In recent years, X-ray topography has increasingly been applied to the study of phase transitions in single crystals. In principle, the following investigations can be performed with this technique: (a) The revelation of the domain configuration, that arises during the transition into a phase having a lower-symmetry and the characterization of the different kinds of domains. The domains can be imaged by domain contrast or by the contrast of their boundaries. (b) The characterization of domain boundaries by analysing their X-ray contrast in different imaging reflections. (c) The observation of the ȁphase boundaryȁ between the transformed and non-transformed crystal regions. The appearance of this boundary in X-ray topographs depends strongly on the character of the transition. The boundary can be expected to have a high strain gradient and to exhibit strong X-ray contrast for first-order transformations. Second-order transformations can be expected to show zero or only faint contrast in the transition region. In addition, the imaging of the phase boundary may reveal the existence of an intermediate (and frequently incommensurate) phase sandwiched between the ȁmainȁ phases involved in the transition. (d) The observation of pre-transition effects, i.e. the formation of strained regions, crystal defects and/or domains prior to the transformation. The main features of X-ray topographic imaging of domains, domain boundaries and phase boundaries are briefly surveyed. Some examples selected from studies of the following transitions are given: (1) The first-order paraelectric-antiferroelectric transition of copper formation tetrahydrate at -38°C. (2) The first-order paraelectric-antiferroelectric transition of ammonium sulphate at about -50°C. (3) The second-order paraelectric-ferroelectric transition of rubidium hydrogen sulphate at about -8°C. (4) The second-order paraelectric-ferroelectric transitions of Rochelle salt at -18°C and +24°C. In these four cases, the formation of domains during the transition into the lower-symmetry ȁferroicȁ phases and their disappearance during re-transformation is observed. Due to the fine-scale domain configurations in copper formate tetrahydrate, ammonium sulphate and rubidium hydrogen sulphate, and the poor spatial resolution of X-ray topography, a clear resolution of domains is not obtained. In Rochelle salt, well-resolved domains in the form of lamellae parallel (010) and (001) are observed. As expected, the first-order phase boundaries of copper formate tetrahydrate and ammonium sulphate appear on the topographs by strong kinematical contrast demonstrating the high strain gradient present in the boundaries. In rubidium hydrogen sulphate and in (100) plates of Rochelle salt (normal to the ferroelectric axis) no X-ray contrast is observed in the transition region, which indicates the absence of a strain gradient in these cases. This transition, however, is recognizable by the vanishing of domains. In (001) plates of Rochelle salt diffuse extended contrast is observed revealing the presence of a long-range strain gradient in the transition region. In ammonium sulphate, strain which develops in the paraelectric phase prior to the transition is observed. The use of X-ray topography for the study of phase transitions is restricted by the poor spatial resolution of this method and by the rather long exposure times. The latter disadvantage can largely be overcome by the application of synchrotron radiation and image intensifiers (real-time topography).
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