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

American Mineralogist; October 2005; v. 90; no. 10; p. 1563-1570; DOI: 10.2138/am.2005.1785
© 2005 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 Kyono, A.
Right arrow Articles by Hatta, T.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Light-induced degradation dynamics in realgar: in situ structural investigation using single-crystal X-ray diffraction study and X-ray photoelectron spectroscopy

Atsushi Kyono1,*, Mitsuyoshi Kimata1 and Tamao Hatta2

1 Division of Earth Evolution Sciences, Graduate School of Life and Environmental Sciences, University of Tsukuba, Tennodai 1-1-1, Tsukuba, Ibaraki 305-8572, Japan
2 Japan International Research Center for Agricultural Sciences, Ohwashi 1-1, Tsukuba, Ibaraki 305-8686, Japan

Correspondence: * E-mail: kyono{at}arsia.geo.tsukuba.ac.jp

Light-induced degradation in realgar (arsenic sulfide) has been studied by means of four-circle single-crystal X-ray diffraction and X-ray photoelectron spectroscopy. Because of the alteration of realgar exposed to light, the a lattice parameter and c sinß value increase linearly from 9.327 to 9.385 Å and from 6.320 to 6.364 Å, respectively. In contrast, the b lattice parameter remains substantially constant. Anisotropic variations of the lattice parameters engender a continuous increase of the unit-cell volume from 799.5 to 810.4 Å3. Nevertheless, no correlation exists between the continuous increase of the unit-cell volume and the bond distance variations in As4S4 molecules because the As4S4 molecule in the unit cell expands very little during light exposure. The most pronounced change was in the distance between centroids in As4S4 cages. The spread of As4S4 intermolecular distances increases continuously from 5.642 to 5.665 Å, which directly affects the unit-cell volume expansion of realgar. In addition, the O1s peak increases rapidly after light exposure. The result substantiates the following reaction proposed by Bindi et al. (2003): 5As4S4 + 3O2 -> 4As4S5 + 2As2O3. That is, realgar is transformed into pararealgar if oxygen exists and produces the As4S5 molecule. The additional S atom contributes to anisotropic expansion for the a and c axes because the direction of the additional S atom points toward [44] in the unit cell. Furthermore, an S atom in the As4S5 molecule is released from one of the equivalent As-S-As linkages in As4S5 which becomes the As4S4 molecular of pararealgar. After the As4S5 molecule is divided into an S atom (radical) and the As4S4 (pararealgar type) molecule, the free S atom is re-attached to another As4S4 (realgar type) molecule, and reproduces an As4S5 molecule. The reproduced As4S5 molecule is again divided into an S atom (radical) and an As4S4 (pararealgar type) molecule. This cycle whereby realgar is indirectly transformed into pararealgar via the As4S5 molecule is promoted by light and repeated during light exposure.




This article has been cited by other articles:


Home page
American MineralogistHome page
A. Kyono
Molecular conformation and anion configuration variations for As4S4 and As4Se4 in an anion-substituted solid solution
American Mineralogist, April 1, 2009; 94(4): 451 - 460.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
L. Bindi and P. Bonazzi
Light-induced alteration of arsenic sulfides: A new product with an orthorhombic crystal structure
American Mineralogist, April 1, 2007; 92(4): 617 - 620.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
P. BALLIRANO and A. MARAS
In-situ X-ray transmission powder diffraction study of the kinetics of the light induced alteration of realgar ({alpha}-As4S4)
European Journal of Mineralogy, October 1, 2006; 18(5): 589 - 599.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
P. Bonazzi, L. Bindi, G. Pratesi, and S. Menchetti
Light-induced changes in molecular arsenic sulfides: State of the art and new evidence by single-crystal X-ray diffraction
American Mineralogist, August 1, 2006; 91(8-9): 1323 - 1330.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
E. Makovicky
Crystal Structures of Sulfides and Other Chalcogenides
Reviews in Mineralogy and Geochemistry, January 1, 2006; 61(1): 7 - 125.
[Full Text] [PDF]




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