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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.1957.031.236.01</article-id>
<title-group>
<article-title>Kingite, a New Hydrated Aluminium Phosphate Mineral from Robertstown, South Australia</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Norrish</surname>
<given-names>K.</given-names>
</name> <degrees>M.Sc., Ph.D., A.Inst.P.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Rogers</surname>
<given-names>Lillian E. R.</given-names>
</name> <degrees>M.Sc.</degrees></contrib>
<contrib contrib-type="author">
<name>
<surname>Shapter</surname>
<given-names>R. E.</given-names>
</name> <degrees>A.A.C.I.</degrees></contrib>
<aff>Division of Soils, Commonwealth Scientific and Industrial Research Organization, Adelaide, South Australia</aff></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1957</year>
</pub-date>
<volume>31</volume>
<issue>236</issue>
<fpage>351</fpage>
<lpage>357</lpage>
<copyright-statement>Copyright &#x00A9; 1957, The Mineralogical Society</copyright-statement>
<copyright-year>1957</copyright-year>
<abstract>
<title>Summary</title>
<p>A new hydrated aluminium phosphate mineral, <italic>kingite</italic>, from phosphate workings near Robertstown, South Australia, has an idealized formula Al<sub>2</sub>O<sub>3</sub>.Al(OH)<sub>3</sub>.P<sub>2</sub>O<sub>5</sub>.9H<sub>2</sub>O, with some replacement of OH by F. The specific gravity is 2&#x00B7;2 to 2&#x00B7;3, refractive index 1&#x00B7;514, and percentage chemical composition Al<sub>2</sub>O<sub>3</sub> 31&#x00B7;92, P<sub>2</sub>O<sub>5</sub> 28&#x00B7;63, H<sub>2</sub>O 37&#x00B7;93. The three strongest lines on the X-ray diffraction pattern are 9&#x00B7;1, 3&#x00B7;45, and 3&#x00B7;48 &#x00C5;. Kingite changes to a less hydrated phase between 154&#x00B0; C. and 163&#x00B0; C., which is also considered to be a new aluminium phosphate (<italic>meta-kingite</italic>) with idealized formula Al<sub>2</sub>O<sub>3</sub>.Al(OH)<sub>3</sub>.P<sub>2</sub>O<sub>5</sub>.4H<sub>2</sub>O. The strongest lines of its X-ray diffraction pattern are at 7&#x00B7;4, 5&#x00B7;02, and 37&#x00B7;19 &#x00C5;.</p></abstract>
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