The crystal chemistry of the solid solution series between chalcostibite (CuSbS2) and emplectite (CuBiS2)

Abstract

AbstractSulphosalts in the system CuSbS2-CuBiS2(chalcostibite-emplectite) form a complete solid solution series. Seven compositions with the general formula Cu(SbxBi1–x)S2have been synthesized using dry methods at 310°C. All members of the series are orthorhombic (space groupPnma) and show smoothly increasingaandbcell parameters with substitution of Bi for Sb; theccell parameter increases up to 50% CuBiS2substitution and then becomes constant. DSC experiments on CuBiS2show an endothermic heat effect (2.45 kJ/mol.) at 472°C due to the breakdown reaction to Cu3BiS3(wittichenite) plus Bi2S3(bismuthinite). With the addition of 10% CuSbS2to CuBiS2, the decomposition temperature increases and the endothermic peak is broadened but the energy remains essentially the same (2.53 kJ/mol.). No evidence of this decomposition was observed when the amount of the CuSbS2component was >30%. The local structure and co-ordination of Cu in the samples were studied by EXAFS analysis of the Cu-Kedge but no significant variation occurs in the local Cu environment. The Debye-Waller factor for the first shell of S atoms surrounding Cu in end member CuSbS2tends to be slightly smaller than for the intermediate solid solutions, suggesting that the tetrahedral Cu environments in the intermediate composition samples is somewhat more disordered than in the end-member. The low expansion characteristics alongcappear to be controlled by the linkages between the (CuS3+ BiS2) sheets perpendicular tocbeing relatively inflexible.