We determined the crystal structure of the high-temperature cubic phase of the langbeinite-type (NH 4 ) 2 Cd 2 (SO 4 )t 3 . The observed Cd-O atomic distances are considerably shorter than the standard Cd-O. The structure refinement revealed that the SO 4 ion has several disordered arrangements indicating the existence of the steric hindrance between Cd and SO 4 . These results are quite similar to the previously reported characteristics of several K 2 B 2 (SO 4 ) 3 -type langbeinites. We conclude that the steric hindrance between Cd and SO 4 dominates the phase transition, while the NH 4 ion plays no direct role on the phase transition.
Acknowledgment
The authors thank Foundation for Promotion of Material Science and Technology of Japan (MST Foundation) for the financial support.
Paper originally presented at IMF-11, Iguassu Falls, Brazil, September 5–9, 2005; received for publication January 26, 2006.