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Dissolution of Iron Oxides and Oxyhydroxides in Hydrochloric and Perchloric Acids

Sidhu, P. S., Gilkes, R. J., Cornell, R. M., Posner, A. M., Quirk, J. P.·1981·Clays and Clay Minerals

Abstract

The dissolution of synthetic magnetite, maghemite, hematite, goethite, lepidocrocite, and akaganeite was faster in HCl than in HClO 4. In the presence of H+, the Cl− ion increased the dissolution rate, but the ClO 4− ion had no effect, suggesting that the formation of Fe-Cl surface complexes assists dissolution. The effect of temperature on the initial dissolution rate can be described by the Arrhenius equation, with dissolution rates in the order: lepidocrocite > magnetite > akaganeite > maghemite > hematite > goethite. Activation energies and frequency factors for these minerals are 20.0, 19.0, 16.0, 20.3, 20.9, 22.5 kcal/mole and 5.8 × 10 11, 1.8 × 10 10, 7.4 × 10 7, 5.1 × 10 10, 2.1 × 10 10, 3.0 × 10 11 g Fe dissolved/m 2/hr, respectively. The complete dissolution of magnetite, maghemite, hematite, and goethite is well described by the cube-root law, whereas that of lepidocrocite is not.

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Metadata

Authors
Sidhu, P. S., Gilkes, R. J., Cornell, R. M., Posner, A. M., & Quirk, J. P.
Venue
Clays and Clay Minerals
Published
1981-08
Volume
29
Issue
4
Pages
269-276
ISSN
  • 0009-8604 (ISSN-L)
  • 1552-8367
OpenAlex
W2164954285
Cited by
250
References
0
FWCI
0.53
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Dissolution of Iron Oxides and Oxyhydroxides in Hydrochloric and Perchloric Acids. https://app.cochat.ai/papers/10.1346/ccmn.1981.0290404
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Sidhu, P. S., Gilkes, R. J., Cornell, R. M., Posner, A. M., & Quirk, J. P. (1981). Dissolution of Iron Oxides and Oxyhydroxides in Hydrochloric and Perchloric Acids. Clays and Clay Minerals. https://doi.org/10.1346/ccmn.1981.0290404

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