Low-temperature FTIR study of kaolin-group minerals

Low-temperature FTIR spectroscopy was used to characterize the ν(OH) region of kaolin-group minerals including well ordered to poorly ordered kaolins from Georgia, Brazil, and England, along with samples of discrete dickite and nacrite. Low-temperature FTIR spectra were useful in resolving dickite-...

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Bibliographic Details
Published in:Clays and clay minerals 2008-08, Vol.56 (4), p.470-485
Main Authors: Johnston, Cliff T, Kogel, Jessica Elzea, Bish, David L, Kogure, Toshihiro, Murray, Haydn H
Format: Article
Language:English
Subjects:
Biogeosciences
chemical properties
clay mineralogy
clay minerals
Dickite
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
Exact sciences and technology
experimental studies
FTIR spectra
FTIR SPECTROSCOPY
Geochemistry
Hinckley Index
infrared spectra
Kaolin-Group Minerals
Kaolinite
low temperature
LOW-TEMPERATURE FTIR SPECTROSCOPY
Medicinal Chemistry
Mineralogy
Nacrite
Nanoscale Science and Technology
rock, sediment, soil
sed rocks, sediments
Sedimentary petrology
sheet silicates
Silicates
Soil Science & Conservation
spectra
Structural Disorder
temperature
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Summary:Low-temperature FTIR spectroscopy was used to characterize the ν(OH) region of kaolin-group minerals including well ordered to poorly ordered kaolins from Georgia, Brazil, and England, along with samples of discrete dickite and nacrite. Low-temperature FTIR spectra were useful in resolving dickite- and nacrite-like features present in the spectra of kaolins when cooled to
ISSN:0009-8604
1552-8367
DOI:10.1346/CCMN.2008.0560408