<?xml version="1.0"?>
<!DOCTYPE article SYSTEM "journalpublishing.dtd">
<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.1958.031.242.05</article-id>
<title-group>
<article-title>Variation of Refractive Index with Ionization Potential in some Isostructural Crystals</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Ahrens</surname>
<given-names>L. H.</given-names>
</name><degrees>M.A., D.Sc., F.R.I.C.</degrees>
<aff>Department of Chemistry, University of Cape Town.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>9</month>
<year>1958</year>
</pub-date>
<volume>31</volume>
<issue>242</issue>
<fpage>929</fpage>
<lpage>936</lpage>
<copyright-statement>Copyright &#x00A9; 1958, The Mineralogical Society</copyright-statement>
<copyright-year>1958</copyright-year>
<abstract>
<title>Summary</title>
<p>A closer understanding of the causes for the variation of refractive index with change of composition has been sought in terms of certain properties of ions. The study is confined to isostructural ionic crystals. It is assumed that polarization of the anions (usually O<sup>2&#x2212;</sup> or F<sup>&#x2212;</sup>) makes the principal contribution to the total refractive index effect, and that variation of refractive index is determined mainly by variable anion polarization. Polarization of the anion is controlled largely by the field in which it finds itself which, in turn, depends on the effective force of attraction of the cation: ionization potentials are used for the purpose of comparing such forces. For compounds involving pairs of 8- and 18-electron cations (Mg<sup>2+</sup> and Zn<sup>2+</sup>; Al<sup>3+</sup> and Ga<sup>3+</sup>; Si&#x007B;4+&#x007D; and Ge<sup>4+</sup>; Ca<sup>2+</sup> and Cd<sup>2+</sup>) or pairs of transition cations (Zr<sup>4+</sup> and Hf<sup>4+</sup>; Nb<sup>5+</sup> and Ta<sup>5+</sup>; Mo<sup>6+</sup> and W<sup>6+</sup>) refractive indices are higher in the crystal that contains the cation of the element with the higher ionization potential. For larger suites of cations of various types (for example, Mg<sup>2+</sup>, Mn<sup>2+</sup>, Fe<sup>2+</sup>, Co<sup>2+</sup>, Ni<sup>2+</sup>, Cu<sup>2+</sup>, and Zn<sup>2+</sup>, radii from 0&#x00B7;65 to 0&#x00B7;80 &#x00C5;.) the predicted relationship between ionization potential and refractive index holds precisely for the compounds <italic>A</italic><sup>2</sup>SiF<sub>6</sub>.6H<sub>2</sub>O (<italic>A</italic><sup>2+</sup>, etc.), but only in part for other compounds; this may be due to the effect of the crystal field on certain 3<italic>d</italic> transition cations.</p></abstract>
</article-meta>
</front>
</article>
