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<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.1957.031.237.07</article-id>
<title-group>
<article-title>Direct Measurement of Standard Reflectances with the Microphotometer</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Hallimond</surname>
<given-names>A. F.</given-names></name><degrees>M.A., Sc.D.</degrees></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1957</year>
</pub-date>
<volume>31</volume>
<issue>237</issue>
<fpage>487</fpage>
<lpage>494</lpage>
<copyright-statement>Copyright &#x00A9; 1957, The Mineralogical Society</copyright-statement>
<copyright-year>1957</copyright-year>
<abstract>
<title>Summary</title>
<p>A visual microphotometer depending on three polarizing screens is used to provide the primary scale for measuring the ratio of intensity between the incident and reflected beams for a prepared standard surface, which is intended for subsequent use in the ordinary procedure with the ore-microscope. A reversing mirror on the microscope stage gives reflection at quasi-normal incidence. Direct measurements on a surface of diamond confirm the validity of the Fresnel formula for a polished surface of this substance, and there is general agreement for a series of transparent bodies ranging up to 17 % reflectance. The standard is a glass-covered metallic surface with a reflectance near 50 %. For pyrite <italic>R</italic><sub><italic>D</italic></sub> = 54&#x00B7;5 %.</p></abstract>
</article-meta>
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</article>
