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Swelling pressure on montmorillonite layers versus H-O-H bending frequency of the interlayer water



Swelling pressure on montmorillonite layers versus H-O-H bending frequency of the interlayer water



Clays and Clay Minerals 44(6): 749-756



The in-depth perturbation of vicinal water by the surfaces of montmorillonite layers was investigated by relating the swelling pressure, Pi , of the montmorillonite layers to the H-O-H bending frequency, v2, of the interlayer water. For this purpose, an oriented montmorillonite gel was deposited on a porous filter in an environmental chamber. On its underside the filter was in contact with a solution maintained at atmospheric pressure.

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Accession: 002973983

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