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Baseline Studies of the Clay Minerals Society Source Clays: Infrared Methods

Published online by Cambridge University Press:  28 February 2024

Jana Madejová  and
Peter Komadel
Jana Madejová*
Affiliation:
Institute of Inorganic Chemistry, Slovak Academy of Sciences, SK-842 36 Bratislava, Slovakia
Peter Komadel
Affiliation:
Institute of Inorganic Chemistry, Slovak Academy of Sciences, SK-842 36 Bratislava, Slovakia
*
E-mail of corresponding author: uachjmad@savba.sk
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Infrared (IR) spectroscopy has a long and successful history as an analytical technique and is used extensively (McKelvy et al., 1996; Stuart, 1996). It is mainly a complementary method to X-ray diffraction (XRD) and other methods used to investigate clays and clay minerals. It is an economical, rapid and common technique because a spectrum can be obtained in a few minutes and the instruments are sufficiently inexpensive as to be available in many laboratories. An IR spectrum can serve as a fingerprint for mineral identification, but it can also give unique information about the mineral structure, including the family of minerals to which the specimen belongs and the degree of regularity within the structure, the nature of isomorphic substituents, the distinction of molecular water from constitutional hydroxyl, and the presence of both crystalline and non-crystalline impurities (Farmel, 1979).

Type
Research Article
Information
Clays and Clay Minerals , Volume 49 , Issue 5 , October 2001 , pp. 410 - 432
Copyright
Copyright © 2001, The Clay Minerals Society

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