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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.1974.039.305.12</article-id>
<title-group>
<article-title>Oxygen Partial Pressures; Control, Variation, and Measurement in Quench Furnaces at One Atmosphere Total Pressure</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Biggar</surname>
<given-names>Gordon M.</given-names>
</name>
<aff>Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1974</year>
</pub-date>
<volume>39</volume>
<issue>305</issue>
<fpage>580</fpage>
<lpage>586</lpage>
<history>
<date date-type="received">
<day>29</day>
<month>3</month>
<year>1973</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1974, The Mineralogical Society</copyright-statement>
<copyright-year>1974</copyright-year>
<abstract>
<title>Summary</title>
<p>Oxygen partial pressures in atmospheric-pressure quench furnaces were found to vary by as much as 0&#x00B7;5 in log <italic>f</italic>o<sub>2</sub> when changes were made in gas flow rate and direction suggesting that careful analysis of the gas mixture supplied to a furnace is <italic>not</italic> a guarantee of the oxygen pressure that a sample in the furnace will attain. The use of magnesiow&#x00FC;stite compositions, with variable oxygen contents, as indicators of oxygen pressure is described.</p></abstract>
</article-meta>
</front>
</article>
