Abstract
DTA and EGA curves of montmorillonite and laponite treated with three metachromic dyes and of sepiolite and palygorskite treated with butylamine and pyridine were described, focussing on the contribution of the EGA to the interpretation of the different DTA peaks.
Zusammenfassung
DTA- und EGA-Kurven von nach dem Metachromverfahren behandeltem Montmorillonit und Laponit sowie von mit Buthylamin und Pyridin behandeltem Sepiolith und Palygorskit werden beschrieben. Schwerpunkt war der Beitrag der EGA zur Interpretierung der verschiedenen DTA-Peaks.
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The author wishes to thank Dr. Harold Cross from Jerusalem for critical reading of the manuscript. A financial support of the Faculty of Science of the Hebrew University of Jerusalem is highly acknowledged. The laponite sample was kindly donated by Laporte Industries, England.
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Yariv, S. Combined DTA — mass spectrometry of organo-clay complexes. Journal of Thermal Analysis 36, 1953–1961 (1990). https://doi.org/10.1007/BF01914111
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DOI: https://doi.org/10.1007/BF01914111