摘要
We report on a temperature-dependent Mossbauer study of natural and synthetic malayaite, CaSnSiO5. Sn-119 spectra have been measured between liquid nitrogen temperatures and 1310 K. The Sn-119 Mossbauer shift is found to show a significantly reduced temperature dependence if compared with predictions for the second-order Doppler contribution. In iron doped malayaite, the two dominating Fe-57 subspectra are attributed to ferric ions located on Sn and Ca sites. The temperature-dependent spectra of Sn-119 and Fe-57 are discussed in context with the structural anomaly at about 500 K reported by Great et al. From comparison of quadrupole interactions of tin and iron, an estimate of the nuclear quadrupole moment of Sn-119 is derived as Q = 0.13b which is in good agreement with recent studies.
- 出版日期1999-2