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Application of modern tensor calculus to engineered domain structures. 2. Tensor distinction of domain states

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aInstitut of Physics, Czech Academy of Sciences, Na Slovance 2, 182 21 Praha 8, Czech Republic , and bDepartment of Mathematics and Didactics of Mathematics, Pedagogical Faculty, Technical University of Liberec, Hálkova 6, 461 17 Liberec 1, Czech Republic
*Correspondence e-mail: [email protected]

(Received 19 August 2005; accepted 12 January 2006)

The theory of domain states is reviewed as a prerequisite for consideration of tensorial distinction of domain states. It is then shown that the parameters of the first domain in a ferroic phase transition from a set of isomorphic groups of the same oriented Laue class can be systematically and suitably represented in terms of typical variables. On replacing these variables by actual tensor components according to the previous paper [Kopský (2006)[Kopský, V. (2006b). Acta Cryst. A62, 47-64.], Acta Cryst. A62, 47–64 ], we can reveal the tensorial parameters associated with each particular symmetry descent. Parameters are distinguished by the ireps to which they belong and this can be used to determine which of them are the principal parameters that distinguish all domain states, in contrast to secondary parameters which are common to several domain states. In general, the parameters are expressed as the covariant components of the tensors. A general procedure is described which is designed to transform the results to Cartesian components. It consists of two parts: the first, called the labelling of covariants, and its inverse, called the conversion equations. Transformation of parameters from the first domain state to other states is now reduced to irreducible subspaces whose maximal dimension is three in contrast with higher dimensions of tensor spaces. With this method, we can explicitly calculate tensor parameters for all domain states. To find the distinction of pairs of domain states, it is suitable to use the concept of the twinning group which is briefly described.

1. Ferroic phase transitions

The structure of a crystal depends frequently on external isotropic conditions, which means the temperature T and the isotropic (hydrostatic) pressure p. For example, the structure of ice is described by a phase diagram which contains regions of (T,p) corresponding to 11 different structures. When the external conditions change across the border between two phases in the diagram, the structure also changes. This phenomenon is called a structural phase transition and it is based on the model introduced by Landau (see collection of papers by Landau, 1937[Landau, L. D. (1937). In Collected Papers of L. D. Landau (1967), edited by D. Ter Haar, pp. 193-216. New York: Gordon and Breach. [JETP, 7, pp. 19 and 627 (in Russian); Phys. Z. Sowjet. 11, pp. 26 and 545 (in German).]]). This model assumes a certain kind of instability which causes the atoms to change their positions. The change of temperature and pressure always leads to changes of the structure – the lattice parameters and distances between atoms change within certain limits without a change of the structure type and hence without a change of the space-group-symmetry type. A structural phase transition caused by such displacements of atoms due to a change in symmetry are called displacive. The physical cause of the transition is a certain mode, whose eigenfrequency tends to zero on crossing a certain line of the (T,p) diagram. This mode is called a soft mode and we used to say that this mode freezes, causing permanent distortions and a change of symmetry.

The importance of the theory of group representations in various descriptions of this phenomenon was realized early on by Landau although he was evidently not aware of the state of the art of group theory in 1937; he used his own term races of functions for the bases of irreducible representations. One of the best descriptions of group-theoretical considerations of structural phase transitions is given by Lyubarskii (1960[Lyubarskii, G. Ya. (1960). The Applications of Group Theory in Physics. Oxford: Pergamon Press.]); the use of density functions is more general than the usual model of displacive transitions. The components of distortions which cause the transition are called the transition parameter; the alternative name soft mode reflects the physical origin of the transition. The eigenenergy of this mode tends to zero as the isotropic conditions approach the transition point. The onset of this parameter may induce the onset of other changes described as secondary (improper, faint) parameters.

By ferroic phase transitions, we understand transitions in which the point symmetry of the crystal changes. This occurs in the majority of cases but there also exist transitions to equiclass subgroups in which the point symmetry does not change. Since the point symmetry decreases in ferroic transitions, the transitions are accompanied by an onset of tensor properties which were originally disallowed. The symmetry group G of the original phase is called the parent group, the symmetry Fi of the ferroic phase its ferroic subgroup. We shall talk about the symmetry descent Mathematical equation which characterizes the ferroic transition and our concern will be the qualitative change of tensor properties. However, neither the symmetry nor the newly acquired tensor properties are defined uniquely. If the ferroic group Fi is not a normal subgroup, then its conjugate subgroups are equivalent and any of them may appear as the resulting symmetry. This shows that there does not exist just one specific ferroic state but a set of equivalent ferroic states. The crystal may therefore adopt one of these states but it may also happen that different states correspond to different regions of a crystal. Such regions are called ferroic domains and the states are called ferroic domain states. From now on we shall drop the adjective ferroic. The equivalence of domain states means that they have the same properties with reference to different Cartesian systems so that these properties manifest themselves in different ways with reference to a common Cartesian system of coordinates. A clear theory of domain states has been introduced by Janovec (1972[Janovec, V. (1972). Czech. J. Phys. B22, 974-994.]), and been refined by Kopský (1982a[Kopský, V. (1982a). Group Lattices, Subduction of Bases & Fine Domain Structures for Magnetic Point Groups. Prague: Academia.],b[Kopský, V. (1982b). Czech. J. Phys. B33, 485-509.],c[Kopský, V. (1982c). Czech. J. Phys. B33, 720-744.],d[Kopský, V. (1982d). Czech. J. Phys. B33, 845-869.]).

The existence of domains has an important influence on the final properties of the crystal which is now being utilized in the developing technique of domain engineering. A multidomain sample may be considered as a special case of a polycrystalline state. In both cases, the sample consists of regions of the same structure oriented in different ways with reference to a common Cartesian coordinate system. However, the grains of a polycrystal may be oriented in a rather arbitrary manner while the possible mutual orientations of domains in a multidomain sample are subject to strict rules of the theory of domain states. There are two ways in which the domains affect the resulting properties of a multidomain structure: (i) the volume and spatial arrangement of domains; (ii) the domain walls in which the properties change from one state to another.

It is therefore of interest to develop methods for the calculation of the properties of individual domain states and for comparison of these properties in adjoining domains. The latter is usually called the tensorial distinction of domain states. The standard technique of the characters of ireps allows one to calculate the numbers of tensor components in which domain states differ (Janovec et al., 1992[Janovec, V., Richterová, L. & Litvin, D. B. (1992). Ferroelectrics, 126, 287-292.], 1993[Janovec, V., Richterová, L. & Litvin, D. B. (1993). Ferroelectrics, 140, 95-100.], 1994[Janovec, V., Litvin, D. B. & Richterová, L. (1994). Ferroelectrics, 157, 75-80.], 1995[Janovec, V., Litvin, D. B. & Fuksa, J. (1995). Ferroelectrics, 172, 351-359.]). Our concern is to describe a group-theoretical technique for the calculation of explicit tensor properties of individual domains. This calls for the introduction of some useful concepts.

2. Stability spaces, strata and epikernels

Stability spaces: Anticipating the use of group-theoretical concepts for the description of domain states in ferroic transitions, we first explain the relationship between subgroups and carrier spaces of ireps of the original parent group G. Let us consider a tensor space V(A). It contains subspaces V(A)(G) and V(A)({Fi}) of tensors which are invariant under the groups G and Fi, respectively. Such spaces are called the stability spaces of groups G and Fi. The subspace V(A)(G) is described by tensorial invariants of the group G, while the complementary subspace is defined by components of tensorial Mathematical equation covariants. In considering the symmetry descent Mathematical equation, we have to find those covariant components that became invariant under the action of ferroic groups Fi. Although generally there may exist no such components for a given tensor Mathematical equation, there always exist tensors for which such covariant components exist and hence the stability spaces V(A)(Fi) always contain the stability space V(A)(G) and, for some tensors, these subspaces are proper subspaces. From the set of conjugate subgroups {Fi}, we choose one subgroup F1; the stability space of a conjugate subgroup Fi = giF1gi-1 is related to the stability space V(A)(F1) by V(A)(Fi) = giV(A)(F1). To avoid the necessity of calculation of these spaces for each particular tensor, we use the approach via typical variables and typical carrier spaces. The natural choice of matrix ireps and standard variables for groups of the same oriented Laue class, described in Kopský (2006b[Kopský, V. (2006b). Acta Cryst. A62, 47-64.], hereafter referred to as paper 1), proves also to be the most intelligent and effective.

The typical carrier space Mathematical equation of the parent group G is defined as a direct sum of carrier spaces Mathematical equation of R-ireps of the group G with bases Mathematical equation. All invariants of the group G are represented by a single vector Mathematical equation or by a single variable Mathematical equation. All Mathematical equation covariants are represented by a typical Mathematical equation covariant Mathematical equation.

Let us now consider a subgroup F1 of the group G which is potentially the symmetry of some ferroic state. To this subgroup there corresponds a subspace Mathematical equation of the typical space Vo which contains all those vectors of Vo which are invariant under the action of the subgroup F1. This space is called the typical stability space of the subgroup F1, while individual Mathematical equation are the typical stability spaces of F1 in the carrier spaces Mathematical equation of individual ireps of the group G. Expressing the stability spaces in terms of standard variables, we obtain the set of invariants of the group F1 expressed as linear combinations of these variables. Comparing them with tensorial covariants, we obtain immediately those linear combinations of tensor components that onset at the phase transition from the parent group G to the ferroic subgroup F1. More than that, we can also identify the ireps of the parent group G to which the onsetting parameters belong. Here we simply use the fact that subspaces Mathematical equation behave under the action of the group G like copies of the typical spaces Mathematical equation.

Stabilizers and orbits: Let us now consider the action of the group G on a set Mathematical equation. The elements of Mathematical equation are called points and are denoted by Mathematical equation. The action of G assigns to each element Mathematical equation and to each point Mathematical equation a point Mathematical equation. Let us pick up a certain point Mathematical equation. Some elements Mathematical equation may leave the point Mathematical equation invariant, so that Mathematical equation. It is easy to show that all elements of G that leave the point invariant must constitute a group, which is called the stabilizer of the point Mathematical equation under the action of G.

We denote this group by F1 and the point by Mathematical equation. Performing coset resolution,

Mathematical equation

we can see that all elements of the coset giF1 send the point Mathematical equation to the same point Mathematical equation. The set of points Mathematical equation is called the orbit. If we pick up any point Mathematical equation of the orbit and apply an element of the group G to it, we obtain another point of the orbit. Indeed, Mathematical equation. The stabilizer of a point Mathematical equation is a group Fi = giF1gi-1 conjugate to the group F1. We consider now the first normalizer NG(1)(F1) of the subgroup F1 in G. From coset resolutions

Mathematical equation

and

Mathematical equation

we obtain

Mathematical equation

Changing the indexing of points, starting with Mathematical equation, through Mathematical equation, we obtain that the orbit splits into q subsets labelled by indices from the set Mathematical equation and each of these subsets contains r points Mathematical equation with fixed index i and Mathematical equation. The points with the same i have the same stabilizer Fi = giF1gi-1. The numbers q and r are indices of subgroups q = [G:NG(1)(F1)], r = [NG(1)(F1):F1] and p = qr = [G:F1].

If the set Mathematical equation is the space V of tensors, then the states Mathematical equation are described by tensors Mathematical equation in this space. These tensors then characterize the individual domain states. It is suitable to use the typical spaces and variables for the description of these states.

Linear orbits and strata: If the set Mathematical equation on which the group G acts is a linear space V(n), then the elements are vectors Mathematical equation. If F1 is the stabilizer of a vector Mathematical equation then, using the same coset resolution as in the case of the set Mathematical equation, we obtain an orbit of vectors Mathematical equation for which we use the name linear orbit. Since linear spaces are sets with some special properties, we can expect that linear orbits will also have some properties, characteristic of the linear action of the group G. Indeed, if vector Mathematical equation generates an orbit of vectors Mathematical equation, then every vector Mathematical equation, Mathematical equation, generates an orbit of vectors Mathematical equation. From this we can get the wrong impression that vectors with the same stabilizer F1 form linear spaces. This, however, is not true, as we can already see by considering the trivial vector Mathematical equation which belongs to every linear space and generates an orbit with one vector – itself. Also, if linearly independent vectors Mathematical equation and Mathematical equation have the same stabilizer F1, then the stabilizer of their linear combination Mathematical equation certainly contains F1 but is not necessarily identical with it.

This means that, while all vectors of the stability space V(F1) are by definition invariant under the group F1, the group F1 is not necessarily the stabilizer of an arbitrary vector from V(F1). The set of all vectors of V(n) that have F1 as stabilizer will be called here the stratum of F1 in V(n). The stratum of F1 in a certain space V(n) can be empty. If it is not, then we find it as follows. We consider the stability space V(F1). This is never empty as it contains at least the trivial vector Mathematical equation. If the stability space is nontrivial, it is at least of dimension 1. The stratum is then the set of all vectors of V(F1) with the exception of the trivial vector. If the stability space is of higher dimension, it may contain subspaces, which are stability spaces of supergroups of F1. To get the stratum, we have to take all these stability spaces out of the space V(F1). Since these subspaces are of lower dimensions than V(F1), the stratum of F1 in V(F1) is always a dense subset of V(F1). We shall use the more customary expression that vector Mathematical equation is a general vector of the stability space V(F1) as this expression is more usual in the literature. Indeed, the vectors that do not belong to the stratum can be considered as vectors of special symmetry.

Remark

This definition of stratum is different from its use in the mathematical literature where Stratum is defined as a collection of orbits of the same type. This Stratum is therefore the union of strata as defined here for the set of conjugate subgroups and it coincides with our concept of strata for a normal subgroup. If it is necessary to use both concepts, we suggest the use of a capital S as the symbol for the original Stratum.

Kernels and epikernels: Let us now replace the set Mathematical equation by a typical carrier space Mathematical equation. If the corresponding R-irep Mathematical equation is one-dimensional, Mathematical equation, then the space Mathematical equation contains only two types of orbits:

  • (i) the trivial vector Mathematical equation, whose stabilizer under the action of G is the group G itself;

  • (ii) if Mathematical equation, then the stabilizer of this vector is the halving subgroup Mathematical equation, and, from coset resolution Mathematical equation, we obtain the second vector of the orbit which is Mathematical equation.

Notice that the set of all vectors with stabilizer Mathematical equation is the whole space Mathematical equation with the exception of the trivial vector. This set is the stratum of Mathematical equation.

If the dimension of the R-irep is at least two, we have to analyse the structure of the space Mathematical equation as follows.

  • (i) The stabilizer of the trivial vector Mathematical equation is again the group G itself.

  • (ii) The stabilizer of any other vector Mathematical equation is at least the group Mathematical equation. The index of Mathematical equation is now higher than two and we find the orbit in the usual manner. If every vector of the space has this group for its stabilizer, then we take the trivial vector out and get the typical stratum of Mathematical equation in Mathematical equation. The stratum of the group G always consists of the space V1(G) of its invariants, the stratum of G in Mathematical equation, Mathematical equation, contains only the trivial vector. In no other cases is the stratum a space.

  • (iii) There may, however, exist vectors of the space Mathematical equation, the stabilizers of which are greater than Mathematical equation. Let us assume that such a vector Mathematical equation exists. The stabilizer of this vector is called an epikernel of the R-irep Mathematical equation and we denote it by Mathematical equation. This group cannot be normal in G because normal subgroups leave invariant either all vectors or only the trivial vector in each of the spaces Mathematical equation. Epikernels therefore appear as sets of conjugate subgroups.

The stability space Mathematical equation is of the dimension Mathematical equation. If Mathematical equation, which may happen only if Mathematical equation, there may exist vectors of Mathematical equation, the stabilizer of which is greater than Mathematical equation. The dimension of the stability space of this stabilizer is smaller than Mathematical equation.

The structure of the space Mathematical equation can therefore be described as follows. A general vector of this space has the stabilizer Mathematical equation. All vectors with exactly this stabilizer form the stratum of the group Mathematical equation. This will be obtained if the trivial vector and vectors of stability spaces of epikernels are excluded from the space Mathematical equation.

Epikernels appear as sets of conjugate subgroups Mathematical equation, where the superscript u labels different sets of conjugate subgroups and the index i labels subgroups of the set. The intersections Mathematical equation of all conjugate epikernels always result in the kernel. If one epikernel Mathematical equation is a subgroup of another epikernel Mathematical equation, then the stability space Mathematical equation is a subspace of the stability space Mathematical equation. The stratum of each epikernel is therefore obtained by excluding from its stability space the trivial vector and stability spaces of all epikernels which are supergroups of this epikernel.

In Tables 1[link] and 2[link] are presented typical stability spaces of subgroups of tetragonal point groups of the oriented Laue class D4z - 4z2x2xy and epikernels of their ireps; Table 1[link] applies to those parent groups which are isomorphic to the group D4z - 4z2x2xy, Table 2[link] applies to the centrosymmetric group D4hz - 4z/mzmxmxy. As a result of our choice of ireps and standard variables, it is easy to extend these results to all groups of the oriented Laue class D4z - 4z2x2xy with the exception of the paramagnetic centrosymmetric group Mathematical equation, which must be considered separately.

Table 1
The typical stability spaces and epikernels of R-ireps for tetragonal groups isomorphic with D4z - 4z2x2xy

Parent group  
D4z C4vz D2dz Mathematical equation  
4z2x2xy 4zmxmxy Mathematical equation Mathematical equation Stability space
C4z 4z C4z 4z S4z Mathematical equation S4z Mathematical equation Mathematical equation
                 
D2 2x2y2z C2vz mxmy2z D2 2x2y2z C2vz mxmy2z Mathematical equation
                 
Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation
                 
C2z 112z C2z 112z C2z 112z C2z 112z Mathematical equation, Mathematical equation, Mathematical equation
                 
C2x 2x11 Csx mx11 C2x 2x11 Csx mx11 Mathematical equation, Mathematical equation
C2y 12y1 Csy 1my1 C2y 12y1 Csy 1my1 Mathematical equation, Mathematical equation
                 
C2xy 12xy1 Csxy 1mxy1 Csxy 1mxy1 C2xy 12xy11 Mathematical equation, Mathematical equation
Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation, Mathematical equation
                 
C1 1 C1 1 C1 1 C1 1 Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation

Table 2
The typical stability spaces and epikernels of R-ireps for the group D4hz - 4z/mzmxmxy

C4hz 4z/mz Mathematical equation
     
D2h mxmymz Mathematical equation
     
Mathematical equation Mathematical equation Mathematical equation
     
D4z 4z2x2xy Mathematical equation
     
C4vz 4zmxmxy Mathematical equation
     
D2dz Mathematical equation Mathematical equation
     
Mathematical equation Mathematical equation Mathematical equation
     
C2hz 112z/mz Mathematical equation, Mathematical equation, Mathematical equation
     
C4z 4z Mathematical equation, Mathematical equation, Mathematical equation
     
D2 2x2y2z Mathematical equation, Mathematical equation, Mathematical equation
     
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation
     
S4z Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation
     
C2vz mxmy2z Mathematical equation, Mathematical equation, Mathematical equation
     
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation
     
C2z 112z Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation
     
C2hx 2x/mx11 Mathematical equation, Mathematical equation
C2hy 12y/my1 Mathematical equation, Mathematical equation
     
C2hxy 12xy/mxy1 Mathematical equation, Mathematical equation
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation
     
Ci Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation
     
C2vx 2xmymz Mathematical equation, Mathematical equation
C2vy mx2ymz Mathematical equation, Mathematical equation
     
C2vxy Mathematical equation Mathematical equation, Mathematical equation
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation
     
Csz 11mz Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation
     
C2x 2x11 Mathematical equation, Mathematical equation, Mathematical equation, (x1+,0), (x1-,0)
C2y 12y1 Mathematical equation, Mathematical equation, Mathematical equation, (0,x1+), (0,x1-)
     
C2xy 12xy1 Mathematical equation, Mathematical equation, Mathematical equation, (x1+,x1+), (x1-,x1-)
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation, (x1+,-x1+), (x1-,-x1-)
     
Csx mx11 Mathematical equation, Mathematical equation, Mathematical equation, (x1+,0), (0,x1-)
Csy 1my1 Mathematical equation, Mathematical equation, Mathematical equation, (0,x1+), (x1-,0)
     
Csxy 1mxy1 Mathematical equation, Mathematical equation, Mathematical equation, (x1+,x1+), (x1-,-x1-)
Mathematical equation Mathematical equation Mathematical equation, Mathematical equation, Mathematical equation, (x1+,-x1+), (x1-,x1-)
     
C1 112z Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, Mathematical equation, (x1+,y1+), (x1-,y1-)

The word typical means that the information is given in terms of typical variables which can always be replaced by corresponding tensor components by the use of tables of tensorial covariants. In the two tables, we list the subgroups by both Schoenflies and Hermann–Mauguin symbols and in the right-hand column we record the corresponding stability spaces for these subgroups. If the vector in this column is framed, then the subgroup is an epikernel of that irep to whose space the tensor belongs. Notice that we can present this information in one table for the four isomorphic groups not only because of their isomorphisms but also due to our standard choice of representations and typical variables.

The framed variables correspond to primary tensor par­ameters. These are defined as those parameters whose onset is the cause of the symmetry descent. The other parameters in the same line are then the consequence of this symmetry descent and we call them the secondary tensor parameters. Some subgroups are not epikernels of any of the ireps, so that no variable is framed. Such a symmetry descent needs tensor parameters from more than one irep and we can find which parameters if we look up the groups which are epikernels and whose intersection is the considered group. This boils down to a statement that each subgroup is either itself an epikernel or an intersection of epikernels.1 The difference between stability spaces and strata in these tables is simple. The typical variables must not be zero for a stratum while stability spaces also include vectors for which these variables vanish. The use of these tables is described below.

A philosophical digression: In connection with these tables, we may question the validity of the famous statement by Curie (1884a[Curie, P. (1884a). Bull. Soc. Fr. Minéral. 7, 418-457.], p. 400, 1884b[Curie, P. (1884b). J. Phys. (Paris), 3, 393-415.]): `C'est la dissymétrie qui crée le phénomène' (`dissymmetry creates the phenomenon'). From our consideration it seems more appropriate to say that the principal tensor parameters create (are responsible for) the symmetry descent or, in other words, are the cause of the descent. Though the secondary parameters may seem to be the consequence of the descent, it seems again more appropriate to explain their onset as a consequence of faint interaction (Kopský, 1979[Kopský, V. (1979). J. Phys. A: Math. Gen. 12, L291-L294.]).

Remark

We consider it appropriate to make the following remark of historical and terminological character. Ascher (1977[Ascher, E. (1977). J. Phys. C: Solid State Phys. 10, 1365-1377.]) introduced the term epikernel [see also Kobayashi & Ascher (1977[Kobayashi, J. & Ascher, E. (1977). J. Phys. C: Solid State Phys. 10, 1349-1364.])] in connection with his study of the direct and inverse Landau problem and invented the Ker-core criterion, according to which the groups Fi are epikernels of an irep of the class Mathematical equation if and only if Mathematical equation Mathematical equation. This criterion is more comfortable than the subduction (Birman, 1966[Birman, J. L. (1966). Phys. Rev. Lett. 17, 1216-1219.]) and chain subduction criteria (Jarič, 1981[Jarič, V. (1981). Phys. Rev. 23, 3460-3463.]). Unfortunately, the terms little group or isotropy group crept into the literature instead of epikernel. In our opinion, this is taking jargon too far. A little linguistic analysis seems to be not out of place here. The older terms little group or isotropy group are now frequently replaced by the term stabilizer. The term was introduced in connection with the group action on any set. The stabilizer of a point of the set is then that subgroup which contains all those elements of the group which leave the point invariant. In this sense, an epikernel of an irep Mathematical equation is a stabilizer (little group or isotropy group) of a certain vector of the carrier space Mathematical equation under the action of the group G (it is by no means the stabilizer of its irep). In addition, the term little group (isotropy group) of an irep has its own meaning in the theory of representations of space groups, which is quite a different story.

3. Exomorphic symmetry descents

Let us consider two symmetry descents: Mathematical equation and Mathematical equation. First we construct the intersections Mathematical equation and Mathematical equation which are normal subgroups of G and Mathematical equation, respectively. If the factor groups G/H and Mathematical equation are isomorphic, then there exist homomorphisms Mathematical equation and Mathematical equation, with kernels Mathematical equation, Mathematical equation which map the groups G and Mathematical equation onto the same group Mathematical equation. If these homomorphisms also map the groups F1 and Mathematical equation onto the same subgroup Mathematical equation, then we say that the symmetry descents (group–subgroup relations) Mathematical equation and Mathematical equation are exomorphic or of the same exomorphic type. The following is a diagram of exomorphic relations.

[Scheme 1]

The exomorphism of symmetry descents has powerful consequences.

  • (i) There exists a one-to-one mapping of ireps Mathematical equation of G and Mathematical equation engendered by ireps of the factor group Mathematical equation. There also exists a one-to-one mapping of cosets Mathematical equation such that elements of these cosets act in the same way on spaces of engendered ireps. Indeed, both cosets act in the same way as the element Mathematical equation of the factor group Mathematical equation.

  • (ii) From this it follows that the stability spaces, strata and typical orbits have identical structures.

  • (iii) In addition, all polynomials in variables which belong to engendered ireps have the same transformation properties under the action of elements of corresponding cosets.

The concept was originally introduced by Kopský (1978[Kopský, V. (1978). Phys. Lett. A69, 82-84.]) for equitranslational phase transitions. In this context, we can say that the consideration of two exomorphic transitions is based on the same algebraic relations. In view of this, the classification of symmetry descents into exomorphic types facilitates systematic investigation. Thus in terms of crystallographic point groups we find 44 exomorphic types. Among them we find 28 cases when the subgroup is an epikernel of some irep, and in 5 cases out of this the subgroup is simultaneously an epikernel of two ireps. The number of distinct descents within classical crystallographic point groups is 212, within magnetic crystallographic point groups it goes up to 1599. In terms of equitranslational symmetry descents between ordinary or magnetic space groups, this number will go up into the thousands. The generalization of the concept is rather straightforward (Litvin et al., 1986[Litvin, D. B., Fuksa, J. & Kopský, V. (1986). J. Math. Phys. 27, 661-667.]).

Remark

The permutation representation of the group G on cosets of the subgroup F1 has also been used for derivation of colour groups. A later attempt to rename exomorphism as chromomorphism and a rather brutal attempt to change the usual terminology on the grounds of this fact belongs to the folklore of applications of group theory.

4. The fine structure of a typical linear orbit

We now consider again the typical stability space Vo(F1) of a subgroup F1 of the group G. This space is a direct sum of the stability spaces Mathematical equation of the group F1 in the individual typical carrier spaces Mathematical equation. We denote by Mathematical equation the stabilizer of a general vector Mathematical equation. The stability space Mathematical equation is identical with the stability space Mathematical equation and all stabilizers Mathematical equation contain the group F1. We perform the coset resolution

Mathematical equation

and the more detailed

Mathematical equation

and

Mathematical equation

which combine into

Mathematical equation

to obtain the orbit of vector Mathematical equation. This orbit contains Mathematical equation vectors Mathematical equation and splits into Mathematical equation subsets labelled by indices from the set Mathematical equation and each of these subsets contains Mathematical equation vectors Mathematical equation with fixed index i and index Mathematical equation. The vectors with the same i have the same stabilizer Mathematical equation. The numbers Mathematical equation and Mathematical equation are indices of subgroups: Mathematical equation, Mathematical equation and Mathematical equation Mathematical equation.

A vector Mathematical equation of the typical stability space Vo(F1) of the subgroup F1 generates an orbit of p = qr vectors Mathematical equation with stabilizers Fi, where p = [G:F1] = qr, where q = [G:NG(1)(F1)] and r = [NG(1)(F1):F1]. This vector splits into components Mathematical equation in the typical irreducible subspaces Mathematical equation. Each of these components has its own stabilizer Mathematical equation. Vectors Mathematical equation of the orbit also split into components Mathematical equation. While all vectors Mathematical equation of the typical orbit are distinct, the components Mathematical equation are also distinct only if Mathematical equation. Notice that this means that these components are distinct only if F1 is an epikernel of the irep Mathematical equation. On the other hand, if Mathematical equation, the number Mathematical equation of distinct components is a divisor of the total number p of vectors of the orbit; it is Mathematical equation.

If we label the components Mathematical equation by the original labels ij, then certain groups of these labels denote the same component. To label them uniquely, we use the coset resolutions associated with the stabilizer Mathematical equation which results in a certain unique labelling Mathematical equation. Each label Mathematical equation then corresponds to Mathematical equation labels ij. The set of vectors

Mathematical equation

will be called the typical linear orbit and its representation in terms of components in irreducible typical subspaces will be referred to as the fine structure of the typical linear orbit. Tables of these (under the less precise name fine domain structures and with different symbols of variables) were published a long time ago (Kopský, 1982a[Kopský, V. (1982a). Group Lattices, Subduction of Bases & Fine Domain Structures for Magnetic Point Groups. Prague: Academia.]). The original classification of symmetry descents into exomorphic classes given in this work is used below in the examples.

In Table 3[link] are shown fine structures of typical orbits for a few of the symmetry descents from a particular parent group. The advantage of typical variables is clear if we recall that tables of tensorial covariants assign to each of these variables all covariant tensor components up to fourth order (and if extension to higher orders is necessary, we know how to find it).

Table 3
Examples of the fine structure of typical orbits

Symmetry descent: Mathematical equation
Exomorphic type: 1. Mathematical equation
D4hz D2h 4zD2h
     
D2h Mathematical equation Mathematical equation
Symmetry descent: Mathematical equation
Exomorphic type: 5. Mathematical equation
D4hz C4z iC4z 2xC4z mxC4z
         
C4hz Mathematical equation Mathematical equation Mathematical equation Mathematical equation
D4z Mathematical equation Mathematical equation Mathematical equation Mathematical equation
C4vz Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Symmetry descent: Mathematical equation
Exomorphic type: 7b. Mathematical equation
First normalizer ND4hz(C2hx) = ND4hz(C2hy) = D2h = normal subgroup
D4hz D2h   4zD2h  
  C2hx 2zC2hx 4zC2hx 4z-1C2hx
         
  C2hx   C2hy  
D2h Mathematical equation Mathematical equation Mathematical equation Mathematical equation
C2hi (x1+,0) (-x1+,0) (0,x1+) (0,-x1+)
Symmetry descent: Mathematical equation        
Exomorphic type: 7a. Mathematical equation        
D4hz Csz 4zCsz 2zCsz 4z-1Csz 2xCsz 2xyCsz 2yCsz Mathematical equation
                 
C4hz Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation
D2h Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Csz (x1-,y1-) (-y1-,x1-) (-x1-,-y1-) (y1-,-x1-) (x1-,-y1-) (y1-,x1-) (-x1-,y1-) (-y1-,-x1-)
Symmetry descent: Mathematical equation  
Exomorphic type: 14b. itself  
First normalizer ND4hz(C2x) = ND4hz(C2y) = D2h = normal subgroup  
D4hz D2h       4zD2h        
  C2x iC2x 2zC2x mzC2x 4zC2x Mathematical equation 4z-1C2x Mathematical equation  
  C2x       C2y        
                   
D2h Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation  
D4 Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation  
D2dz Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation  
C2hi (x1+,0) (x1+,0) (-x1+,0) (-x1+,0) (0,x1+) (0,x1+) (0,-x1+) (0,-x1+)  
C2vi (x1-,0) (-x1-,0) (-x1-,0) (x1-,0) (0,x1-) (0,- x1-) (0,-x1-) (0,x1-)  

To attempt a more precise terminology would be appropriate at this point to connect the abstract picture provided by group theory with real physical situations and also with their models. Formation of domains at structural phase transitions is a physically established and observed fact (actually, the concept of domains appears for the first time in connection with the theory of ferromagnetic materials where group theory is dwarfed, while demagnetization fields play the main role). Quite generally, a physical observation of a symmetry descent from the state Mathematical equation of parent symmetry Mathematical equation to some state Mathematical equation of low symmetry Mathematical equation implies that the state of the system may, in the absence of special external conditions, change equally likely to any of the states Mathematical equation, where gi are coset representatives in the coset resolution

Mathematical equation

The states Mathematical equation are called the domain states. It is usually said that the domain states Mathematical equation are symmetrically equivalent. It is probably more precise to say that all relationships of the original state Mathematical equation to any of the states Mathematical equation are mutually geometrically equivalent and hence physically equivalent. Indeed, any element of Mathematical equation leaves the original state Mathematical equation invariant and the change of the relationship between the state Mathematical equation and Mathematical equation to the relationship between the state Mathematical equation and Mathematical equation is obtained by applying an element of gjF1 to both states. The effect of this operation is the rotation and, in full structural considerations, also the possible space shift of the situation in physical space.

The state of the crystal at the transition usually does not change to any particular state Mathematical equation. The crystal splits instead into regions, called domains, and the state in each of the domains is one of the domain states. In addition, if the transition is ferroelastic, the domain states coincide with those predicted by coset resolution only in the vicinity of the transitions point (so-called parent clamping approximation). Ferroelastic phase transitions play a special role in the theory of domains for the following reason: the domain states are eventually realized in the individual domains. The structures of a crystal, which correspond to various domain states, are identical up to their orientation and location in the space. Domains are therefore regions of physical space occupied by such states and there exist interfaces (boundaries) between these regions. Group theory predicts the equivalence of the number of domain states equal to the index [Mathematical equation] of the low symmetry to the parent symmetry. In reality, only two domains can meet at an interface of a certain orientation and location. From group-theoretical analysis, we may predict possible mutual orientations and locations of pairs of respective domain states and continue the analysis for any orientation and location of an interface. However, in the case of ferroelastic phase transitions, there exist physical conditions on the existence of interfaces – the boundary between two domains should be stress free. As a result, the mutual orientation and location of domain states coincides with that predicted by group theory only when spontaneous distortions of the structure are small.

In the examples Mathematical equation, Mathematical equation and Mathematical equation, we can observe that each domain state corresponds to a distinct vector in one of the typical spaces. There are the variables or vectors Mathematical equation, (x1+,0) and (x1-,y1-) in the first domain state, which change from one domain to the other, so that all domains are characterized by distinct vectors. In the case of descents Mathematical equation, Mathematical equation, we need to take vectors of two ireps to distinguish all domain states.

5. Labelling of covariants and conversion equations

Substituting actual tensor components for typical variables in the tables of the fine structure of typical orbits, we obtain as complete a description of all domain states in terms of their tensor properties as the tables of tensorial covariants provide. If this turns out not to be sufficient, we can always extend the tables of tensorial covariants to higher ranks.

However, if we inspect tables of covariants or if we try an actual substitution, we shall find that typical variables are substituted by covariant tensor components which are frequently linear combinations of Cartesian components. It is therefore necessary to convert this information into the Cartesian frame of reference. The situation is analogous to the consideration of invariant tensor forms. Invariants are frequently linear combinations of Cartesian components and, as a result, we obtain an invariant tensor in the Cartesian frame which has more allowed components than the number of independent invariants. In this case, there appear relations between the Cartesian components which reduce the number of independent components to the correct one.

The effect in ferroic transitions is that Cartesian components are not necessarily the principal parameters and there appear increments to these components which are again not independent. To resolve this problem, we introduce the method of labelling the covariants and of conversion equations (Kopský, 2001a[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.],b[Kopský, V. (2001b). Ferroelectrics, 252, 21-30.],c[Kopský, V. (2001c). Ferroelectrics, 252, 51-58.]), which was later used by Janovec & Kopský (2003[Janovec, V. & Kopský, V. (2003). International Tables for Crystallography, Vol. D, section 3.1.3, Equitranslational Phase Transitions. Property Tensors at Ferroic Phase Transitions, pp. 350-361. Dordrecht: Kluwer Academic Publishers. ]).

The method is illustrated in Table 4[link] for the tetragonal group D4z. Table 4[link](a) defines the labels of covariants as linear combinations of Cartesian components and Table 4[link](b) gives the Cartesian components expressed as linear combinations of covariant components. The principles of notation are explained below. It is our opinion that it would be useful to standardize the labels of covariants.

Table 4
Labelling of covariants and conversion equations: Group 4z2x2xy – (D4z)

(a) Labelling of covariants

Mathematical equation   Mathematical equation Mathematical equation
Mathematical equation   Mathematical equation  
       
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
  Mathematical equation Mathematical equation Mathematical equation
  Mathematical equation    
       
Mathematical equation   Mathematical equation  
Mathematical equation   Mathematical equation  
    Mathematical equation  
       
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Mathematical equation   Mathematical equation Mathematical equation
Mathematical equation   Mathematical equation Mathematical equation
Mathematical equation      
Mathematical equation   Mathematical equation  
Mathematical equation   Mathematical equation  
    Mathematical equation  
    Mathematical equation  
       
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
  Mathematical equation Mathematical equation Mathematical equation
       
    Mathematical equation  
    Mathematical equation  
    Mathematical equation  
    Mathematical equation  

(b) Conversion equations

Mathematical equation Mathematical equation Mathematical equation  
u4 = u1x u5 = -u1y Mathematical equation  
       
A11 = A1x,1 A22 = A1y,1 A12 = A1x,2 A21 = A1y,2
A13 = A1x,3 A23 = A1y,3 A26 = A1x,4 A16 = A1y,4
A35 = A1x,5 A34 = A1y,5 Mathematical equation Mathematical equation
  Mathematical equation Mathematical equation  
  Mathematical equation Mathematical equation  
  Mathematical equation Mathematical equation  
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
Mathematical equation Mathematical equation Mathematical equation Mathematical equation Mathematical equation
s14 = s1x,1 s25 = -s1y,1 s24 = s1x,2 s15 = -s1y,2
s34 = s1x,3 s35 = -s1y,3 s56 = s1x,4 s46 = -s1y,4
Mathematical equation Mathematical equation Mathematical equation Mathematical equation
  Mathematical equation Mathematical equation Mathematical equation
q14 = q1x,1 q25 = -q1y,1 q24 = q1x,2 q15 = -q1y,2
q34 = q1x,3 q35 = -q1y,3 q56 = q1x,4 q46 = -q1y,4

To each group there are assigned two tables. The first table, called `Labelling of covariants' assigns numerical labels to linearly independent Mathematical equation covariants in the case when more than one covariant of a given tensor to this irep exists. We shall illustrate it for the case of tensor Mathematical equation. One-dimensional covari­ants, including invariants, are denoted by sans-serif letter Mathematical equation with two indices, the first of which is the numerical label of an irep, the second is the number of the covariant. If only one covariant of the type exists, we drop the second index. Thus, Mathematical equation means an invariant, Mathematical equation means a Mathematical equation covari­ant but Mathematical equation, Mathematical equation, Mathematical equation mean the first, second and third invariants and Mathematical equation, Mathematical equation mean the first and second Mathematical equation covariants. The two-dimensional D(1)(G) covariants are expressed as Mathematical equation, Mathematical equation, Mathematical equation and so on if more than three linearly independent D(1)(G) covariants exist while Mathematical equation signals that there is no other D(1)(G) covariant.

The second table bears the title `Conversion equations' and contains Cartesian tensor components expressed in terms of the covariant components. If all non-invariant components are set to zero, we get the tensor form, invariant under the group G. By comparison with the main tables, we can see which covariant components onset at each transition from the parent group G. Thus these components can be described as the tensor parameters of the transition. Conversion equations are a convenient platform to launch the detailed investigation of domain pairs and domain walls. The results of such an investigation in a form which an experimentalist can directly use are in preparation as a continuation of this work.

Example: Using the conversion Table 4[link] for the group D4z - 4z2x2xy and Table 1[link] of stability spaces and epikernels, find how the Cartesian components of the piezoelectric tensor Mathematical equation change as we descend with the symmetry (on various paths) to trivial symmetry C1 -1.

First we take into account that tensor Mathematical equation transforms in this group in the same way as tensor Mathematical equation for which labelling of covariants and conversion equations are listed. We just replace the characters A and Mathematical equation by d and Mathematical equation.

In the group D4z - 4z2x2xy, we find that only two components are nonvanishing: Mathematical equation and equal to one invariant with opposite signs.

In the group C4z - 4z, variable Mathematical equation onsets to which there correspond Cartesian components Mathematical equation, Mathematical equation and Mathematical equation.

To the group D2 - 2x2y2z there corresponds variable Mathematical equation which indicates onset of the component Mathematical equation. The covariant Mathematical equation contributes to already allowed components by Mathematical equation. Owing to this increment, the components d14 and d25 are now independent.

To the group Mathematical equation there corresponds variable Mathematical equation which contributes to Cartesian components by Mathematical equation and Mathematical equation. These Cartesian components are not independent because of the orientation of this group.

All three variables Mathematical equation, Mathematical equation, Mathematical equation are invariant under the group C2z and hence all components d14, d25, d31, d32, d15 and d24 are independent and can be expressed through two consecutive increments as seen from conversion equations.

In the group C2x - 2x, we obtain again the increments Mathematical equation to components already allowed in the parent group. In addition, the first component (x1,0) is now allowed, to which there corresponds an onset of tensor components: d11 = d1x,1, d13 = d1x,3, d35 = d1x,5, d12 = d1x,2 and d26 = d1x,4.

In the group C2y - 2y, we obtain again the increments Mathematical equation to components already allowed in the parent group. In addition, the second component (0,x1) is now allowed, to which there corresponds an onset of tensor components: d22 = d1y,1, d23 = d1y,3, d34 = d1y,5, d21 = d1y,2 and d16 = d1y,4. The magnitude of these components must be the same as that of corresponding components in the group C2x - 2x, because the state is actually another domain state of the same descent.

In the groups C2xy - 2xy and Mathematical equation, we obtain Cartesian components Mathematical equation and Mathematical equation. Vector (x1,x1) indicates that in the group C2xy - 2xy we obtain d11 = d22, d13 = d23, d35 = d34, d12 = d21 and d26 = d16, while, in the other group Mathematical equation, d11 = -d22, d13 = -d23, d35 = -d34, d12 = -d21 and d26 = -d16.

We have to check now that all these components taken together are all components of tensor Mathematical equation as it should be in the trivial group C1 - 1.

Conversion equations are not necessary for parent groups up to mxmymz - D2h because Cartesian components are themselves relative invariants (this is, however, due to the choice of group orientations). Labelling of covariants and solution of conversion equations for other tensors and for other groups can be performed by rewriting results for groups of proper rotations with the use of Opechowski's magic relations (Kopský, 2006a[Kopský, V. (2006a). Z. Kristallogr. 221, 51-62.]).

6. The twinning group and completely transposable pairs of domain states

The original tables of the fine structure of domain states (Kopský, 1982a[Kopský, V. (1982a). Group Lattices, Subduction of Bases & Fine Domain Structures for Magnetic Point Groups. Prague: Academia.]) have now been revised because some of the original numerical labels of ireps were changed to a more systematic labelling. With their use and with the use of conversion equations, we are able to describe all domain states by desirable tensors. This might be useful, for example, in averaging domain states of engineered multidomain structures with certain weights as well as in the determination of tensor distinction of domain states.

In consideration of domain walls or twin boundaries, we consider only pairs of domain states because only two domains meet at the wall. Here we are interested in the tensor distinction of pairs of domain states. Domain walls, pairs of domain states and their tensor distinction were extensively studied by Janovec and others (Janovec et al., 1992[Janovec, V., Richterová, L. & Litvin, D. B. (1992). Ferroelectrics, 126, 287-292.], 1993[Janovec, V., Richterová, L. & Litvin, D. B. (1993). Ferroelectrics, 140, 95-100.], 1994[Janovec, V., Litvin, D. B. & Richterová, L. (1994). Ferroelectrics, 157, 75-80.], 1995[Janovec, V., Litvin, D. B. & Fuksa, J. (1995). Ferroelectrics, 172, 351-359.]; Fuksa & Janovec, 1995[Fuksa, J. & Janovec, V. (1995). Ferroelectrics, 172, 343-350.]; Fuksa, 1997[Fuksa, J. (1997). Ferroelectrics, 204, 135-155.]). In this connection, the concept of the embracing group or fundamental group of dichromatic pattern (Shubnikov & Kopcik, 1974[Shubnikov, A. V. & Kopcik, V. A. (1974). Symmetry in Science and Art. New York: Plenum Press.]; Pond & Vlachavas, 1983[Pond, R. C. & Vlachavas, V. A. (1983). Proc. R. Soc. London Ser. A, 386, 95-143.]; Wadhawan, 2000[Wadhawan, H. (2000). Introduction to Ferroic Materials. Amsterdam: Gordon and Breach.]) introduced originally as a bicrystallographic construction has been given the better name of the twinning group (cf. Litvin & Kopský, 1997[Litvin, D. B. & Kopský, V. (1997). Ferroelectrics, 204, 217-223.], on magnetic twins; Janovec, Hahn & Klapper, 2003[Janovec, V., Hahn, T. & Klapper, H. (2003). International Tables for Crystallography, Vol. D, section 3.2, Twinning and Domain Structures, pp. 377-392. Dordrecht: Kluwer Academic Publishers.]; Janovec & Přívratská, 2003[Janovec, V. & Přívratská, J. (2003). International Tables for Crystallography, Vol. D, section 3.4, Domain Structures, pp. 449-502. Dordrecht: Kluwer Academic Publishers.]).

The twinning group: To study the distinction of the tensorial properties of a pair of domain states Mathematical equation, it is frequently not necessary to know the symmetry descent Mathematical equation or the whole set of domain states. It is sufficient to find an element g which sends the state Mathematical equation into the state Mathematical equation. The twinning group Mathematical equation is defined as the group generated by the symmetry of the first state and an element g which sends it to the second state.

The next two Tables 5[link] and 6[link] refer to parent groups D4z - 4z2x2xy and Mathematical equation. Separated by blank lines are symmetry descents to subgroups of these two groups (in the second case only the descents of low index are given). Under each of the subgroups are listed representatives of cosets in the coset resolution of the parent group. The elements of each coset send the first domain state to another distinct domain state. The twinning group is given in the right column.

Table 5
Twinning groups for pair of domain states in symmetry descents from the parent group D4z - 4z2x2xy

Parent group Twinning group
4z (C4z)  
2x Mathematical equation [Mathematical equation]
   
2x2y2z (D2)  
Mathematical equation Mathematical equation [Mathematical equation]
   
Mathematical equation (Mathematical equation)  
2x Mathematical equation [Mathematical equation]
   
2z (C2z)  
2x Mathematical equation [Mathematical equation]
2xy Mathematical equation [Mathematical equation]
4z Mathematical equation [Mathematical equation]
   
2x (C2x)  
2z Mathematical equation [Mathematical equation]
2xy 4z2x2xy (D4z)
Mathematical equation
   
2xy (C2xy)  
2z Mathematical equation [Mathematical equation]
2x 4z2x2xy (D4z)
2y
   
1 (C1)  
2z Mathematical equation [Mathematical equation]
2x Mathematical equation [Mathematical equation]
2y Mathematical equation [Mathematical equation]
2xy Mathematical equation [Mathematical equation]
Mathematical equation Mathematical equation [Mathematical equation]
4z 4z (C4z)
4z3

Table 6
Twinning groups for pair of domain states in symmetry descents of low index from the parent group Mathematical equation

Parent group Twinning group
Mathematical equation (Th)  
mxy Mathematical equation [Mathematical equation]
   
432 (O)  
i Mathematical equation [Mathematical equation]
   
Mathematical equation (Td)  
i Mathematical equation [Mathematical equation]
   
23 (T)  
i Mathematical equation [Mathematical equation]
2xy Mathematical equation [Mathematical equation]
mxy Mathematical equation [Mathematical equation]
   
4z/mzmxmxy (D4hz)  
myz Mathematical equation (Oh)
mzx
   
mxmymz (D2h)  
mxy Mathematical equation [Mathematical equation]
myz Mathematical equation [Mathematical equation]
mzx Mathematical equation [Mathematical equation]
3p Mathematical equation (Th)
3p2
   
4z/mz (C4hz)  
mx Mathematical equation [Mathematical equation]
mzx Mathematical equation (Oh)
Mathematical equation
myz
Mathematical equation

We shall consider here only the case of so-called completely transposable pairs of domain states which have the property that from Mathematical equation follows Mathematical equation. In this case, the two states have the same symmetry which is a halving subgroup of the twinning group T. This leads to a notation in the style of magnetic point groups: some generators in the symbol of the twinning group are starred in the Hermann–Mauguin symbols, in Schoenflies symbols the star is attached to the symbol of T and the subgroup F1 is specified in parentheses. All elements of the coset Mathematical equation transpose the domain states Mathematical equation and Mathematical equation. The tensor properties of the two states are the same for those tensor components that are invariant under the group T, they differ in sign for those components that correspond to symmetry descent Mathematical equation. This descent may not be the actual symmetry descent Mathematical equation at which the two domain states arise and tensor components by which the states differ may belong to an irep of G which is not one-dimensional. On the other hand, this means that an experiment that leads to such a pair of states does not necessarily imply the actual symmetry descent. If Mathematical equation, which implies Mathematical equation, this may need the knowledge of a wider set of domain states.

Although the concept of the twinning group is useful for classification purposes and in cases of twinning, it is not quite necessary in the determination of the tensor distinction of domain states where tables of fine structure of domain states in conjunction with the `Main Tables' of tensor parameters of the first domain state in ferroic symmetry descents [Kopský (2001a[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.]), and GIMathematical equationKoBo-1 (Kopský & Boček (2003[Kopský, V. & Boček, P. (2003). GIKoBo-1 (Group Informatics, release 1). CD ROM Supplement to International Tables for Crystallography, Vol. D.])] provide more complete information. Thus in Table 3.4.3.4. of section 3.4 of International Tables for Crystallography (2003[International Tables for Crystallography (2003). Vol. D, Physical Properties of Crystals, edited by A. Authier. Dordrecht: Kluwer Academic Publishers. ], Vol. D, pp. 478–479) are given only the numbers of components of tensors Mathematical equation (enantiomorphism), Mathematical equation (polarization), g (gyrotropy), d (piezoelectricity), A (electrogyrotropy), s (elastic stiffness) and Q (elastooptics) in which pairs of domain states of completely transposable domain pairs differ. In an example below, we show the difference between the full analysis and a shortcut provided by the twinning group.

Example: We consider the transition Mathematical equation or, in Hermann–Mauguin notation, Mathematical equation. The principal parameters for the first domain state Mathematical equation with symmetry C4hz  (4z/mz) can be found on page 381 of the paper by Kopský (2001a[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.]) as covari­ant tensor components corresponding to variable z1+. These are A33, A32+A31, A24+A15, s26-s16, Q26-Q16, Q62-Q61, Q45-Q54 = q45. Secondary tensor parameters correspond to typical vector (x3+,0). Twinning operation mx sends the vector (0,0,z1+) to (0,0,-z1+) and leaves the vector (x3+,0) intact. The pair of domain states Mathematical equation, where Mathematical equation, is completely transposable and the corresponding twinning group is Mathematical equation. On page 165 of the same work[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.], we find tensor parameters in which the two domain states differ as A33, A32+A31, A24+A15, s26-s16, Q26-Q16, Q62-Q61, Q45-Q54 = q45, i.e. we get the same result as before without the use of the twinning group. If we look up the subduction tables, which were given together with fine structures of domain states, we find that the variable z+1 in the group Mathematical equation subduces the variable Mathematical equation which is to be replaced by these tensor parameters in the group C4hz - 4z/mz.

With the use of conversion equations, we find that the transition is accompanied by an onset of Cartesian components A33, A32 = -A31, A24 = -A15, s26 = s16, Q26 = Q16, Q26 = Q16 and q45 which change their sign if we go from the domain state Mathematical equation to the state Mathematical equation. Thus we can obtain explicitly those tensor parameters in which the domain states differ as well with the use of the twinning group as without it. On the other hand, the table on page 381 of the cited work[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.] provides as easily the information about the other two pairs of domain states which correspond to typical variables x1+ and y1+ and to symmetries C4hx - 4x/mx and C4hy - 4y/my. The first pair is distinguished by tensor components A11, A13 = -A12, A35 = -A26, s34 = s24, Q34 = Q24, Q43 = Q42 and q56, the second by components A22, A21 = -A23, A16 = -A34, s15 = s35, Q15 = Q35, Q51 = Q53 and q64. Thus we obtain a complete description of the distinction of the six domains with covariant as well as Cartesian components of tensors A, s and Q (q is the antisymmetric part of Q).

In addition, we can also obtain the information about the secondary parameters which correspond to variables, transforming by the irep D(3+)(Oh), where the domain states are characterized by tensor parameters corresponding to states (x3+,0), (-ax3+-by3+,bx3+-ay3+) and (-ax3++by3+,-bx3+-ay3+). These states correspond to symmetries D4hz - 4z/mzmxmxy, D4hx - 4x/mxmymyz and D4hy - 4y/mymzmzx. With the use of conversion equations, we can find the distinction of pairs of domain states that belong to different choices of these symmetries in terms of those components of tensors u, A, s and Q which appear in the block, corresponding to the first state with the symmetry D4hz - 4z/mzmxmxy.

Thus the twinning group is only of auxiliary value in cases when we need to consider only a certain pair of domain states. Complete description of domain states in terms of tensors up to fourth rank may be obtained from the `Main tables' [Kopský (2001a[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.]) or GIMathematical equationKoBo-1 (Kopský & Boček, 2003[Kopský, V. & Boček, P. (2003). GIKoBo-1 (Group Informatics, release 1). CD ROM Supplement to International Tables for Crystallography, Vol. D.])] and from tables of the fine structure of domain states. An experienced user can even bypass the use of the latter tables because the transformations of the typical variables do not go beyond the action of symmetry operations on two- or three-dimensional spaces. The essential points of an analysis of tensor properties of domain states are the decomposition of the tensor into tensorial covariants and the conversion equations.

7. Discussion

It's a long way to Tipperrary! Indeed, let us recall the steps of this version of tensor calculus and its outcome. We begin with meticulous specification of magnetic point groups and their isomorphisms. Precise specification of typical variables is a central point of systemization while the Clebsch–Gordan products represent the background for calculation of tensorial covariants or rather of the decomposition of tensors into these covariants. The choice of isomorphisms and of symbols for typical variables together with Opechowski's magic relations maximally simplify this task and cut down the tedious part of calculations to a minimum.

The knowledge of tensorial covariants is itself a starting point for the investigation of ferroic phase transitions, especially for the consideration of tensor properties of individual domain states which is necessary in modelling the properties of multidomain systems. The typical variables also prove to be useful in this application. With their use in tables of stability spaces and epikernels, we establish the quantities that characterize the first domain and in tables of fine structure of domain states we find complete information about these states. Up to orthorhombic parent groups, we do not need such a sophisticated scheme because the ireps are one-dimensional and tensorial covariants (relative invariants in these cases) coincide with Cartesian components. Starting with tetragonal parent groups, we meet, however, the difference between transition parameters and Cartesian tensor components. There are two options for resolving this discrepancy. We may obtain the results in terms of Cartesian tensor components using the procedure of labelling the covariants with subsequent transformation of results to Cartesian system through conversion equations. It would be, however, also possible to express the experimental results directly in terms of covariant components.

One of the problems of the practical use not only of this theory but also of the tables by experimentalists is the necessity of learning a certain minimal pensum of group theory such as given in this work. Tables are of no use if one does not know what information they contain. Let me, however, give an example that shows that learning at least the basic principles is worth the time. A recognized experimentalist asked me recently whether it is in order if he uses the relation Mathematical equation where Mathematical equation are the matrices of vector transformation to calculate the changes of tensor s from one domain state to another. Like the method of projection operators to find tensorial bases, this is theoretically correct. But in practice? With 21 components of the tensor s and up to 48 domain states? Would it not be more productive to spend the time necessary for such error-prone calculations by learning the basic principles of the theory of irreducible representations? Indeed, the principle behind our system is the same as used in spectroscopy. Using covariant tensor components we split the space of dimension 21 to subspaces whose maximal dimension is 3.

All information necessary to find tensor characteristics of individual domain states up to tensors of fourth rank and for the ordinary point groups is contained in the monograph by Kopský (2001a[Kopský, V. (2001a). Phase Transit. 73, Nos. 1-2 (Special issue), pp. 1-422.]) and in the software GIMathematical equationKoBo-1 (Kopský & Boček, 2003[Kopský, V. & Boček, P. (2003). GIKoBo-1 (Group Informatics, release 1). CD ROM Supplement to International Tables for Crystallography, Vol. D.]). Explicit tabulation of analogous results for magnetic point groups and magnetic properties in printed form is out of the question as well as the tabulation of the final results because of the volume required. On the other hand, the volume of basic tables from which desired information can be derived is relatively small and algorithms for its derivation rather transparent. We are preparing an extension of the software GIMathematical equationKoBo-1 (Kopský & Boček, 2003[Kopský, V. & Boček, P. (2003). GIKoBo-1 (Group Informatics, release 1). CD ROM Supplement to International Tables for Crystallography, Vol. D.]) which will provide explicit results for magnetic point groups and magnetic properties with the hope that it will be helpful to experimentalists.

Supporting information


Footnotes

1Analogous tables for other oriented Laue classes are available from the IUCr electronic archives (Reference: XO5008 ). Services for accessing these data are described at the back of the journal.

Acknowledgements

This work is part of project AVO 10100520 of the Czech Academy and has been supported by grant No. 202/04/0992 of the Czech Grant Agency. Thanks are due to Professor M. Nespolo, who gave the author the opportunity to present the results in lectures at the Summer School of the MathCryst group in Nancy, and to the French Embassy in Prague (Service de coopération et d'action culturelle) for generous support of local expenses as well as to my friend Professor D. B. Litvin who took care of the accommodation.

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