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The visible and infrared spectral properties of jarosite and alunite

Bishop, J. L.·2005·American Mineralogist

Abstract

The visible and infrared spectral properties of two natural jarosite minerals and a suite of synthetic jarosites and alunite samples are described here. The fundamental stretching and bending vibrations observed in the infrared region for SO 4 2- and OH - are compared with the near-infrared overtones and combinations of these vibrations. Shifts were observed in the SO 4 2- and OH - bands for Al 3+ vs. Fe 3+ at the octahedral sites and K + vs. Na + at the “A„ (frequently monovalent) sites. Crystal-field theory bands were observed for jarosite near 435, 650, and 900.925 nm and were compared to those of iron oxides. Spectral bands near 1.76, 2.17, 2.53, 4.5, 8.10, and 15.24 μm (corresponding to ~5670, 4600, 3970.4150, 2100.2300, 1000.1225, and 420.675 cm -1 , respectively) for alunite and near 0.43, 0.91, 1.85, 2.27, 2.63, 4.9, 8.10, and 15.24 μm (corresponding to ~23 000, 10 990, 5400, 4350.4520, 3800.4150, 1950.2200, 1000.1190, and 440.675 cm -1 , respectively) for jarosite would be most useful for detecting these minerals using remote sensing on Earth or Mars. These minerals are important indicators of alteration processes, and this study contributes toward combined visible/near-infrared and mid-infrared spectral detection of these two alunite-group minerals.

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Metadata

Authors
Bishop, J. L.
Venue
American Mineralogist
Published
2005-07-01
Volume
90
Issue
7
Pages
1100-1107
ISSN
0003-004X (ISSN-L)
OpenAlex
W2004822956
Cited by
245
References
5
FWCI
8.59
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The visible and infrared spectral properties of jarosite and alunite. https://app.cochat.ai/papers/10.2138/am.2005.1700
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Bishop, J. L. (2005). The visible and infrared spectral properties of jarosite and alunite. American Mineralogist. https://doi.org/10.2138/am.2005.1700

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