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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.1976.040.314.07</article-id>
<title-group>
<article-title>The Halotrichite Group: The Crystal Structure of Apjohnite</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Menchetti</surname>
<given-names>S.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Sabelli</surname>
<given-names>C.</given-names>
</name></contrib>
<aff>Centro di Studio per la Mineralogia e la Geochimica dei Sedimenti, Istituto di Mineralogia dell'Universit&#x00E0; di Firenze, Italy</aff></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1976</year>
</pub-date>
<volume>40</volume>
<issue>314</issue>
<fpage>599</fpage>
<lpage>608</lpage>
<history>
<date date-type="received">
<day>13</day>
<month>5</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>Apjohnite, MnAl<sub>2</sub> (SO<sub>4</sub>)<sub>14</sub>. 22H<sub>2</sub>O,is monoclinic, space group <italic>P</italic>21/<italic>c</italic>, <italic>a</italic> 6&#x2013;198 (2), <italic>b</italic> 24&#x00B7;347 (4), <italic>c</italic> 21&#x2013;66 (4) &#x00C5;, &#x03B2; 100&#x00B7;28 (3)&#x00B0; and Z = 4. The crystal structure was determined by means of direct methods applied to X-ray data collected with a single-crystal diffractometer. At the end of the refinement, performed with least-squares method, the R index was 0&#x00B7;039.</p>
<p>The SO<sub>4</sub> tetrahedra, AI(H<sub>2</sub>O)<sub>6</sub> octahedra, and MnO(H<sub>2</sub>O)<sub>5</sub> octahedra are connected by a hydrogen bonding system; the only direct connection between polyhedra is by sharing of an oxygen between S(4) and Mn. In the asymmetric unit there are twenty-two water molecules, five of which lie in channels of the structure and are not linked to the cations but only to ligand water oxygens by means of hydrogen bonds.</p>
<p>Powder data indicate a close structural relationship between apjohnite, halotrichite, and pickeringite.</p></abstract>
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</article>
