surface Structure and Its Effects on Phase Transformation

Zhao, Jianmin, Huggins, Frank E., Feng, Zhen, Huffman, Gerald P.·1994·Clays and Clay Minerals

Abstract

X-ray absorption fine structure (XAFS) spectra were collected on a series of ferrihydrite samples prepared over a range of precipitation and drying conditions. Analysis of the XAFS pre-edge structures shows clear evidence of the presence of lower coordination sites in the material. These sites, which are most likely tetrahedral, are believed to be at the surface and become coordination unsaturated (CUS) after dehydroxylation. With chemisorbed water molecules, the CUS sites become the crystal growth sites responsible for the phase transformation of ferrihydrite to hematite at low temperatures. On the other hand, when impurity anions such as SiO 4−4 are present in the precipitation solution, the CUS sites may instead absorb the impurity anions, thereby blocking the crystal growth sites and inhibiting the formation of hematite.

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Metadata

Authors
Zhao, J., Huggins, F. E., Feng, Z., & Huffman, G. P.
Venue
Clays and Clay Minerals
Published
1994-12
Volume
42
Issue
6
Pages
737-746
ISSN
  • 0009-8604 (ISSN-L)
  • 1552-8367
OpenAlex
W1951468408
Cited by
226
References
0
FWCI
3.37
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Ferrihydrite: Surface Structure and Its Effects on Phase Transformation. https://app.cochat.ai/papers/10.1346/ccmn.1994.0420610
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Zhao, J., Huggins, F. E., Feng, Z., & Huffman, G. P. (1994). Ferrihydrite: Surface Structure and Its Effects on Phase Transformation. Clays and Clay Minerals. https://doi.org/10.1346/ccmn.1994.0420610

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