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.
Original language | English |
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Pages (from-to) | 655-661 |
Number of pages | 7 |
Journal | Clays and Clay Minerals |
Volume | 41 |
Issue number | 6 |
DOIs | |
Publication status | Published - 1993 Dec |
Keywords
- Low temperature
- Smectite
- Sodium hydroxide concentration
- Synthesis
- Volcanic glass
- Zeolites
ASJC Scopus subject areas
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth and Planetary Sciences (miscellaneous)