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Abstract

The vacuum-oven technique for quantitative sorption of a glycerol duointerlayer by montmorillonite at 35°C is adapted to 130°C to obtain a mono-interlayer of glycerol, glycerol vapor relative pressure being controlled by temperature differential. Values obtained for montmorillonite agree closely with theoretical values based on liquid glycerol density, while vermiculite retains a mono-interlayer of somewhat less than liquid glycerol density.

References

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Science
Volume 135 | Issue 3507
16 March 1962

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Published in print: 16 March 1962

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M. H. Milford
Department of Soils, University of Wisconsin, Madison
M. L. Jackson
Department of Soils, University of Wisconsin, Madison

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