CADMIUM SUBSTITUTION IN MIARGYRITE (AGSBS2) AND RELATED PHASES - AN EXPERIMENTAL RECONNAISSANCE

Citation
I. Kelleher et al., CADMIUM SUBSTITUTION IN MIARGYRITE (AGSBS2) AND RELATED PHASES - AN EXPERIMENTAL RECONNAISSANCE, Mineralogical Magazine, 60(400), 1996, pp. 393-401
Citations number
12
Categorie Soggetti
Mineralogy
Journal title
ISSN journal
0026461X
Volume
60
Issue
400
Year of publication
1996
Pages
393 - 401
Database
ISI
SICI code
0026-461X(1996)60:400<393:CSIM(A>2.0.ZU;2-5
Abstract
An experimental study of cadmium substitution into AgXS(2) phases (X = As, Bi, Sb) indicates significant amounts of cadmium can be incorpora ted in the structure by the mechanism 2Cd reversible arrow Ag + X. The limit of substitution of Cd in the high-temperature polymorph of miar gyrite, beta-AgSbS2 is 6.2 at.%, whereas the low-temperature polymorph , alpha-AgSbS2, can accommodate at least 12 at.% cadmium. Substitution of Cd into the cubic beta-AgSbS2 induces a small monoclinic distortio n and the unit cell becomes pseudo-cubic. The alpha reversible arrow b eta transition in Cd-substituted miargyrites is modified by the solute ions, with both a reduction of T-c and transition smearing evident. S imilar effects are also recorded in Cd-substituted AgAsS2 and AgBiS2.