Structural role of large cations in sulfides with Cs+ and Tl+


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Resumo

The results of a crystallographic analysis of the structures of CsFe2S3, Tl2PbZrS4, and Tl2PbGeS4 with a 1:1 cation–anion ratio are used to identify a joint F sublattice for Cs and S in the first compound and two separate F sublattices for cations and anions in the second compound (the PbS structural type). The substitution of the small Ge4+ (with its tetrahedral coordination by sulfur) for Zr4+ in the composition results in an increase in the unit cell volume, i.e., a decrease in the packing density for both cations and anions in the structure of the third compound. In the absence of regular F sublattices, there are “two-dimensional” orderings, typical of the PbS type, for the atomic positions in the projections of this structure.

Sobre autores

S. Borisov

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Email: svetlana@niic.nsc.ru
Rússia, Novosibirsk

S. Magarill

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Autor responsável pela correspondência
Email: svetlana@niic.nsc.ru
Rússia, Novosibirsk

N. Pervukhina

Nikolaev Institute of Inorganic Chemistry, Siberian Branch

Email: svetlana@niic.nsc.ru
Rússia, Novosibirsk

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