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

Clays and Clay Minerals; August 2001; v. 49; no. 4; p. 347-354
© 2001 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 HighWire
Right arrow Citing Articles via Web of Science (6)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Shoval, S.
Right arrow Articles by Panczer, G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

HYDROXYL-STRETCHING BANDS IN CURVE-FITTED MICRO-RAMAN, PHOTOACOUSTIC AND TRANSMISSION INFRARED SPECTRA OF DICKITE FROM ST. CLAIRE, PENNSYLVANIA

S. Shoval1, S. Yariv2, K.H. Michaelian3, M. Boudeulle4 and G. Panczer4

1 Geology Group, Department of Natural Sciences, The Open University of Israel, 16 Klausner St., 61392 Tel Aviv, Israel
2 Department of Inorganic and Analytical Chemistry, The Hebrew University of Jerusalem, 91904 Jerusalem, Israel
3 Natural Resources Canada, CANMET Western Research Centre, Devon, Alberta, Canada T9G 1A8
4 LPCML, UMR 5620 CNRS, Claude Bernard University-Lyon 1, 43 Bd. 11 November 1918, 69622 Villeurbanne Cedex, France

E-mail of corresponding author: shoval{at}oumail.openu.ac.il

The OH-stretching region in curve-fitted micro-Raman, photoacoustic and transmission IR spectra of St. Claire dickite was investigated. Polarized Raman spectra recorded from the (001) and (010) faces of the dickite crystal displayed six prominent OH bands. The relative intensities depend strongly on both the orientation of the crystallographic axes and the direction of the electric vector of the laser beam. Four out-of-plane vibrations, AA, AZ, CA and CZ, at ~3710, 3706, 3654 and 3643 cm–1 respectively, predominate when the electric vector is perpendicular to the dickite plates. Two in-plane vibrations, DZ and DA at 3627 and 3623 cm–1, intensify when the electric vector is parallel to the plane. The relationship between band intensity and crystal orientation was interpreted in terms of longitudinal optic (LO) and transverse optic (TO) crystal vibration modes. These LO and TO crystal modes were also observed in curve-fitted photoacoustic and transmission IR spectra of coarse, non-oriented crystals of the dickite.

Key Words: Curve-fitting • Dickite • Infrared • LO and TO Crystal Modes • Micro-Raman • OH bands • SEM




This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
C. T. Johnston, J. E. Kogel, D. L. Bish, T. Kogure, and H. H. Murray
LOW-TEMPERATURE FTIR STUDY OF KAOLIN-GROUP MINERALS
Clays and Clay Minerals, August 1, 2008; 56(4): 470 - 485.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
E. Balan, M. Lazzeri, A. M. Saitta, T. Allard, Y. Fuchs, and F. Mauri
First-principles study of OH-stretching modes in kaolinite, dickite, and nacrite
American Mineralogist, January 1, 2005; 90(1): 50 - 60.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
T. ALLARD, P. ILDEFONSE, L. P. D. VILLAR, S. SORIEUL, M. PELAYO, B. BOIZOT, E. BALAN, and G. CALAS
Radiation-induced defects in dickites from the EI Berrocal granitic system (Spain): relation with past occurrence of natural radioelements
European Journal of Mineralogy, August 1, 2003; 15(4): 629 - 640.
[Abstract] [Full Text] [PDF]




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