Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Clay Minerals Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Clay Minerals; December 2001; v. 36; no. 4; p. 467-472; DOI: 10.1180/0009855013640001
© 2001 Mineralogical Society of Great Britain and Ireland
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by BREEN, C.
Right arrow Articles by MORONTA, A. J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Research Paper

Influence of exchange cation and layer charge on the isomerization of {alpha}-pinene over SWy-2, SAz-1 and Sap-Ca

C. BREEN* and A. J. MORONTA{dagger}

Materials Research Institute, Sheffield Hallam University, Sheffield S1 1WB, UK

* E-mail: c.breen{at}shu.ac.uk

(Received 27 November 2000; revised 20 March 2000)

SWy-2 (Wyoming), Sap-Ca saponite (California) and SAz-1 (Cheto, Arizona) were exchanged with different cations (Al, Ni, Mg, Ca and Na). The catalytic activity of these ion-exchanged clays was measured directly using the isomerization of {alpha}-pinene at 80°C for 2 h to yield camphene, limonene and other minor products. The order of activity for the different cation-exchanged forms was Al > Ni > Mg > Ca > Na, which correlated well with the known polarizing power of these cations and the resulting interlayer acidity. Catalysts derived from Sap-Ca were the most active followed by SWy-2, with SAz-1 the least active by a considerable margin. The greater activity of Sap-Ca over SWy-2 was attributed to the high tetrahedral charge in the former. Reduction of the layer charge of SAz-1 using Li fixation caused a significant improvement in the catalytic activity of the Al-exchanged reduced-charge SAz-1.

KEYWORDS: {alpha}-pinene, ion-exchanged clays, exchangeable cations, catalysis







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of Great Britain and Ireland