International
Tables for Crystallography Volume D Physical properties of crystals Edited by A. Authier © International Union of Crystallography 2006 |
International Tables for Crystallography (2006). Vol. D. ch. 3.4, p. 457
Section 3.4.2.2.2. Ferroelectric domain states
a
Department of Physics, Technical University of Liberec, Hálkova 6, 461 17 Liberec 1, Czech Republic, and bDepartment of Mathematics and Didactics of Mathematics, Technical University of Liberec, Hálkova 6, 461 17 Liberec 1, Czech Republic |
Ferroelectric domain states are defined as states with a homogeneous spontaneous polarization; different ferroelectric domain states differ in the direction of the spontaneous polarization. Ferroelectric domain states are specified by the stabilizer of the spontaneous polarization in the first principal domain state [see equation (3.4.2.16)]:The stabilizer is one of ten polar groups: 1, 2, 3, 4, 6, m, , , , . Since must be a polar group too, it is simple to find the stabilizer fulfilling relation (3.4.2.31).
The number of ferroelectric domain states is given byIf the polar group does not exist, we put . The number of ferroelectric domain states is given for all ferroic phase transitions in the eighth column of Table 3.4.2.7.
The number of principal domain states compatible with one ferroelectric domain state (degeneracy of ferroelectric domain states) is given by
The product of and is equal to the number n of all principal domain states [see equation (3.4.2.19)],The degeneracy of ferroelectric domain states can be calculated for all ferroic phase transitions from the ratio of the numbers n and that are given in Table 3.4.2.7.
According to Aizu (1969, 1970a), we can again recognize three possible cases (see also Table 3.4.2.3):
The classification of full-, partial- and non-ferroelectrics and ferroelastics is given for all Aizu's species in Aizu (1970a).
This classification for all symmetry descents is readily available from the numbers n, , in Table 3.4.2.7. One can conclude that partial ferroelectrics are rather rare.
Example 3.4.2.3. Domain structure in tetragonal perovskites. Some perovskites (e.g. barium titanate, BaTiO3) undergo a phase transition from the cubic parent phase with to a tetragonal ferroelectric phase with symmetry . The stabilizer Hol . There are 3 ferroelastic domain states each compatible with 2 principal ferroelectric domain states that are related e.g. by inversion , i.e. spontaneous polarization is antiparallel in two principal domain states within one ferroelastic domain state.
A similar situation, i.e. two non-ferroelastic domain states with antiparallel spontaneous polarization compatible with one ferroelastic domain state, occurs in perovskites in the trigonal ferroic phase with symmetry and in the orthorhombic ferroic phase with symmetry .
Many other examples are discussed by Newnham (1974, 1975), Newnham & Cross (1974a,b), and Newnham & Skinner (1976).
References
Aizu, K. (1969). Possible species of `ferroelastic' crystals and of simultaneously ferroelectric and ferroelastic crystals. J. Phys. Soc. Jpn, 27, 387–396.Google ScholarAizu, K. (1970a). Possible species of ferromagnetic, ferroelectric and ferroelastic crystals. Phys. Rev. B, 2, 754–772. Google Scholar
Newnham, R. E. (1974). Domains in minerals. Am. Mineral. 59, 906–918.Google Scholar
Newnham, R. E. (1975). Structure–property relations. Berlin: Springer.Google Scholar
Newnham, R. E. & Cross, L. E. (1974a). Symmetry of secondary ferroics I. Mater. Res. Bull. 9, 927–934.Google Scholar
Newnham, R. E. & Cross, L. E. (1974b). Symmetry of secondary ferroics II. Mater. Res. Bull. 9, 1021–1032.Google Scholar
Newnham, R. E. & Skinner, D. P. Jr (1976). Polycrystalline secondary ferroics. Mater. Res. Bull. 11, 1273–1284.Google Scholar