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<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1970.037.291.09</article-id>
<title-group>
<article-title>Sintering and Crystal Growth of Magnesia in the Presence of Lime and Forsterite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Spencer</surname>
<given-names>D. R. F.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Coleman</surname>
<given-names>D. S.</given-names>
</name></contrib>
<aff>Department of Materials Technology, University of Technology, Loughborough, Leicestershire</aff></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1970</year>
</pub-date>
<volume>37</volume>
<issue>291</issue>
<fpage>839</fpage>
<lpage>851</lpage>
<copyright-statement>Copyright &#x00A9; 1970, The Mineralogical Society</copyright-statement>
<copyright-year>1970</copyright-year>
<abstract>
<title>Summary</title>
<p>The densification of pure magnesia was examined along with mixtures containing 0&#x00B7;5 and 1&#x00B7;0 mol % of calcium oxide and forsterite. The sintering behaviour at temperatures between 1400 and 1800 &#x00B0;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&#x00B7;5 and 1&#x00B7;0 mol % additions enhanced the sintering of pure magnesia in the temperature range 1500&#x2013;1700 &#x00B0;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 &#x00D7; Constant = (grain size)<sup><italic>n</italic></sup>, where <italic>n</italic> = 2 for the grain growth of pure magnesia and mixtures containing lime, but <italic>n</italic> = 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.</p>
<p>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.</p></abstract>
</article-meta>
</front>
</article>
