1996 Volume 65 Issue 8 Pages 2664-2669
We have found the high-temperature dielectric anomaly around 130°C (Tp) even on first heating of virgin crystal of ferroelastic ammonium sulfate (NH4)2SO4. It has been observed by using polarizing microscope that after heat treatment above Tp the multigrains appeared in the ferroelastic domain, indicating that the nature of the high-temperature anomaly around Tp is of topochemistry, i.e., not related to the high-temperature phase transition but related to chemical change accompanied by partial thermal decomposition at the surface of crystals. This work suggests the origin of nonexistence of prototypic phase in ferroelastic (NH4)2SO4.
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