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Structural Model for Ferrihydrite

Drits, V. A., Sakharov, B. A., Salyn, A. L., Manceau, A.·1993·Clay Minerals

Abstract

The structure of 6-line and 2-line ferrihydrite (Fh) has been reconsidered. X-ray diffraction (XRD) curves were first simulated for the different structural models so far proposed, and it is shown that neither of these corresponds to the actual structure of ferrihydrite. On the basis of agreement between experimental and simulated XRD curves it is shown that Fh is a mixture of three components: (i) Defect-free Fh consisting of anionic ABACA . . . close packing in which Fe atoms occupy only octahedral sites with 50% probability; the hexagonal unit-cell parameters are a = 2-96 Å and c = 9-40 Å, and the space group is P 1c. (ii) Defective Fh in which Ac 1 Bc 2 A and Ab 1 Cb 2 A structural fragments occur with equal probability and alternate completely at random; Fe atoms within each of these fragments have identical ordered distribution with in the hexagonal super-cell with a = 5.26 Å. (iii) Ultradispersed hematite with mean dimension of coherent scattering domains (CSD) of 10-20 Å. The main structural difference between 6-line and 2-line Fh is the size of their CSD which is extremely small for the latter structure. Nearest Fe-Fe distances calculated for this new structural model are very close to those determined by EXAFS spectroscopy on the same samples.

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Metadata

Authors
Drits, V. A., Sakharov, B. A., Salyn, A. L., & Manceau, A.
Venue
Clay Minerals
Published
1993-06
Volume
28
Issue
2
Pages
185-207
ISSN
  • 0009-8558 (ISSN-L)
  • 1471-8030
OpenAlex
W2122697462
Cited by
356
References
0
FWCI
5.27
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Structural Model for Ferrihydrite. https://app.cochat.ai/papers/10.1180/claymin.1993.028.2.02
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Drits, V. A., Sakharov, B. A., Salyn, A. L., & Manceau, A. (1993). Structural Model for Ferrihydrite. Clay Minerals. https://doi.org/10.1180/claymin.1993.028.2.02

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