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- W2099759904 abstract "In a paper to the Faraday Society (1946), Mering showed that the temperature to which one required to heat montmorillonite to produce irreversible collapse of the c-axis depended on the exchangeable cation. With Na-montmorillonite irreversibility began at about 550°C but with Ca-montmorillonite below 350°C During a study of the liquid phase sorption of pyridine by montmorillonite, the writer obtained evidence that irreversible collapse occurred at 200°C with Li-montmorillonite. The source of montmorillonite was a sample of Wyoming bentonite, which was purified by passing through a Sharples supercentrifuge. The resultant exchange capacity to ammonium acetate at pH 7 was about 90 m.e./100 gms. and the displaced ions chiefly consisted of Na+ and Ca++." @default.
- W2099759904 created "2016-06-24" @default.
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- W2099759904 date "1952-01-01" @default.
- W2099759904 modified "2023-10-18" @default.
- W2099759904 title "Irreversible Dehydration in Montmorillonite" @default.
- W2099759904 doi "https://doi.org/10.1180/claymin.1952.001.7.06" @default.
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