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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.1976.040.314.08</article-id>
<title-group>
<article-title>Crystallinity Among Some Hydrous Aluminium Phosphates</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>McConnell</surname>
<given-names>Duncan</given-names>
</name>
<aff>The Ohio State University, Columbus, Ohio 43210</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1976</year>
</pub-date>
<volume>40</volume>
<issue>314</issue>
<fpage>609</fpage>
<lpage>610</lpage>
<history>
<date date-type="received">
<day>19</day>
<month>5</month>
<year>1975</year>
</date>
<date date-type="rev-recd">
<day>26</day>
<month>7</month>
<year>1975</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1976, The Mineralogical Society</copyright-statement>
<copyright-year>1976</copyright-year>
<abstract>
<title>Summary</title>
<p>Compositions of nine hydrous aluminium phosphates are considered with respect to the Al, P, and H contents per 8 oxygens, and it is suggested that when the ratio (Al. P)/H is less than 0&#x00B7;11 (or (Al.P<sup>2</sup>)/H<sup>2</sup> is less than 0&#x00B7;01 such compositions do not crystallize. Examples are bolivarite and evansite.</p></abstract>
</article-meta>
</front>
</article>
