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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.1992.056.383.08</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>The Stabilities of Secondary Tin Minerals: Abhurite and its Relationships to Sn(II) and Sn(IV) Oxides and Oxyhydroxides</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Edwards</surname>
<given-names>R.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Gillard</surname>
<given-names>R. D.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Williams</surname>
<given-names>P. A.</given-names>
</name>
<xref ref-type="author-notes" rid="FN1">*</xref></contrib>
<aff>School of Chemistry and Applied Chemistry, University of Wales College of Cardiff, P.O. Box 912, Cardiff CF1 3TB, U.K.</aff></contrib-group>
<author-notes>
<fn fn-type="present-address" id="FN1"><label>*</label><p>Present address: Department of Chemistry, University of Western Sydney Nepean, P.O. Box 10, Kingswood, NSW 2747, Australia.</p></fn></author-notes>
<pub-date pub-type="ppub">
<month>6</month>
<year>1992</year>
</pub-date>
<volume>56</volume>
<issue>383</issue>
<fpage>221</fpage>
<lpage>226</lpage>
<history>
<date date-type="received">
<day>20</day>
<month>6</month>
<year>1991</year>
</date>
<date date-type="rev-recd">
<day>16</day>
<month>9</month>
<year>1991</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1992, The Mineralogical Society</copyright-statement>
<copyright-year>1992</copyright-year>
<abstract>
<title>Abstract</title>
<p>The true formula of abhurite is Sn<sub>21</sub>Cl<sub>16</sub>(OH)<sub>14</sub>O<sub>6</sub>. A stability constant for the phase has been determined at 298.2 K. For the reaction Sn<sub>21</sub>Cl<sub>16</sub>(OH)<sub>14</sub>O<sub>6</sub> (s) + 26H<sup>+</sup> (aq) &#x21CC; 21Sn<sup>2+</sup> (aq) + 16Cl<sup>&#x2212;</sup> (aq) + 20H<sub>2</sub>O (1), log <italic>K</italic><sub>H+</sub> (298.2 K) is equal to &#x2212;39.9 (7). This value is used to assess the relative stability of abhurite in the natural environment and to evaluate its modes of occurrence in relation to other secondary Sn(II) and Sn(IV) species.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>abhurite</kwd>
<kwd>tin minerals</kwd>
<kwd>stability constant</kwd>
</kwd-group>
</article-meta>
</front>
</article>
