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Spencer, D. R. F., Coleman, D. S. (1970) Sintering and crystal growth of magnesia in the presence of lime and forsterite. Mineralogical Magazine, 37 (291) 839-851 doi:10.1180/minmag.1970.037.291.09

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Reference TypeJournal (article/letter/editorial)
TitleSintering and crystal growth of magnesia in the presence of lime and forsterite
JournalMineralogical Magazine
AuthorsSpencer, D. R. F.Author
Coleman, D. S.Author
Year1970 (September)Volume37
Issue291
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-291-839.pdf+
DOIdoi:10.1180/minmag.1970.037.291.09Search in ResearchGate
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Mindat Ref. ID6389Long-form Identifiermindat:1:5:6389:4
GUID0
Full ReferenceSpencer, D. R. F., Coleman, D. S. (1970) Sintering and crystal growth of magnesia in the presence of lime and forsterite. Mineralogical Magazine, 37 (291) 839-851 doi:10.1180/minmag.1970.037.291.09
Plain TextSpencer, D. R. F., Coleman, D. S. (1970) Sintering and crystal growth of magnesia in the presence of lime and forsterite. Mineralogical Magazine, 37 (291) 839-851 doi:10.1180/minmag.1970.037.291.09
In(1970, September) Mineralogical Magazine Vol. 37 (291) Mineralogical Society
Abstract/NotesSummaryThe densification of pure magnesia was examined along with mixtures containing 0·5 and 1·0 mol % of calcium oxide and forsterite. The sintering behaviour at temperatures between 1400 and 1800 °C was studied and measurements made of changes in shrinkage, porosity, bulk density, and grain size for sintering times of up to 8 h at sintering temperature. It was found that both the 0·5 and 1·0 mol % additions enhanced the sintering of pure magnesia in the temperature range 1500–1700 °C Increased grain growth was found for mixtures containing forsterite but little change occurred for mixtures containing lime. Examination of the grain growth data showed that the mixtures obeyed a relationship: Time at temperature × Constant = (grain size)n, where n = 2 for the grain growth of pure magnesia and mixtures containing lime, but n = 3 for mixtures of magnesia with additions of a silicate such as forsterite. A value of 78 kcal/mole was obtained for the grain growth of pure magnesia, which agrees with other researches.The extent of the solubility of lime in periclase for each lime-magnesia mixture at each temperature was also examined using electron probe analysis and related to the sintering behaviour observed for these mixtures.


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