Journal ArticleDOI
Energy Changes in Dehydroxylation of Silicate Minerals
M. Adhikari,M. K. Majumdar +1 more
TLDR
In this article, the dehydroxylation reactions of three 2: 1 layer type clay minerals, illite, vermiculite and chlorite, and the measurement of relative thermal energies involved in the process have been reported.Abstract:
The dehydroxylation reactions of three 2: 1 layer type clay minerals, illite, vermiculite and chlorite and the measurement of relative thermal energies involved in the process have been reported.read more
Citations
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Journal ArticleDOI
Physico-Chemical Properties of Clay Minerals from Alluvial Soil Sediment of West Bengal
TL;DR: The results indicated the presence of illite (2: mical type) as the dominant clay mineral with traces of kaolinite in alluvial soil clays (pond sediments) as mentioned in this paper.
Journal ArticleDOI
Thermal Decomposition of Vermiculites: Kinetics of Dehydration and Dehydroxylation Processes
TL;DR: In this article, the thermal decomposition reactions of homoionic clay minerals, viz. vermiculite, in air in the temperature range 30°-1000°C by thermo-analytical methods are reported.
References
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Journal ArticleDOI
A quick, direct method for the determination of activation energy from thermogravimetric data
Joseph H. Flynn,Leo A. Wall +1 more
Book
Textbook of quantitative inorganic analysis
Izaak M. Kolthoff,E. B. Sandell +1 more
TL;DR: Textbook of quantitative inorganic analysis as discussed by the authors, Textbook of qualitative and quantitative analysis of inorganic properties, textbook of quantitatively analytically-inorganic analysis, as discussed by the authors.
Journal ArticleDOI
Homogeneous and Inhomogeneous Mechanisms in the Dehydroxylation of Minerals
TL;DR: In this paper, a new approach to the dehydroxylation of clay minerals is suggested, based on the concept of inhomogeneous mechanisms, and it is shown that certain calcium minerals undergo dehydroxymethylation in this way.
Journal ArticleDOI
Kinetics of Clay Dehydration
TL;DR: In this paper, the first order nature of the dehydration reaction is shown to be the underlying basis of the type of curve obtained in differential thermal analysis, and the effect of heating at a constant rate on the progress of a reaction for which the isothermal velocity constants are known.