Article contents
The dissociation of dolomite
Published online by Cambridge University Press: 14 March 2018
Extract
That dolomite (CaCO3 . MgCO3) on being heated behaves as though it were a mixture of the two carbonates by dissociating in two distinct stages, appears to be the widely accepted opinion. Thus it is staled (Mem. Geol. Survey, Special Reports on Min. Resources, London, 1920, vol. 16, ‘Refractory Minerals’, p. 102) ‘On calcination, dolomite undergoes a progressive dissociation which may be considered chemically as covering two distinct stages. The first effect of rising temperature is the expulsion of carbon dioxide from the magnesium carbonate contained in the dolomite and the formation of a mixture of magnesium oxide and calcium carbonate, accompanied by a considerable reduction in volume… . Complete calcination results in the expulsion of the remaining carbon dioxide, a still further reduction in volume, and the production of a dense crystalline aggregate of magnesium and calcium oxides.’
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 20 , Issue 101 , June 1923 , pp. 54 - 59
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1923
- 2
- Cited by