Artigo Revisado por pares

Crystal Structure, Mössbauer Spectra, Thermal Expansion, and Phase Transition of Berthierite FeSb2S4

2001; Elsevier BV; Volume: 162; Issue: 1 Linguagem: Inglês

10.1006/jssc.2001.9347

ISSN

1095-726X

Autores

K. Łukaszewicz, A. Pietraszko, J. Stępień‐Damm, A. Kajokas, J. Grigas, H. Drulis,

Tópico(s)

Crystal Structures and Properties

Resumo

Dielectric and ultrasound measurements of berthierite FeSb2S4 reported in the literature revealed a phase transition at Tc=348 K. In the present study the phase transition was confirmed by Mössbauer spectra exhibiting anomalous behavior close to 350 K. Precise lattice parameters measured in the temperature region 305–380 K show a change of slope at about 350 K. The crystal structure of FeSb2S4 has been determined using single-crystal X-ray diffraction data at both room temperature and 370 K above the phase transition. The crystal structure is orthorhombic, Z=4. At 295 K a=11.412(2) Å, b=3.763(1) Å, c=14.161(3) Å, and R=0.0280, and at 370 K a=11.421(2) Å, b=3.771(1) Å, c=14.173(3) Å, and R=0.0274. No symmetry change has been observed. At both temperatures the space group of FeSb2S4 is Pnma with small changes in atomic parameters and interatomic distances. The transition observed at 348 K is, therefore, to be classified as a weak phase transition going on without essential changes in the crystal structure.

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