Clays and Clay Minerals · 1974 · 41 citations · 20 references
Natural SciencesChemistryMaterials ScienceInorganic ChemistryMaterials ChemistryNanomaterialsClay DispersionClay MineralogyClay MineralsMineral-organic InteractionsSurface HydrophilicityClay Mineral SwellingSwellingSwelling Behavior
Abstract The crystalline and osmotic swelling of Na-, Cs-, Mg- and Ca-montmorillonite has been measured in dimethyl sulphoxide and in formamide, N -methyl formamide, dimethyl formamide, N -methyl acetamide and dimethyl acetamide. These liquids have similar dipole moments but their relative permittivities vary appreciably from values less than water to values greater than water. Na-montmorillonite exhibits osmotic swelling (diffuse double layer development − d (001) ≫ 19 Å) in formamide and N -methyl formamide and Cs gives osmotic swelling behavior in formamide. Cs-montmorillonite in the crystalline swelling region give spacings greater than those found for water with all liquids. Mg- and Ca-montmorillonite did not give spacings greater than 19 Å in any of the liquids studied. The swelling behavior of montmorillonite is affected by relative permittivity but for liquids with a similar relative permittivity methyl substitution in the molecule may prevent the development of diffuse double layers on the particle surfaces.
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The swelling of montmorillonite
K. Norrish · Discussions of the Faraday Society · 1954 · 1.2K citations
Properties of ordinary water-substance
R.H. Oppermann · Journal of the Franklin Institute · 1940 · 833 citations