dc.contributor.author |
Ball, Matthew C. |
|
dc.contributor.author |
Norwood, Leslie S. |
|
dc.date.accessioned |
2025-04-11T09:28:01Z |
|
dc.date.available |
2025-04-11T09:28:01Z |
|
dc.date.issued |
1978 |
|
dc.identifier.uri |
http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/18640 |
|
dc.description.abstract |
Measurements 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.language.iso |
en |
en_US |
dc.publisher |
Journal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1978, 74 (06) |
en_US |
dc.subject |
Chemistry |
en_US |
dc.subject |
Surface chemistry |
en_US |
dc.subject |
Porosity |
en_US |
dc.subject |
Journal of the Chemical Society : Faraday Transaction - I |
en_US |
dc.title |
Studies in the system CaSO4+ H2O. Part 6.—Surface chemistry and porosity of the CaSO4 hemihydrates |
en_US |
dc.type |
Article |
en_US |