THE CRYSTAL-CHEMISTRY OF THE SOLID-SOLUTION SERIES BETWEEN CHALCOSTIBITE (CUSBS2) AND EMPLECTITE (CUBIS2)

Citation
Mf. Razmara et al., THE CRYSTAL-CHEMISTRY OF THE SOLID-SOLUTION SERIES BETWEEN CHALCOSTIBITE (CUSBS2) AND EMPLECTITE (CUBIS2), Mineralogical Magazine, 61(1), 1997, pp. 79-88
Citations number
15
Categorie Soggetti
Mineralogy
Journal title
ISSN journal
0026461X
Volume
61
Issue
1
Year of publication
1997
Pages
79 - 88
Database
ISI
SICI code
0026-461X(1997)61:1<79:TCOTSS>2.0.ZU;2-Y
Abstract
Sulphosalts in the system CuSbS2-CuBiS2 (chalcostibite-emplectite) for m a complete solid solution series. Seven compositions with the genera l formula Cu(SbxBi1-x)S-2 have been synthesized using dry methods at 3 10 degrees C. All members of the series are orthorhombic (space group Pnma) and show smoothly increasing a and b cell parameters with substi tution of Bi for Sb; the c cell parameter increases up to 50% CuBiS2 s ubstitution and then becomes constant. DSC experiments on CuBiS2 show an endothermic heat effect (2.35 kJ/mol.) at 472 degrees C due to the breakdown reaction to Cu3BiS3 (wittichenite) plus Bi2S3 (bismuthinite) . With the addition of 10% CuSbS2 to CuBiS2, the decomposition tempera ture increases and the endothermic peak is broadened but the energy re mains essentially the same (2.53 kJ/mol.). No evidence of this decompo sition was observed when the amount of the CuSbS2 component was >30%. The local structure and co-ordination of Cu in the samples were studie d by EXAFS analysis of the Cu-K edge but no significant variation occu rs in the local Cu environment. The Debye-Waller factor for the first shell of S atoms surrounding Cu in end member CuSbS2 tends to be sligh tly smaller than for the intermediate solid solutions, suggesting that the tetrahedral Cu environments in the intermediate composition sampl es is somewhat more disordered than in the end-member. The low expansi on characteristics along c appear to be controlled by the linkages bet ween the (CuS3 + BiS2) sheets perpendicular to c being relatively infl exible.