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Synthesis of Smectite from Volcanic Glass at Low Temperature

Published online by Cambridge University Press:  28 February 2024

Katsutoshi Tomita ,
Hisanori Yamane  and
Motoharu Kawano
Katsutoshi Tomita
Affiliation:
Institute of Earth Sciences, Faculty of Science, Kagoshima University, 1-21-35 Korimoto, Kagoshima 890, Japan
Hisanori Yamane
Affiliation:
Institute for Materials Research, Tohoku University, 2-1-1, Katahira, Sendai-shi 980, Japan
Motoharu Kawano
Affiliation:
Department of Environmental Sciences and Technology, Faculty of Agriculture, Kagoshima University, 1-21-24 Korimoto, Kagoshima 890, Japan
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Abstract

Smectite and zeolites were formed from a volcanic glass as the products of reaction with NaOH solution at 90°C and 100°C under atmospheric pressure. Formation conditions of smectite and various zeolites were determined by the ratio of the amounts of volcanic glass (g) to NaOH (g) in the solution. Smectite was formed under the condition that the values of weight of volcanic glass (g)/(NaOH(g)/40) are between 0.5 and 6. Fe was an important constituent of the octahedral layer of smectite.

Keywords

Low temperatureSmectiteSodium hydroxide concentrationSynthesisVolcanic glassZeolites
Type
Research Article
Information
Clays and Clay Minerals , Volume 41 , Issue 6 , December 1993 , pp. 655 - 661
Copyright
Copyright © 1993, The Clay Minerals Society

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