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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.1994.058.393.04</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Petrology and Geochemistry</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Phase Relations in the System PbS-PbSe-PbTe</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Liu</surname>
<given-names>H.</given-names>
</name></contrib>
<contrib contrib-type="author">
<name>
<surname>Chang</surname>
<given-names>L. L. Y.</given-names>
</name></contrib>
<aff>Department of Geology, University of Maryland, College Park, Maryland 20742, U.S.A.</aff></contrib-group>
<pub-date pub-type="ppub">
<month>12</month>
<year>1994</year>
</pub-date>
<volume>58</volume>
<issue>393</issue>
<fpage>567</fpage>
<lpage>578</lpage>
<history>
<date date-type="received">
<day>10</day>
<month>1</month>
<year>1994</year>
</date>
<date date-type="rev-recd">
<day>28</day>
<month>2</month>
<year>1994</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1994, The Mineralogical Society</copyright-statement>
<copyright-year>1994</copyright-year>
<abstract>
<title>Abstract</title>
<p>Phase relations in the system PbS-PbSe-PbTe were investigated in the temperature range between 1150 and 300&#x00B0;C. There is a complete solid solution series along the join PbS-PbSe, whereas miscibility gaps exist below &#x223C; 350&#x00B0;C and 805&#x00B0;C along joins PbSe-PbTe and PbS-PbTe, respectively. Both gaps extend into the ternary system, and the range of the gap between PbS and PbTe reduces in size with temperature as well as Se-content.</p>
<p>By using the subregular model of mixing (Ganguly and Saxena, 1987), mixing energetics and activity composition relations of Pb<italic>X</italic> were derived. The temperature-dependence of the interaction parameters was calculated to be 5057.6 &#x2212; 1.7<italic>T</italic>, 9605.2 &#x2212; 4.4<italic>T</italic>, 3933.2 &#x2212; 3.1<italic>T</italic> (<italic>T</italic> &#x003C; 500&#x00B0;C), 6410.3 &#x2212; 6.35<italic>T</italic> (<italic>T</italic> &#x003C; 500&#x00B0;C) 1649 &#x2212; 0.26<italic>T</italic>, 1594.6 &#x2212; 0.2<italic>T</italic>, and 12906.3 &#x2212; 17.3<italic>T</italic> for WW<sub>Ste</sub>, W<sub>TeS</sub>, W<sub>SeTe</sub>, W<sub>TeSe</sub>, W<sub>SSe</sub>, W<sub>SeS</sub>, and W<sub>SSeTe</sub>, respectively. A critical temperature along the join PbS-PbSe at &#x223C; 100&#x00B0;C was obtained from interaction parameter calculation, which suggests the separation of the PbS-PbSe series.</p>
<p>Correlation of solid-solution ranges established in this study with natural occurrences was made.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>lead chalcogenides</kwd>
<kwd>phase relations</kwd>
<kwd>thermodynamics</kwd>
<kwd>PbS-PbSe-PbTe system</kwd>
</kwd-group>
</article-meta>
</front>
</article>
