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Science 11 September 1964:
Vol. 145. no. 3637, pp. 1189 - 1190
DOI: 10.1126/science.145.3637.1189
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Articles

Infrared Absorption of Hydroxyl Groups in Kaolinite

Victor C. Farmer 1

1 Macaulay Institute for Soil Research, Craigiebuckler, Aberdeen, Scotland

Effects of sample orientation on the hydroxyl absorption of kaolinite can be interpreted in terms of the structure indicated by x-ray investigations, in which the surface hydroxyl groups of each layer are directed toward the oxygen atoms on the surface of the next layer.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
COLIN FARMER (1920-2006).
M. J. Wilson (2006)
Clay Minerals 41, 693-695
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ALTERATION OF VOLCANIC ROCKS AND GENESIS OF KAOLIN DEPOSITS IN THE SILE REGION, NORTHERN ISTANBUL, TURKEY. I: CLAY MINERALOGY.
O. I. Ece, O. I. Ece, Z.-E Nakagawa, and P. A. Schroeder (2003)
Clays and Clay Minerals 51, 675-688
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IN SITU CHARACTERIZATION AND DIFFERENTIATION OF KAOLINITES IN LATERITIC WEATHERING PROFILES USING INFRARED MICROSPECTROSCOPY.
A. Beauvais, A. Beauvais, and J. Bertaux (2002)
Clays and Clay Minerals 50, 314-330
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INFLUENCE OF SYNTHESIS pH ON KAOLINITE "CRYSTALLINITY" AND SURFACE PROPERTIES.
C.-I. Fialips, C.-I. Fialips, S. Petit, A. Decarreau, and D. Beaufort (2000)
Clays and Clay Minerals 48, 173-184
   Abstract »    Full Text »    PDF »


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Science. ISSN 0036-8075 (print), 1095-9203 (online)