Studies in the system CaSO4+ H2O. Part 6.—Surface chemistry and porosity of the CaSO4 hemihydrates

dc.contributor.authorBall, Matthew C.
dc.contributor.authorNorwood, Leslie S.
dc.date.accessioned2025-04-11T09:28:01Z
dc.date.available2025-04-11T09:28:01Z
dc.date.issued1978
dc.description.abstractMeasurements of surface area and pore size distributions have been used to compare the two forms of calcium sulphate hemihydrate. The α-form, prepared from solution has a low surface area and transitional pores. Dehydration causes a reduction in the volume of the smaller transitional pores and subsequent rehydration causes little change. The β-form has a higher surface area and larger pores. Dehydration increases the volume of the smaller transitional pores and again the effect of rehydration is negligible.en_US
dc.identifier.urihttp://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/18640
dc.language.isoenen_US
dc.publisherJournal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1978, 74 (06)en_US
dc.subjectChemistryen_US
dc.subjectSurface chemistryen_US
dc.subjectPorosityen_US
dc.subjectJournal of the Chemical Society : Faraday Transaction - Ien_US
dc.titleStudies in the system CaSO4+ H2O. Part 6.—Surface chemistry and porosity of the CaSO4 hemihydratesen_US
dc.typeArticleen_US

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