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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.1988.052.366.08</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Mineralogy and Crystal Structures</subject>
</subj-group>
</article-categories>
<title-group>
<article-title>Comparison of Cation Exchange in Ganophyllite and [Na + Al]-Substituted Tobermorite: Crystal-Chemical Implications</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Komarneni</surname>
<given-names>Sridhar</given-names>
</name>
<aff>Materials Research Laboratory and Department of Agronomy, The Pennsylvania State University, University Park, Pennsylvania 16802, U.S.A.</aff></contrib>
<contrib contrib-type="author">
<name>
<surname>Guggenheim</surname>
<given-names>Stephen</given-names>
</name>
<aff>Department of Geological Sciences, University of Illinois at Chicago, Chicago, Illinois 60680, U.S.A.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>6</month>
<year>1988</year>
</pub-date>
<volume>52</volume>
<issue>366</issue>
<fpage>371</fpage>
<lpage>375</lpage>
<history>
<date date-type="received">
<day>24</day>
<month>3</month>
<year>1987</year>
</date>
<date date-type="rev-recd">
<day>1</day>
<month>7</month>
<year>1987</year>
</date></history>
<copyright-statement>Copyright &#x00A9; 1988, The Mineralogical Society</copyright-statement>
<copyright-year>1988</copyright-year>
<abstract>
<title>Abstract</title>
<p>Ganophyllite and [Na<sup>+</sup> + Al<sup>3+</sup>]-substituted tobermorite exhibited similar cation exchange properties and, in particular, selective cesium exchange. [Na<sup>+</sup> + Al<sup>3+</sup>]-substituted tobermorite and ganophyllite showed a selective Cs exchange of 10.77 and 8.71 meq/100 g from 0.02N NaCl and of 11.08 and 9.04 meq/100 g from 0.02N CaCl<sub>2</sub>, respectively. The [Na<sup>+</sup> + Al<sup>3+</sup>]-substituted tobermorite is structurally similar to ganophyllite: both are roughly analogous to 2:1 layer silicates, both have cross-linking tetrahedra across the interlayer region, and both have exchangeable cations located in zeolite-like sites in the interlayer region. The similarities in cation exchange properties imply that the residual charge configuration of the analogue 2 : 1 layer must be approximately equivalent also.</p></abstract>
<kwd-group>
<title>Keywords</title>
<kwd>ganophyllite</kwd>
<kwd>tobermorite</kwd>
<kwd>cation exchange</kwd>
</kwd-group>
</article-meta>
</front>
</article>
