Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Clays and Clay Minerals Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Clays and Clay Minerals; December 2003; v. 51; no. 6; p. 625-633; DOI: 10.1346/CCMN.2003.0510605
© 2003 Clay Minerals Society
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 Similar articles in Web of Science
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 Web of Science (7)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Langella, A.
Right arrow Articles by de’Gennaro, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

THERMAL BEHAVIOR OF NATURAL AND CATION-EXCHANGED CLINOPTILOLITE FROM SARDINIA (ITALY)

Alessio Langella1,*, Michele Pansini2, Guido Cerri3, Piergiulio Cappelletti4 and Maurizio de’Gennaro4

1 Dipartimento di Studi Geologici ed Ambientali, Via Port’Arsa 11, 82100, Benevento, Italy
2 Laboratorio Materiali del Dipartimento di Meccanica, Strutture, Ambiente e Territorio dell’Università di Cassino, Via Di Biasio 43, 03043 Cassino (FR), Italy
3 Istituto di Scienze Geologico-Mineralogiche dell’Università di Sassari, Corso Angioj 10, 07100 Sassari, Italy
4 Dipartimento di Scienze della Terra dell’Università Federico II, Via Mezzocannone 8, 80134 Naples, Italy

* E-mail address of corresponding author: langella{at}unisannio.it

The thermal behavior of two clinoptilolites from an epiclastic and a pyroclastic deposit of central-northern Sardinia and of their exchanged forms (Li, Na, K, Cs, Mg, Ca, Sr and ammonium) were investigated by differential thermal analysis and thermogravimetry up to 1000°C. Their thermal stability was studied by evaluating the residual crystallinity (expressed as rehydration capacity) after 2 h thermal treatments at 450, 600 and 900°C. The water loss at 1000°C was linearly related to the radius (r) and the charge (z) of the exchangeable cations by the equations r2/z or r3/z, which are proportional to the inverse of the charge density over the surface or to the charge density over the volume of the cations.

The cation composition plays a crucial role in determining the thermal behavior of clinoptilolite. The presence of cations such as Cs or K, which have low surface or volume charge densities, was found to increase the thermal resistance. In particular, the crystallinity of Cs- and K-exchanged forms of both clinoptilolites was not affected by thermal treatment at 450°C and was only slightly reduced by thermal treatment at 600°C.

Predicting the thermal behavior of natural and cation-exchanged forms of these clinoptilolites can provide useful information for possible applications in catalysis, in the case of high thermal stability, or for thermal transformation into ceramics or lightweight aggregates.

Key Words: Clinoptilolite • Ionic Potential • Rehydration Capacity • Thermal Stability • Sardinia • Italy







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Clay Minerals Society