Abstract

The two-phase region in the system 2(ZnSe)x(CuInSe2)1−x covers the chemical composition range 0.10<x⩽0.36, in which a tetragonal and a cubic phase are coexisting. The structural relation between both phases was determined by selected area diffraction (SAD) and transmission electron microscopy (TEM). Both crystal structures are very similar and the extremely small mismatch of the lattice constants of the tetragonal phase and the embedding cubic matrix phase allows for the grain boundaries to be virtually strain-free and, therefore, without notable dislocations. The tetragonal phase forms grains of flat discus-like shape in the ambient cubic matrix, with the short discus axis parallel to the tetragonal c-axis. TEM experiments proved that the discus-shaped tetragonal particles are collinear with the (100)cub, (010)cub and (001)cub planes of the cubic phase. Cooling and annealing experiments revealed a near-equilibrium state only to be realized for small cooling rates less than 2K/h and/or for a long-time annealing with subsequent rapid quenching. Only then there will be no cation ordering in both, the tetragonal domains and the parental cubic matrix phase. If, however, the samples are kept in a state far away from the equilibrium condition both phases reveal Stannite-type cation ordering. Within the composition range of 0⩽x⩽0.10 only tetragonal 2(ZnSe)x(CuInSe2)1−x-alloys exist. At concentration rates above 36mol% 2(ZnSe) only cubic structured solid solutions of ZnSe and CuInSe2 are found to be stable. However, in the range 36mol% to about 60mol% 2(ZnSe) tiny precipitates with Stannite-like structure exist, too.

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