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Geochemistry: Exploration, Environment, Analysis; 2003; v. 3; issue.3; p. 219-228;
DOI: 10.1144/1467-7873/03-001
© 2003 Geological Society of London

Original Article

Spectral reflectance properties (0.4–2.5 µm) of secondary Fe-oxide, Fe-hydroxide, and Fe-sulphate-hydrate minerals associated with sulphide-bearing mine wastes

J.K. Crowley1, D.E. Williams2, J.M. Hammarstrom1, N. Piatak1, I-Ming Chou1 & J.C. Mars1

1 U.S. Geological Survey, MS 954, Reston, VA 20192, USA (e-mail: jcrowley@usgs.gov)
2 Environmental Protection Agency, MS 555, Reston, VA 20192, USA

Diffuse reflectance spectra of 15 mineral species commonly associated with sulphide-bearing mine wastes show diagnostic absorption bands related to electronic processes involving ferric and/or ferrous iron, and to vibrational processes involving water and hydroxyl. Many of these absorption bands are relatively broad and overlapping; however, spectral analysis methods, including continuum removal and derivative analysis, permit most of the minerals to be distinguished. Key spectral differences between the minerals are illustrated in a series of plots showing major absorption band centres and other spectral feature positions. Because secondary iron minerals are sensitive indicators of pH, Eh, relative humidity, and other environmental conditions, spectral mapping of mineral distributions promises to have important application to mine waste remediation studies.

Key Words: Spectral reflectance • mine wastes • iron sulphates • iron oxides • remote sensing




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T. F. McConachy, K. Yang, M. Boni, and N. J. Evans
Spectral reflectance: preliminary data on a new technique with potential for non-sulphide base metal exploration
Geochemistry: Exploration, Environment, Analysis, 2007; 7: 139 - 151.
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