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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.1972.038.300.09</article-id>
<title-group>
<article-title>Calcium Sulphosilicate in Lime-Kiln Wall Coating</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Pryce</surname>
<given-names>M. W.</given-names>
</name>
<aff>Government Chemical Laboratories, Perth, Western Australia</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1972</year>
</pub-date>
<volume>38</volume>
<issue>300</issue>
<fpage>968</fpage>
<lpage>971</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>1</month>
<year>1972</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1972, The Mineralogical Society</copyright-statement>
<copyright-year>1972</copyright-year>
<abstract>
<title>Summary</title>
<p>Green calcium sulphosilicate layers were formed in lime-larnite-calcite wall coating in a lime kiln at Rivervale, Western Australia. The compound formed in the kiln flame area by the combination of siliceous lime sand feed with sulphur trioxide from the sulphurous oil fuel.</p>
<p>The calcium sulphosilicate is orthorhombic with <italic>a</italic> 10&#x00B7;183, <italic>b</italic> 15&#x00B7;408, <italic>c</italic> 6&#x00B7;825 &#x00C5;, space group <italic>Pcmn</italic>. Crystals are [100] tablets or prisms elongated along <italic>c</italic>, D 2&#x00B7;95, hardness 5, streak pale green, decomposed by organic acids. Optical properties <italic>&#x03B1;</italic> 1&#x00B7;632 = [001] blue, <italic>&#x03B2;</italic> 1&#x00B7;638 = [100] yellow-green <italic>&#x03B3;</italic> 1&#x00B7;640 yellow-green, 2V<italic>&#x03B1;</italic> = 60&#x00B0;, dispersion <italic>r</italic> &#x003E; <italic>v</italic>, X-ray powder lines: 2&#x00B7;855 (10) 032,202; 2&#x00B7;838 (7) 330,321; 3&#x00B7;35 (6) 012; 2&#x00B7;622 (6) 331; 2&#x00B7;571 (6) 060; 3&#x00B7;20 (5) 231; 1&#x00B7;962 (5); 1&#x00B7;899 (5); 1&#x00B7;896 (5); 1&#x00B7;372 (5).</p>
<p>Chemical analysis by P. Hewson gave: SiO<sub>2</sub> 21&#x00B7;50, Al<sub>2</sub>O<sub>3</sub> 1&#x00B7;83, Fe<sub>2</sub>O<sub>2</sub> 0&#x00B7;50, CO<sub>2</sub> 0&#x00B7;49, P<sub>2</sub>O<sub>5</sub> 0&#x00B7;23, CaO 57&#x00B7;19, MgO 0&#x00B7;35, Na<sub>2</sub>O 0&#x00B7;22, K<sub>2</sub>O 0&#x00B7;22, SrO 0&#x00B7;15, Li<sub>2</sub>O 0&#x00B7;06, SO<sub>3</sub> 16&#x00B7;71, H<sub>2</sub>O<sup>+</sup> 0&#x00B7;28, H<sub>2</sub>O<sup>&#x2212;</sup> 0&#x00B7;10, others 0&#x00B7;04, total 99&#x00B7;87. On a water-free basis the unit cell contains <inline-formula><mml:math><mml:mrow><mml:msub><mml:mo>Ca</mml:mo><mml:mrow><mml:mn>19</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>66</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>Mg</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>17</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>Na</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>14</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>K</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>08</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>Sr</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>03</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>Li</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>08</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mo>S</mml:mo></mml:mrow><mml:mrow><mml:mn>4</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>02</mml:mn></mml:mrow><mml:mrow><mml:mn>6</mml:mn><mml:mo>&#x2212;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mo>Si</mml:mo><mml:mrow><mml:mn>6</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>90</mml:mn></mml:mrow></mml:msub><mml:msub><mml:mo>Al</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>78</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mo>Fe</mml:mo></mml:mrow><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>12</mml:mn></mml:mrow><mml:mrow><mml:mn>3</mml:mn><mml:mo>&#x002B;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mo>C</mml:mo><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>21</mml:mn></mml:mrow></mml:msub><mml:msubsup><mml:mrow><mml:mo>P</mml:mo></mml:mrow><mml:mrow><mml:mn>0</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>06</mml:mn></mml:mrow><mml:mrow><mml:mn>5</mml:mn><mml:mo>&#x2212;</mml:mo></mml:mrow></mml:msubsup><mml:msub><mml:mo>O</mml:mo><mml:mrow><mml:mn>47</mml:mn><mml:mo>&#x00B7;</mml:mo><mml:mn>71</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>, approximately 4[Ca<sub>5</sub>(SiO<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>] and isostructural with silicocarnotite, 4[Ca<sub>5</sub>(PO<sub>4</sub>)<sub>2</sub>SiO<sub>4</sub>]. Type material is preserved at the Government Chemical Laboratories, Perth, Western Australia.</p></abstract>
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