Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist RIMG advertisement
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; January 2001; v. 86; no. 1-2; p. 124-131
© 2001 Mineralogical Society of America
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (8)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Alba, M.D.
Right arrow Articles by Perdigón, A.C.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Hydrothermal reactivity of Lu-saturated smectites: Part II. A short-range order study

M.D. Alba, A.I. Becerro, M.A. Castro* and A.C. Perdigón

Departamento de Química Inorgánica. Instituto de Ciencia de Materiales, Universidad de Sevilla, Consejo Superior de Investigaciones Científicas, Avda. Américo Vespucio, 41092-Sevilla, Spain

Correspondence: * E-mail: mcastro{at}cica.es

The short-range order of a set of Lu-saturated smectites, modified by hydrothermal treatment at 400 °C, which give rise to a new crystalline phase (Lu2Si2O7), has been analyzed. In particular, the modifications undergone by the tetrahedral Si atoms of the lattice and the possible diffusions of O-T layer ions to other structural positions were investigated. Single-pulse, magic-angle-spinning nuclear magnetic resonance (MAS-NMR) measurements from the 1H, 7Li, 27Al, and 29Si nuclei, as well as two-dimensional 1H-27Al cross-polarization MAS-NMR experiments, have been made on both the initial and the hydrothermally treated samples. The results show that (1) the formation of the Lu2Si2O7 takes place from Si atoms surrounded by Al tetrahedra in the samples that contain tetrahedral Al; (2) there is a diffusion of octahedral cations to the interlayer positions during the hydrothermal treatments, compatible with the X-ray diffraction data reported for this reaction; and (3) the octahedral Al migrates to the vacant tetrahedral positions that appear during the formation of the new Lu2Si2O7 phase. A clear relationship between each sample composition and its reactivity is defined.




This article has been cited by other articles:


Home page
Eur J MineralHome page
F. MARTIN, E. FERRAGE, S. PETIT, P. de PARSEVAL, L. DELMOTTE, J. FERRET, D. ARSEGUEL, and S. SALVI
Fine-probing the crystal-chemistry of talc by MAS-NMR spectroscopy
European Journal of Mineralogy, October 1, 2006; 18(5): 641 - 651.
[Abstract] [Full Text] [PDF]


Home page
Clays and Clay MineralsHome page
P. Di Leo, P. Di Leo, and J. Cuadros
113Cd, 1H MAS NMR AND FTIR ANALYSIS OF Cd2+ ADSORPTION ON DIOCTAHEDRAL AND TRIOCTAHEDRAL SMECTITE
Clays and Clay Minerals, August 1, 2003; 51(4): 403 - 414.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America