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Conversion equations and domain states in ferroic phase transitions

Abstract Tensorial covariants whose components are linear combinations of the cartesian tensor components which transform like bases for irreducible representations of parent groups facilitate determination of tensorial parameters that onset at ferroic phase transitions. Conversion equations express cartesian tensor components in terms of these parameters. In conjunction with existing tables of fine domain structures these equations enable a complete analysis of tensor properties of domain states in each ferroic phase transition. This includes the tensor distinction of pairs of domain states from which to continue to considerations of tensorial properties when crossing a domain wall is quite straightforward.