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<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<article article-type="research-article">
<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.1969.037.285.13</article-id>
<title-group>
<article-title>Thermal Investigations on Alunite and Its Mixtures with Quartz and Dickite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Kashkai</surname>
<given-names>M.-A.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Babaev</surname>
<given-names>I. A.</given-names>
</name></contrib>
<aff>Ulitsa Husi Hadzhieva II, apt. 6, Baku-5, U.S.S.R.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1969</year>
</pub-date>
<volume>37</volume>
<issue>285</issue>
<fpage>128</fpage>
<lpage>134</lpage>
<history>
<date date-type="received">
<day>00</day>
<month>11</month>
<year>1966</year>
</date>
<date date-type="rev-recd">
<day>00</day>
<month>6</month>
<year>1968</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1969, The Mineralogical Society</copyright-statement>
<copyright-year>1969</copyright-year>
<abstract>
<title>Summary</title>
<p>The thermal decomposition of alunite and of mixtures of alunite with dickite or quartz or both has been studied, and X-ray determinations of the products at various stages of the decomposition have been made. Between 600 and 700&#x00B0;C the product from alunite is a mixture of anhydrous alum and amorphous alumina; between 700 and 770&#x00B0;C the anhydrous alum breaks down into aluminium sulphate and alkali sulphate; then in the prominent 850&#x00B0;C endothermic reaction three-quarters of the sulphate is lost, leaving a mixture of alkali sulphate and <italic>&#x03B3;</italic>-alumina. The area of the 850 &#x00B0;C endothermic peak may be used as a measure of the percentage of alunite in alunitized rocks (alunite-quartz-dickite mixtures).</p></abstract>
</article-meta>
</front>
</article>
