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<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.1973.039.304.04</article-id>
<title-group>
<article-title>Application of Gas Chromatography to Mineral Chemistry: Aluminium-Silicon Ordering in Melilites</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Lachowski</surname>
<given-names>E. E.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Glasser</surname>
<given-names>F. P.</given-names>
</name></contrib>
<aff>Department of Chemistry, University of Aberdeen, Old Aberdeen, Meston Walk, Aberdeen AB9 2UE, Scotland</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1973</year>
</pub-date>
<volume>39</volume>
<issue>304</issue>
<fpage>412</fpage>
<lpage>419</lpage>
<history>
<date date-type="received">
<day>23</day>
<month>2</month>
<year>1973</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1973, The Mineralogical Society</copyright-statement>
<copyright-year>1973</copyright-year>
<abstract>
<title>Summary</title>
<p>The mole fractions of the silicons present in melilites as monomeric (SiO<sub>4</sub>) and dimeric (Si<sub>2</sub>O<sub>7</sub>) groups depends both upon the composition of the melilite and also upon the degree of Al-Si ordering. It is shown that the absolute numbers of monomeric and dimeric silicons in a 10 mg polycrystalline sample can be determined by a relatively rapid chromatographic method.</p>
<p>A statistical theory is developed to treat the data; this contains a variable &#x03BA;-parameter that describes the degree of ordering.</p>
<p>Experimental results are presented and interpreted for one natural and five synthetic melilites. The synthetic gehlenite-rich melilites are appreciably, but not completely disordered. The natural melilite is well ordered, but heating at 1050 &#x00B0;C introduces considerable disorder.</p></abstract>
</article-meta>
</front>
</article>
