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- W2006590935 abstract "The kinetics of the isothermal dehydration of two clay minerals, attapulgite and powdered vermiculite were studied both in vacuo and in the presence of constant water vapour pressure. The mechanism of dehydration was found to be interfacial where diffusion plays a dominant role and it is called “activated diffusion”. A comparison is made with some layered structure clay minerals." @default.
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- W2006590935 date "1979-04-01" @default.
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- W2006590935 title "Effect of structure on the mechanism of dehydration of clay minerals" @default.
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- W2006590935 doi "https://doi.org/10.1016/0040-6031(79)87091-4" @default.
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