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. 3.2, pp. 377392
doi: 10.1107/97809553602060000643 Chapter 3.2. Twinning and domain structures^{a}Department of Physics, Technical University of Liberec, Hálkova 6, 461 17 Liberec 1, Czech Republic,^{b}Institut für Kristallographie, Rheinisch–Westfälische Technische Hochschule, D52056 Aachen, Germany, and ^{c}MineralogischPetrologisches Institut, Universität Bonn, D53113 Bonn, Germany This chapter forms the introduction to the treatment of twinning in Chapter 3.3 and of domain structures in Chapter 3.4 . It starts with a historical overview of twinning (beginning with a paper by Romé de l'Isle from 1783) and continues with the history of the various forms of domain structures: ferromagnetism, ferroelectricity and ferroelasticity, summarized as ferroic by Aizu in 1970. This historical survey is followed by a brief excursion into the rather new field of bicrystallography and grain boundaries. The major part of the chapter is concerned with an extended exposition of the mathematical tools needed in the subsequent parts, especially in Chapter 3.4 . One section introduces the basic concepts of set theory and explains the notion of unordered and ordered pairs, mappings of sets and the partition of a set into equivalence classes. The next section deals with basic group theory and is devoted mainly to group–subgroup relations and relevant notions, of which blackandwhite and colour groups and coset decompositions of a group into left and double cosets are of central importance. In the final section, group theory is combined with set theory in the `action of a group on a set' which represents an effective algebraic tool for the symmetry analysis of domain structures. The notions of stabilizer, orbit and stratum are explained and their significance in the analysis is illustrated by concrete examples. 
Twins have been known for as long as mankind has collected minerals, admired their beauty and displayed them in museums and mineral collections. In particular, large specimens of contact and penetration twins with their characteristic reentrant angles and simulated higher symmetries have caught the attention of mineral collectors, miners and scientists. Twinning as a special feature of crystal morphology, therefore, is a `child' of mineralogy, and the terms and symbols in use for twinned crystals have developed during several centuries together with the development of mineralogy.
The first scientific description of twinning, based on the observation of reentrant angles, goes back to Romé de l'Isle (1783). Haüy (1801) introduced symmetry considerations into twinning. He described hemitropes (twofold rotation twins) and penetration twins, and stated that the twin face is parallel to a possible crystal face. Much pioneering work was done by Weiss (1809, 1814, 1817/1818) and Mohs (1822/1824, 1823), who extended the symmetry laws of twinning and analysed the symmetry relations of many twins occurring in minerals. Naumann (1830) was the first to distinguish between twins with parallel axes (Zwillinge mit parallelen Achsensystemen) and twins with inclined (crossed) axes (Zwillinge mit gekreuzten Achsensystemen), and developed the mathematical theory of twins (Naumann, 1856). A comprehensive survey of the development of the concept and understanding of twinning up to 1869 is presented by Klein (1869).
At the beginning of the 20th century, several important mineralogical schools developed new and farreaching ideas on twinning. The French school of Mallard (1879) and Friedel (1904) applied the lattice concept of Bravais to twinning. This culminated in the lattice classification of twins by Friedel (1904, 1926) and his introduction of the terms macles par mériédrie (twinning by merohedry), macles par pseudomériédrie (twinning by pseudomerohedry), macles par mériédrie réticulaire [twinning by reticular (lattice) merohedry] and macles par pseudomériédrie réticulaire (twinning by reticular pseudomerohedry). This concept of twinning was very soon taken up and further developed by Niggli in Zürich, especially in his textbooks (1919, 1920, 1924, 1941). The lattice theory of Mallard and Friedel was subsequently extensively applied and further extended by J. D. H. Donnay (1940), and in many later papers by Donnay & Donnay, especially Donnay & Donnay (1974). The Viennese school of Tschermak (1904, 1906), Tschermak & Becke (1915), and Tertsch (1936) thoroughly analysed the morphology of twins, introduced the Kantennormalengesetz and established the minimal conditions for twinning. The structural and energy aspects of twins and their boundaries were first accentuated and developed by Buerger (1945). Presently, twinning plays an important (but negative) role in crystal structure determination. Several sophisticated computer programs have been developed that correct for the presence of twinning in a small single crystal.
A comprehensive review of twinning is given by Cahn (1954); an extensive treatment of mechanical twinning is presented in the monograph by KlassenNeklyudova (1964). A tensor classification of twinning was recently presented by Wadhawan (1997, 2000). Brief modern surveys are contained in the textbooks by Bloss (1971), Giacovazzo (1992) and Indenbom (see Vainshtein et al., 1995), the latter mainly devoted to theoretical aspects. In previous volumes of International Tables, two articles on twinning have appeared: formulae for the calculation of characteristic twin data, based on the work by Friedel (1926, pp. 245–252), are collected by Donnay & Donnay in Section 3 of Volume II of the previous series (Donnay & Donnay, 1972), and a more mathematical survey is presented by Koch in Chapter 1.3 of Volume C of the present series (Koch, 2004).
Independently from the development of the concept of twinning in mineralogy and crystallography, summarized above, the concept of domain structures was developed in physics at the beginning of the 20th century. This started with the study of ferromagnetism by Weiss (1907), who put forward the idea of a molecular field and formulated the hypothesis of differently magnetized regions, called ferromagnetic domains, that can be switched by an external magnetic field. Much later, von Hámos & Thiessen (1931) succeeded in visualizing magnetic domains by means of colloidal magnetic powder. For more details about magnetic domains see Section 1.6.4 of the present volume.
In 1921, Valasek (1921) observed unusual dielectric behaviour in Rochelle salt and pointed out its similarity with anomalous properties of ferromagnetic materials. This analogy led to a prediction of `electric' domains, i.e. regions with different directions of spontaneous polarization that can be switched by an electric field. Materials with this property were called Seignette electrics (derived from the French, `sel de Seignette', denoting Rochelle salt). The term seignettoelectrics is still used in Russian, but in English has been replaced by the term ferroelectrics (Mueller, 1935). Although many experimental and theoretical results gave indirect evidence for ferroelectric domain structure [for an early history see Cady (1946)], it was not until 1944 that Zwicker & Scherrer (1944) reported the first direct optical observation of the domain structure in ferroelectric potassium dihydrogen phosphate (KDP). Four years later, KlassenNeklyudova et al. (1948) observed the domain structure of Rochelle salt in a polarizing microscope (see KlassenNeklyudova, 1964, p. 27). In the same year, Blattner et al. (1948), Kay (1948) and Matthias & von Hippel (1948) visualized domains and domain walls in barium titanate crystals using the same technique.
These early studies also gave direct evidence of the influence of mechanical stress and electric field on domain structure. Further, it was disclosed that a domain structure exists only below a certain temperature, called the Curie point, and that the crystal structures below and above the Curie point have different pointgroup symmetries. The Curie point thus marks a structural phase transition between a paraelectric phase without a domain structure and a ferroelectric phase with a ferroelectric domain structure. Later, the term `Curie point' was replaced by the more suitable expression Curie temperature or transition temperature.
The fundamental achievement in understanding phase transitions in crystals is the Landau theory of continuous phase transitions (Landau, 1937). Besides a thermodynamic explanation of anomalies near phase transitions, it discloses that any continuous phase transition is accompanied by a discontinuous decrease of crystal symmetry. In consequence, a phase with lower symmetry can always form a domain structure.
The basic role of symmetry was demonstrated in the pioneering work of Zheludev & Shuvalov (1956), who derived by simple crystallographic considerations the point groups of paraelectric and ferroelectric phases of all possible ferroelectric phase transitions and gave a formula for the number of ferroelectric domain states.
A mechanical analogy to ferroelectric domains exists in the form of domains that differ in strain and can be switched by mechanical stress. This effect was studied under the name `twinning with change of form' in the monoclinic ferroelectric phase of Rochelle salt by KlassenNeklyudova et al. (1948) and Chernysheva (1950). A detailed description of this work in English is presented by KlassenNeklyudova (1964, pp. 27–30, 75–78) in her monograph on mechanical twinning of crystals. Indenbom (1960) has shown that such behaviour is not confined to ferroelectric crystals and has listed many symmetry changes of potential phase transitions accompanied by the appearance of a spontaneous strain that could give rise to domains with different strain. Aizu (1969) called such crystals ferroelastic crystals in analogy with ferroelectric crystals. Ferroelastic domains differ in spontaneous strain and can be switched by mechanical stress.
Generalization of the concepts of ferromagnetic, ferroelectric and ferroelastic crystals followed soon after (Aizu, 1970): A ferroic crystal has two or more orientation states (oriented bulk structures of domains) that can be switched by means of a magnetic field, an electric field, a mechanical stress or by a combination of these. Ferroic domains are distinct in some tensors describing the material properties of the crystal. Aizu has also shown that the type of domain structure is determined by the change of pointgroup symmetry at the structural phase transition from a prototypic (parent, highsymmetry) phase without domains to a ferroic (distorted, lowsymmetry, daughter) phase in which domains appear.
A more detailed history of the research of ferromagnetic, ferroelectric, ferroelastic and ferroic materials in general can be found in the book by Wadhawan (2000).
The domain structure determines to a certain extent electric, elastic, electromechanical and other properties of ferroic crystals. The investigation of domain structures has thus become an inseparable part of the research of ferroelectrics, ferroelastics and ferroic crystalline materials in general.
Most of the work has been devoted to ferroelectrics, since their specific properties have found important applications, some of which (e.g. production of anisotropic ceramics, ferroelectric memories) are based on irreversible and hysteretic changes of the ferroelectric domain structure under an electric field. References to ferroelectric, ferroelastic and other domain structures are given at the end of Section 3.4.1 .
Even though the basic concepts of twinning and domain structures are closely related and have many aspects in common, the study of both subjects has developed independently, using different terms and symbols to describe rather similar facts. There are many cases that can be treated equally well by both approaches, e.g. merohedral twins and nonferroelastic domain structures. There are cases, however, which can only be understood with one of the two concepts, e.g. the (111) spinel twins cannot be interpreted as a domain structure, because a highsymmetry parent phase does not exist. Of the two topics, twinning is the older, whereas the younger topic domain structure has recently advanced to a more detailed physical understanding.
In the two following chapters, 3.3 and 3.4 , the two topics are treated separately and in their own right. It will be apparent that the two approaches, despite the great similarity of their objects, are quite different: for domain structures the allimportant theoretical basis is the existence of a – real or potential (hypothetical) – parent (prototypic) phase from which the ferroic (distorted) phase is derived. This lowering of symmetry, expressed by a group–subgroup relation between the symmetries of the parent and ferroic phases, is the source of an impressive theoretical edifice which allows the explanation, and even the prediction, of many crystallographic properties of a given domain structure.
The situation is different in twinning: whereas transformation twins are closely related to domain structures and hence can be treated with the same theoretical tools, many growth twins and mechanical twins are characterized by the absence of an existing – and even a hypothetical – parent structure. From this it follows that growth and mechanical twins (which are the typical twin specimens of mineral collections) are to a much lesser extent amenable to grouptheoretical analysis. Instead, each twinning case must be considered separately, and the orientation and contact relations of the twin partners must be individually ascertained. This requires discussion of many `type cases'.
The present chapter continues with a short excursion into bicrystallography (Section 3.2.2), a topic not treated further in this article, followed by Section 3.2.3 with an exposition of basic concepts of set theory and group theory needed in Chapters 3.3 and 3.4 .
Both twinning and domain structures appear to be special cases of the relatively young research field of bicrystallography (Pond & Vlachavas, 1983), which has its origin in the study of grain boundaries in metals. Grains are coexisting crystals with identical composition and structure but with different orientations. Coexisting grains can be formally treated as generalized twins in which one of the conditions (viz a crystallographic relation between the twin components) is dropped.
A common feature of twins, domain structures and grain aggregates is the interface between coexisting crystals. The simplest edifice containing a crystalline interface is a bicrystal consisting of two semiinfinite perfect crystals (components) and a single planar interface along which the two crystals adjoin. For easier comprehension, one crystal of a bicrystal can be `coloured' black and the other crystal white. Then the operations that leave both crystals unchanged are trivial colourpreserving symmetry operations, whereas the symmetrizing operations, which transform the black crystal into the white one and vice versa, are nontrivial colourreversing operations. If one marks these colourreversing operations by a prime or a star, then the symmetry group of a bicrystal has the structure of a dichromatic (blackandwhite) group (see Section 3.2.3.2.7).
The dissymmetrization (symmetry reduction or lowering, symmetry descent) plays a basic role in bicrystallography. This is a process in which an object changes from a highsymmetry form into a lowsymmetry form. As shown in Chapter 3.4 , any dissymmetrization is accompanied by the formation of several symmetrically equivalent specimens of the low symmetry called variants. Variants are related by suppressed (lost) symmetry operations that are present in the lowsymmetry form but are missing in the highsymmetry form. The set of all lowsymmetry variants recovers the symmetry of the highsymmetry form. This general statement is referred to as the law of symmetry compensation and can be alternatively expressed by the following sentence (Shubnikov & Koptsik, 1974): If symmetry is reduced at one structural level, it arises and is recovered at another structural level. A paradigmatic example of dissymmetrization is a structural phase transition in which a highsymmetry parent (prototypic) phase changes into a lowsymmetry distorted (ferroic) phase. The variants of the lowsymmetry distorted phase are called single domain states or orientation states. The set of all single domain states recovers the high symmetry of the parent phase (see Chapter 3.4 ).
A systematic method for deriving the bicrystal symmetry, which is identical with the symmetry of the bicrystal interface, consists of four hierarchical stages (Pond & Vlachavas, 1983). At each stage, the bicrystal is represented by a construct (model) which is more detailed – and has, therefore, the same or lower symmetry – than the construct of the previous stage. These successive dissymmetrizations bring about at each stage equivalent variants of the bicrystal's construct. Different sets of variants at different stages have distinct physical significance and provide a basic generic classification of bicrystals and their interfaces.
The first stage deals with the socalled dichromatic pattern consisting of two interpenetrating black and white lattices of the two crystal components (Pond & Bollmann, 1979). The coinciding `grey' points constitute the coincidence site lattice (CSL) (see Bollmann, 1970, 1982), which corresponds to the twin lattice in twinning (see Section 3.3.8 ). To find variants of the dichromatic pattern, bicrystallography replaces the symmetry group of a nonexistent previous `zero stage' with a minimal group containing symmetries of the black crystal and the white crystal. This group is called the embracing or fundamental group of dichromatic patterns (Shubnikov & Koptsik, 1974; Pond & Vlachavas, 1983; Wadhawan, 2000). If the symmetry group of the dichromatic pattern is smaller than the embracing group, then this dissymmetrization produces orientational or translational variants of the dichromatic pattern.
In the second stage, black and white lattices are decorated by atoms and these crystal structures are represented by lattice complexes. [A lattice complex of a crystal is here defined as the set of points obtained by carrying out on each occupied atomic position all symmetry operations of the crystal's space group. Note that in crystallography the term `lattice complex' has a different meaning; see IT A (2005), Parts 8 and 14 .] Two interpenetrating black and white lattice complexes of crystal components form the dichromatic complex of a bicrystal. If the symmetry of the dichromatic complex is lower than that of the dichromatic pattern, the dissymmetrization gives rise to complex variants of the dichromatic complex. The concept of a dichromatic complex corresponds to the concept of a domain pair in domain structure analysis (see Section 3.4.3 ).
Mental constructions of the first two stages specify only the relation between the lattices and structures of crystal components of a bicrystal. In the third stage, an ideal bicrystal is formed by sectioning the blackandwhite lattice (or structure) on the interface plane and discarding the black lattice (or structure) on one side of the section and the white lattice (structure) on the other side. If the interfacial plane is a crystallographic plane with twodimensional periodicity, then the symmetry of this ideal bicrystal is described by a dichromatic layer group (see Sections 3.4.4.2 and 3.4.4.3 ). This group is smaller than the spacegroup symmetry of the dichromatic complex and this dissymmetrization gives rise to morphological variants of the ideal bicrystal. Operations suppressed at this dissymmetrization relate different morphological variants of the ideal bicrystal. An ideal bicrystal corresponds to a domain twin with zerothickness domain wall (see Section 3.4.4).
All three preceding stages use geometrical models of an interface with fixed atomic positions. At the final fourth stage, these geometrical constraints are lifted and the ideal bicrystal relaxes to a real or relaxed bicrystal with a minimum free energy. During this relaxation process the interface plane may migrate into either crystal, one crystal may translate rigidly with respect to the other, and each atom may adjust its position to relax any resultant force acting on it. The relaxation may even include insertion or removal of additional material at the interface. If the symmetry of the relaxed bicrystal is lower than that of the ideal bicrystal, then relaxational variants of the relaxed bicrystal appear. The onedimensional interface between two interfacial relaxational variants forms a line defect of the bicrystal interface. Relaxation variants of finitethickness domain walls and line defects in these walls are discussed in Section 3.4.4 .
Two main theoretical approaches have been used in examining the microscopic structure of a real bicrystal interface. In the older one, a real interface is treated as a periodic array of dislocations. This approach, still based on geometrical models, has explained successfully the microscopic structure of smallangle grain boundaries, but has failed in largeangle grain boundaries (misorientation angle larger than 15°).
More recent investigations utilizing computer simulations allow one to lift geometrical constraints and permit the calculation of equilibrium atomic positions directly from interatomic forces. These calculations have revealed that the lattice coincidence is almost always lost upon relaxation and that the microscopic structure of bicrystal interfaces can be described as an ordered sequence of coordination polyhedra. These conclusions have been confirmed by highresolution electron microscopy. For more details see, for example, Fischmeister (1985), Sutton & Balluffi (1995) and Gottstein & Shvindlerman (1999).
The first three `classical' stages of the bicrystallographical analysis already yield valuable conclusions. They disclose generic relations between different interfaces, specify crystallographically equivalent variants of an interface and classify line defects in interfaces. The symmetry of a bicrystal imposes constraints on tensor properties of the bicrystal interface, provides classification of the interfacial vibrational modes, discloses possible interfacial transitions etc. (see, for example, Kalonji, 1985).
The methodology of bicrystallography has many common features with the symmetry analysis of domain structures but, since both approaches have developed independently, they use a different terminology. Moreover, in comparison with bicrystals, domain structures and twins are more restricted by crystallographic constraints. This has resulted in more extensive application of group theory in domain structures than in bicrystallography. On the other hand, bicrystallography is more general and can even treat interfaces between two crystals belonging to different phases (heterophase interfaces).
A synoptic `roadmap for the use of interfacial symmetry', compiled by Kalonji (1985), provides a quick guide to the possible applications of bicrystallography. A short introduction to bicrystallography can be found in Wadhawan (2000); a brief comparison of the concepts and terminologies of bicrystals, twins and domain structures is presented by Hahn et al. (1999). An extensive treatment of bicrystallography is available in the paper by Pond & Vlachavas (1983) and in the book by Sutton & Balluffi (1995), where other aspects of crystalline interfaces are also thoroughly covered.
Analysis of domain structures and twins does not deal primarily with singlecrystal structures, as does classical crystallography, but studies collections of several crystal structures – which usually differ in orientation and position in space – and examines relations between these structures and their coexistence. The exact formulation of such an analysis uses mathematical concepts that are not yet quite common in crystallography. Thus, e.g., a collection of crystallographic objects has to be decomposed into equivalence classes called orbits and strata, or the symmetry of an object (structure, domain wall, twin) has to be described with respect to a given group, which necessitates replacing the usual notion of a symmetry group by a `stabilizer' (isotropy group). A prerequisite of introducing these terms is the concept of group action, which provides a basic and efficient tool for domainstructure analysis.
Another special feature of domain studies is that one can associate with a ferroic structure under study another structure, called the parent (prototypic) structure, from which the ferroic structure can be derived by small microscopic distortions. The fact that the symmetry of the ferroic phase is lower than that of the parent phase invokes the notion of a subgroup. Associated notions such as conjugate subgroups, normalizers and decomposition of a group into left and double cosets of a subgroup play an important role in the analysis.
Since some of these concepts are not available in standard texts, we present in this section the necessary mathematical background and explanation of terms and relations that appear in Chapters 3.3 and 3.4 .
Section 3.2.3.1 introduces the basic concepts of set theory and explains the notion of unordered and ordered pairs, mappings of sets and the partition of a set into equivalence classes. Section 3.2.3.2 deals with basic group theory and is devoted mainly to group–subgroup relations and relevant notions, of which the coset decompositions are of central importance. In Section 3.2.3.3, group theory is combined with set theory in the `action of a group on a set' (for short, `group action'). Notions of stabilizer, orbit and stratum are explained and their significance is illustrated by several examples.
A simple exposition of the main grouptheoretical concepts, including group action and orbits, can be found in the book by Hahn & Wondratschek (1994). A concise presentation of group actions and related notions with many examples has been given by Michel (1980). Other more detailed references are given at the end of each of the following sections.
Definition 3.2.3.1. A set is a collection of distinguishable objects. The objects constituting a set are called elements (or points) of the set.
In Chapter 3.4 we encounter mainly two types of sets: sets the elements of which are crystalline objects (domain states, domain twins, domain walls etc.), and sets, like groups, with elements of mathematical nature, e.g. rotations, transformations, operations etc. The sets of crystalline objects will be denoted by capital sansserif letters, e.g. , and capital bold letters, e.g. or , will be used to denote elements of such sets. Groups will be denoted by capital italic letters, e.g. G, F etc., and their elements by lowercase italic letters, e.g. . The exposition of this section is given for sets the elements of which are (crystalline) objects, but all notions and relations hold for any other sets.
If an element belongs to the set , one writes , in the opposite case . Sets consisting of a small number of elements can be expressed explicitly by writing their elements between curly braces, . The order of elements in the symbol of the set is irrelevant. From the definition of a set it follows that there are no equal elements in the set, or in other words, any two equal elements coalesce into one:If a set contains many (or an infinite number of) elements, the elements are specified in another way, e.g. by stating that they have a certain property in common.
The number of elements in a set is the order of the set. A finite set consists of a finite number of elements and this number is denoted by . An infinite set contains infinite number of elements and an empty set, denoted by , contains no element. In what follows, the term `set' will mean a `finite nonempty set' unless explicitly stated otherwise.
A set is a subset of , or , if every element of is an element of . If each element of is an element of , and vice versa, then is equal to or identical with , or . If there exists at least one element of which is not contained in , then is a proper subset of , or . The subset is often defined by a restriction that specifies only some elements of as elements of . This is written in short as ; the expression means that consists of all elements of that satisfy the restriction given behind the sign .
The intersection of two sets and , or , is a set comprising all elements that belong both to and to . If the sets and have no element in common, , then one says that the sets and are disjoint. The union of sets and , or , is a set consisting of all elements that belong either to or to . Sometimes the symbol is used instead of the symbol . The difference of set and , or the complement of in , , comprises those elements of that do not belong to .
A collection of two objects and constitutes an unordered pair. The objects of an unordered pair are called elements or points. A trivial unordered pair consists of two identical elements. A nontrivial unordered domain pair comprises two nonidentical elements and is identical with a set of order two.
Note that we do not identify an unordered pair with a set of order two where, according to (3.2.3.1), two equal objects coalesce into one. In spite of this difference we shall use the same symbol for the unordered pair as for the set of order two, but reverse the symbol for the trivial unordered pair. With this reservation, the identityholds for both unordered pairs and for sets of order two.
An ordered pair, denoted , consists of the first and the second member of the pair. If , the ordered pair is called a trivial ordered pair, ; if the pair is a nontrivial ordered pair. The ordered pair with a reversed order of elements is called a transposed pair. In contrast to unordered pairs, initial and transposed nontrivial ordered pairs are different objects,
The members and of an ordered pair can either belong to one set, , or each to a different set, .
Two ordered pairs and are equal, , if and only if and .
We shall encounter ordered and unordered pairs in Sections 3.4.3 and 3.4.4 , where the members of pairs are domain states or domain twins. However, pairs are also essential in introducing further concepts of set theory. The starting point is the following construction of a set of pairs that are formed from two sets:
A Cartesian product of two sets and is a set of all ordered pairs , where . The sets and can be different or identical sets. If the sets and are finite, then the Cartesian product consists of ordered pairs.
A mapping of a set into a set is a rule which assigns to each element a unique element . This is written symbolically as or , and one says that is mapped to under the mapping . The element is called the image of the element S under . The assignment can be expressed by an ordered pair , if one ascribes to the first member of the pair and the element to the second member of the pair . Then the mapping of a set into a set , symbolically written as , can be identified with such a subset of ordered pairs of the Cartesian product in which each element of occurs exactly once as the first member of the pair . If is a finite set, then consists of ordered pairs.
We note that in a mapping several elements of may be mapped to the same element of . In such a case, the mapping is called a manytoone mapping. If the mapping is such that each element of is the image of some element of , then the mapping is called a mapping of onto . If is a mapping of onto and, moreover, each element of is the image of exactly one element of , then the mapping becomes a onetoone correspondence between and , . In this case, and are of the same order.
One often encounters a situation in which one assigns to each ordered pair an element , where all three elements are elements from the same set , symbolically ; or . Such a mapping is called a binary operation or a composition law on the set . A sum of two numbers or a product of two numbers , where belong to the set of all real numbers, are elementary examples of binary operations.
The notion of the ordered pair allows one to introduce another useful concept, namely the relation on a set. An example will illustrate this notion. Let be a set of integers, . For each ordered pair , , one can decide whether m is smaller than n, , or not. All pairs that fulfil the condition form a subset of all possible ordered pairs . In other words, the relation defines a subset of the set , . Similarly, the relation ( denotes absolute value of n) defines another subset of .
To indicate that an element is related to by , where , one writes , where the relation defines a subset of all ordered pairs , (the same letter is used for the subset and for the relation on ). The opposite also holds: Each subset of defines a certain relation on .
A relation is called an equivalence relation on the set if it satisfies three conditions: Thus, for example, it is easy to corroborate that the relation on the set of integers fulfils all three conditions (3.2.3.3) to (3.2.3.5) and is, therefore, an equivalence relation on the set . On the other hand, the relation is not an equivalence relation on since it fulfils neither the reflexivity (3.2.3.3) nor the symmetry condition (3.2.3.4).
Let be an equivalence relation on and ; all elements such that constitute a subset of denoted and called the equivalence class of with respect to (or the equivalence class of S). The element is called the representative of the class . Any other member of the class can be chosen as its representative. Any two elements of the equivalence class are equivalent elements of .
From the definition of the equivalence class, it follows that any two elements are either equivalent elements of , , and thus belong to the same class, , or are not equivalent, and thus belong to two different classes that are disjoint, . In this way, the equivalence relation divides the set into disjoint subsets (equivalence classes), the union of which is equal to the set itself. Such a decomposition is called a partition of the set associated with the equivalence relation . For a finite set this decomposition can be expressed as a union of equivalence classes, where are representatives of the equivalence classes.
Generally, any decomposition of a set into a system of disjoint nonempty subsets such that every element of the set is a member of just one subset is called a partition of the set. To any partition of a set there corresponds an equivalence relation such that the equivalence classes of form that partition. This equivalence relation defines two elements as equivalent if and only if they belong to the same subset.
The term `equivalent' is often used when it is clear from the context what the relevant equivalence relation is. Similarly, the term `class' is used instead of `equivalence class'. Sometimes equivalence classes have names that do not explicitly indicate that they are equivalence classes. For example, in group theory, conjugate subgroups, left, right and double cosets form equivalence classes (see Section 3.2.3.2). Often instead of the expression `partition of a set ' an equivalent expression `classification of the elements of a set ' is used. The most important equivalence classes in the symmetry analysis of domain structures are called orbits and will be discussed in Section 3.2.3.3.
More details on set theory can be found in Kuratowski & Mostowski (1968), Lipschutz (1981), and Opechowski (1986).
Operations (isometries) that act on a body without changing its form and internal state combine in the same way as do elements of a group. Group theory is, therefore, the main mathematical tool for examining transformation properties – symmetry properties in particular – of crystalline objects. The basic concept of group theory is that of a group.
Definition 3.2.3.2. A group G is a set that satisfies four postulates:
The number of elements of a group G is called the order of the group. If the order of the group is finite, it is denoted by .
The multiplication of group elements is, in general, not commutative, i.e. may hold for some . If the multiplication is commutative, i.e. if for all , then the group G is called a commutative or Abelian group. All groups of orders 1 to 5 are Abelian. In Abelian groups, an additive notation is sometimes used instead of the multiplicative notation, i.e. if and are elements of an Abelian group G then one writes instead of . Additive notation is usually used in groups of translations.
The nth power of an element , where n is a positive integer, is defined recursively in the following manner:
If G is written additively, one writes instead of and speaks of a multiple of g.
If m and n are integers and g is an element of G then the following laws of exponents hold:
A set of elements of a group G is called a set of generators of G if any element of the group G can be written as a product of powers of these generators. In general, a group may have several sets of generators.
The order of an element g is the smallest positive integer m such that . An element g and the inverse element have the same order. The order m of any element g of a finite group G is a factor of the order .
Two groups G and with elements and , respectively, are isomorphic if there is an onetoone correspondence between G and , such thatIn other words, the isomorphism of two groups G and is a onetoone mapping of G onto [(3.2.3.13)] which preserves the products of the elements of the two groups [(3.2.3.14)]. Two isomorphic groups G and are denoted as .
Isomorphism is an equivalence relation that divides the set of all groups into classes of isomorphic groups. Between two groups G and there may exist several isomorphisms.
Groups that appear in Chapters 3.3 and 3.4 are mostly crystallographic groups [for their definition and properties see Bradley & Cracknell (1972), Hahn & Wondratschek (1994), IT A (2005), IT A1 (2004), Janssen (1973), Opechowski (1986), and Vainshtein (1994)]. Elements of these groups are distancepreserving transformations (mappings) called isometries, Euclidean transformations, motions or crystallographic operations. Whenever we encounter crystallographic groups we shall use the term `crystallographic operation' or just `operation' or `isometry' instead of `element'.
In what follows, the group G may be a crystallographic point group or a crystallographic space group. Since we shall be mainly concerned with a continuum approach, we shall have in mind point groups. When we consider space groups, we shall mention this explicitly and, if possible, use calligraphic letters, e.g. , etc. for space groups.
Crystallographic operations of crystallographic point groups and products of these operations can be found by means of the multiplication calculator in the software GIKoBo1 under the menu item Group Elements (see the manual for GIKoBo1).
Definition 3.2.3.3. Let G be a group. A subset F of G is a subgroup of G if it forms a group under the product rule of G, i.e. if it fulfils the group postulates (1) to (4).
For finite groups these requirements can be replaced by a single condition [see e.g. Opechowski (1986)]: The product of any two elements of F belongs to F,
The groups G and F are denoted the highsymmetry group and the lowsymmetry group, respectively. The pair `group G – subgroup F' is called the symmetry descent , dissymmetrization or symmetry reduction . A symmetry descent is a basic specification of a phase transition and corresponding domain structure (see Chapters 3.1 and 3.4 ).
Each group G always has at least two subgroups: the group G itself (sometimes called the improper subgroup) and the trivial subgroup consisting of the unit element only. The symbol signifies that F is a subgroup of G including the improper subgroup G, whereas means that F is a proper subgroup of G which differs from G. By this definition, the trivial subgroup is a proper subgroup. This definition of a proper subgroup [used e.g. in Volume A of the present series (IT A, 2005) and by Opechowski (1986)] is convenient for our purposes, although often by the term `proper subgroup' one understands a subgroup different from G and from the trivial subgroup.
A proper subgroup F of G is a maximal subgroup of G if it is not a proper subgroup of some other proper subgroup H, i.e. if there exists no group H such that A group can have more than one maximal subgroup.
A group P for which G is subgroup is called a supergroup of G, . If G is a proper subgroup of Q, , then Q is a proper supergroup of G. If G is a maximal subgroup of P, then P is called a minimal supergroup of G.
Let a group L be a proper supergroup of a group F, , and simultaneously a proper subgroup of a group G, . Then the sequence of subgroups will be called a group–subgroup chain and the group L an intermediate group of the chain (3.2.3.16).
Subgroups of crystallographic point groups are listed in Table 3.4.2.7 and are displayed in Figs. 3.1.3.1 and 3.1.3.2 (see also the software GIKoBo1, menu item Subgroups).
If is a proper subgroup of G and is a fixed element of G, then the set of all products , where f runs over all elements of the subgroup , is denoted and is called the left coset of in G, where the sign means `for all'. Similarly, one defines a right coset of in G: [Some authors, e.g. Hall (1959), call the set a right coset of in G and the set a left coset of in G.] Since in the application of cosets in the symmetry analysis of domain structures left cosets are used almost exclusively, all statements that follow are formulated for left cosets. Each statement about left cosets has a complementary statement about right cosets which can in most cases be obtained by replacing `left' with `right'.
The element which appears explicitly in the symbol of the left coset of is called a representative of the left coset . Any element of a left coset can be chosen as its representative.
Left coset criterion: Two elements and belong to the same left coset, , if and only if belongs to the subgroup , .
The property of `belong to the same left coset' is an equivalence relation, therefore two left cosets of the same subgroup are either identical or have no elements in common.
Proposition 3.2.3.4. The union of all distinct left cosets of in G constitutes a partition of G and is called the decomposition of G into the left cosets of . If the set of left cosets of in G is finite, then the decomposition of G into the left cosets of can be expressed aswhere the symbol is the settheoretical union (see Section 3.2.3.1). For the representative of the first left coset the unit element e is usually chosen, . Then the first left coset is identical with the subgroup . The number of elements in each left coset of the decomposition is equal to the order of the group .
The set of leftcoset representatives is sometimes called a left transversal to in G.
The number n of distinct left cosets is called the index of the subgroup in the group G and is denoted by the symbol . If the groups G and are of finite order then where and are the orders of G and , respectively. From this equation follows:
Lagrange's theorem : the order of a finite group is a multiple of the order of each of its subgroups. Alternatively, the index of a subgroup and the order of a finite subgroup are divisors of the group order.
We note that an infinite subgroup of an infinite group can have a finite index. Important examples are subgroups of translational groups of crystallographic space groups and subgroups of space groups (see Example [oC] 3.2.3.32 in Section 3.2.3.3.5).
The decompositions of crystallographic point groups into left and right cosets are available in the software GIKoBo1, under Subgroups\View\Twinning Group.
Proposition 3.2.3.5. Let be an intermediate group . The group G can be decomposed into left cosets of , where and the group into left cosets of , where Then the decomposition of G into left cosets of can be written in the form and the index n of in G can be expressed as a product of indices m and d,
Decompositions (3.2.3.19) and (3.2.3.21) of a group into left cosets enable one to divide a set of objects into classes of symmetrically equivalent objects (see Section 3.2.3.3.4). The concept of domain states is based on this result (see Section 3.4.2 ).
Two subgroups and are conjugate subgroups if there exists an element g of G such that More explicitly, one says that the subgroup is conjugate by g (or conjugate under G) to the subgroup . Conjugate subgroups are isomorphic.
The property of `being conjugate' is an equivalence relation. The set of all subgroups of a group G can therefore be partitioned into disjoint classes of conjugate subgroups. Conjugate subgroups of crystallographic point groups are given in Table 3.4.2.7 and in the software GIKoBo1, under Subgroups\View\Twinning Group.
The collection of all elements g that fulfil the relation constitutes a group denoted by and is called the normalizer of in G. The normalizer is a subgroup of G and a supergroup of ,
The normalizer determines the subgroups conjugate to under G (see Example 3.2.3.10). The number m of subgroups conjugate to a subgroup under G equals the index of in G: where the last equation holds for finite G and .
Normalizers of the subgroups of crystallographic point groups are available in Table 3.4.2.7 and in the software GIKoBo1 under Subgroups\View\Twinning Group.
Among subgroups of a group, a special role is played by normal subgroups. A subgroup H of G is a normal (invariant, selfconjugate) subgroup of G if and only if it fulfils any of the following conditions:
For a normal subgroup H of a group G a special symbol is often used instead of , .
Any subgroup H of a group G of index 2, called a halving subgroup, is a normal subgroup. The decomposition of G into left cosets of H consists of two left cosets, Sometimes it is convenient to distinguish elements of the coset from elements of the halving subgroup H. This can be achieved by attaching a sign (usually written as a superscript) to all elements of the coset. We shall use for this purpose the sign . To aid understanding, we shall also mark for a while the elements of the group H with another sign, . The multiplication law for these `decorated elements' can be written in the following form:Now we replace the label by a dummy `no mark' sign (i.e. we remove ), but we still keep in mind the multiplication rules (3.2.3.34). Then the decomposition (3.2.3.33) becomessince the coset assembles all marked elements and H consists of all bare elements of the group G.
The sign can carry useful additional information, e.g. the application of labelled operations is connected with some changes or new effects, whereas the application of a bare operation brings about no such changes or effects.
The label can be replaced by various signs which can have different meanings. Thus in Chapter 3.3 a prime signifies a nontrivial twinning operation, in Chapter 1.5 it is associated with time inversion in magnetic structures, and in blackandwhite patterns or structures a prime denotes an operation which exchanges black and white `colours' (the qualifier `blackandwhite' concerns group operations, but not the blackandwhite pattern itself). In Chapter 3.4 , a star denotes a transposing operation which exchanges two domain states, while underlining signifies an operation exchanging two sides of an interface and underlined operations with a star signify twinning operations of a domain twin. Various interpretations of the label attached to the symbol of an operation have given rise to several designations of groups with partition (3.2.3.34): blackandwhite, dichromatic, magnetic, antisymmetry, Shubnikov or Heech–Shubnikov and other groups. For more details see Opechowski (1986).
Let and be two proper subgroups of the group G. The set of all distinct products , where is a fixed element of the group G and f and h run over all elements of the subgroups and , respectively, is called a double coset of and in G. The symbol of this double coset is , where the sign means `for all'.
In the symmetry analysis of domain structures, only double cosets with are used. We shall, therefore, formulate subsequent definitions and statements only for this special type of double coset.
The fixed element is called the representative of the double coset . Any element of a double coset can be chosen as its representative.
Two double cosets are either identical or disjoint.
Proposition 3.2.3.6. The union of all distinct double cosets constitutes a partition of G and is called the decomposition of the group G into double cosets of , since . If the set of double cosets of in G is finite, then the decomposition of G into the double cosets of can be written asFor the representative of the first double coset the unit element e is usually chosen, . Then the first double coset is identical with the subgroup .
A double coset consists of left cosets of the form , where . The number r of left cosets of in the double coset is (Hall, 1959) where
The following definitions and statements are used in Chapter 3.4 for the double cosets [for derivations and more details, see Janovec (1972)].
The inverse of a double coset is a double coset , which is either identical or disjoint with the double coset . The double coset that is its own inverse is called an invertible (selfinverse, ambivalent) double coset. The double coset that is disjoint with its inverse is called a noninvertible (polar) double coset and the double cosets and are called complementary polar double cosets.
The inverse left coset contains representatives of all left cosets of the double coset . If a left coset belongs to an invertible double coset, then contains representatives of left cosets constituting the double coset . If a left coset belongs to a noninvertible double coset, then contains representatives of left cosets constituting the complementary double coset .
A double coset consisting of only one left coset, is called a simple double coset. A double coset is simple if and only if the inverse of the left coset is again a left coset. For an invertible simple double coset .
The union of all simple double cosets in the double coset decomposition of G (3.2.3.36) constitutes the normalizer (Speiser, 1927).
A double coset that comprises more than one left coset will be called a multiple double coset. Four types of double cosets are displayed in Table 3.2.3.1. The double coset decompositions of all crystallographic point groups are available in the software GIKoBo1 under Subgroups\View\Twinning Group.

Double cosets and the decomposition (3.2.3.36) of a group in double cosets are mathematical tools for partitioning a set of pairs of objects into equivalent classes (see Section 3.2.3.3.6). Such a division enables one to find possible twin laws and different types of domain walls that can appear in a domain structure resulting from a phase transition with a given symmetry descent (see Chapters 3.3 and 3.4 ).
More detailed introductions to group theory can be found in Budden (1972), Janssen (1973), Ledermann (1973), Rosen (1995), Shubnikov & Koptsik (1974), Vainshtein (1994) and Vainshtein et al. (1995). More advanced books on group theory are, for example, Bradley & Cracknell (1972), Hall (1959), Lang (1965), Opechowski (1986), Robinson (1982) and Speiser (1927). Parts of group theory relevant to phase transitions and tensor properties are treated in the manual of the software GIKoBo1. Representations of the crystallographic groups are presented in Chapter 1.2 of this volume and in the software GIKoBo1 (see the manual).
A direct application of the set and group theory to our studies would hardly justify their presentation in the last two sections. However, an appropriate combination of these theories, called group action, forms a very useful tool for examining crystalline materials and domain structures in particular. In this section, the main concepts (action of a group on a set [a], orbits [o], stabilizers [s]) are explained and their application is illustrated with examples from crystallography, where the group G is either a crystallographic point group or space group (denoted , if necessary), and the set is the threedimensional point space [P], a crystal [C], a property tensor [T] and a subgroup of G [S]. Letters in square brackets in front of the sequential number of examples and definitions should aid navigation in the text.
Example [aP] 3.2.3.7 . Crystals are objects in a threedimensional space called point space. Points of this space form an infinite set which we denote . If one chooses a point O as the origin, then to each point one can assign the position vector of a vector space [see, for example, IT A (2005), Part 8 ]. There is a onetoone correspondence between points of the point space and corresponding position vectors of the vector space, If one further selects three noncoplanar basic vectors , then the position vector r can be written as where are coordinates of the point X.
Let G be a point group. An operation (isometry) transforms (moves) the point X to a point with the position vector Coordinates of this image point are related to coordinates of the initial point by a linear relation, where are components of a matrix representing the operation g.
The described motion of the point X under the operation g can be formally expressed as a simple relation the exact meaning of which can be formulated in terms introduced in Section 3.2.3.1 as a mapping that assigns to an ordered pair a point of the set , The mapping – i.e. a prescription for how to determine from g and X the resulting point – is defined by (3.2.3.40) to (3.2.3.43). The relation (3.2.3.44) should be considered as only a shorthand version of the explicit relation (3.2.3.45).
The action of a group on a set generalizes the described procedure to any group and any set. In this section, we shall use the term `object' for an element of a set and the term `operation' for an element of a group.
Definition [a] 3.2.3.8 . Let G be a group, a set of objects and a mapping that assigns to an ordered pair , where and are objects of the set : The ordered pair can often be written simply as a product and the mapping as an equation. Then the relation (3.2.3.46) can be expressed in a simpler form: If the mapping (3.2.3.46), expressed in this condensed way, fulfils two additional conditions, where e is the identity operation (unit element) of G, andthen the mapping is called an action (or operation) of a group G on a set , or just a group action.
We must note that the replacement of the explicit mapping (3.2.3.46) by a contracted version (3.2.3.47) is not always possible (see Example [aS] 3.2.3.11).
The condition (3.2.3.49) requires that the first action followed by the second action gives the same result as if one first calculates the product and then applies it to , .
When a group G, a set , and a mapping fulfil the requirements (3.2.3.47) to (3.2.3.49), one says that G acts or operates on and the set is called a Gset.
Example [aC] 3.2.3.9 . We shall examine the action of an isometry g on an ideal infinite crystal in the threedimensional space. Let us choose four points (atoms) of the crystal that define three noncoplanar vectors (e.g. basic lattice translations). These vectors will specify the orientation of the crystal in space. Let g be a pointgroup operation. This isometry g transforms (moves) points of the crystal to new positions and changes the orientation of the crystal to a new orientation specified by vectors , where are coefficients of a matrix representing the operation g. For nontrivial operations g, the resulting vectors always differ from the initial ones. If g is an improper rotation (rotoinversion), then these vectors have an opposite handedness to the vectors of the initial orientation and, for enantiomorphous crystals, the transformed crystal is an enantiomorphous form of the crystal in the initial orientation.
We choose a reference coordinate system defined by the origin O and by three noncoplanar basis vectors . By the state S of a crystal we shall understand, in a continuum description, the set of all its properties expressed by components of physical property (matter) tensors in the reference coordinate system or, in a microscopic description, the positions of atoms in the elementary unit cell expressed in the reference coordinate system. States defined in this way may change with temperature and external fields, and also with the orientation of the crystal in space. At constant temperature and external fields, the states are in onetoone correspondence with the orientations of the crystal.
Application of an isometry on a state of a crystal can be treated as a group action: Let G be a point group and a set of all conceivable states of a crystal. We denote by the state of the crystal in an initial orientation. An operation g of G changes the orientation of the crystal and the resulting state of the crystal in a new orientation is determined by and g. This is, in mathematical terms, a mapping of a pair on a state from the set , , or in the shorthand notation, Since this mapping fulfils conditions (3.2.3.48) and (3.2.3.49), it is a group action. We note that for some g the resulting state can be identical with the initial state and that several operations can produce the same resulting state .
Group action of an isometry on a crystal applies in a natural way to domain structures, where the group G describes the symmetry of the parent (highsymmetry) phase and the states are crystallographically equivalent (Gequivalent) states of the distorted (lowsymmetry) phase called domain states. This means that domain states are states that are crystallographically equivalent in G. In a continuum description, domain states differ in orientation and are called ferroic domain states or orientation states (see Section 3.4.3.2 ).
Example [aT] 3.2.3.10 . Let us consider a property tensor (e.g. polarization, permittivity, piezoelectric coefficients) and let us denote by components of this tensor expressed in a fixed reference coordinate system. This set can be represented by a point in the corresponding tensor space. Let us denote by the set of all points of this tensor space and by G a point group. The mapping is defined by the transformation law of the tensor components (see Chapter 1.1 ). This mapping fulfils conditions (3.2.3.48) and (3.2.3.49), and can therefore be treated as a group action.
Example [aS] 3.2.3.11 . Let G be a group, F a subgroup of G, , and the set of all subgroups of G. The group G can act on the set by conjugation: In this case, one has to write the mapping explicitly since the abbreviated form would mean a left coset and not a conjugate subgroup . One also has to corroborate the validity of condition (3.2.3.49): , which is the image of .
An action of a group G on a set introduces two basic notions, namely stabilizers and orbits.
The concept of a stabilizer is closely connected with the notion of the symmetry group of an object. Under the symmetry group F of an object one understands the set of all operations (isometries) that map the object onto itself, i.e. leave this object invariant. In this approach, one usually `attaches' the symmetry elements to the object. Then the symmetry group F of the object is its inherent property which does not depend on the orientation and position of the object in space. The term eigensymmetry is used in Chapter 3.3 for symmetry groups defined in this way.
The notion of a stabilizer describes the symmetry properties of an object from another standpoint, in which the object and the group of isometries are decoupled and introduced independently. One chooses a reference coordinate system and a group G of isometries, the operations of which have a defined orientation in this reference system. Usually, it is convenient to choose as the reference system the standard coordinate system (crystallographic or crystallophysical) of the group G. The object under consideration is specified not only per se but also by its orientation in the reference system. Those operations of G that map the object in this orientation onto itself form a group called the stabilizer of in the group G. An algebraic definition is formulated in the following way:
Definition [s] 3.2.3.12 . The stabilizer (isotropy group) of an object of a Gset in group G is that subgroup of G comprised of all operations of G that do not change ,
Unlike the `eigensymmetry', the stabilizer depends on the group G, is generally a subgroup of G, , and may change with the orientation of the object .
There is an important relation between stabilizers of two objects from a Gset (see e.g. Aizu, 1970; Kerber, 1991):
Proposition 3.2.3.13 . Consider two objects from a Gset related by an operation g from the group G. The respective stabilizers are conjugate by the same operation g,
Let us illustrate the meaning of stabilizers with four examples of group action considered above.
Example [sP] 3.2.3.14 . Let be a crystallographic space group and X a point of the threedimensional point space (see Example 3.2.3.7). The stabilizer , called the sitesymmetry group of the point X in , consists of all symmetry operations of that leave the point X invariant. Consequently, the stabilizer is a crystallographic point group. If the stabilizer consists only of the identity operation, then the point X is called a point of general position. If is a nontrivial point group, X is called a point of special position (IT A , 2005).
Example [sC] 3.2.3.15 . The symmetry of domain states , treated in Example [sP] 3.2.3.9, is adequately expressed by their stabilizers in the group G of the parent (highsymmetry) phase, , . These groups are called symmetry groups of domain states. If domain states are related by an operation , then their symmetry groups are, according to (3.2.3.55), conjugate by g,
Symmetry characterization of domain states by their stabilizers properly reflects a difference between ferroelastic single domain states and ferroelastic disoriented domain states (see Sections 3.4.3 and 3.4.4 ).
Example [sT] 3.2.3.16 . The notion of the stabilizer enables one to formulate a basic relation between the symmetry group of the parent phase, the symmetry group of the first domain state and order parameters of the transition. In a microscopic description, the symmetry of the parent phase is described by a space group and the symmetry of the first basic (microscopic) single domain state by the stabilizer . The stabilizer of the primary order parameter must fulfil the condition The appearance of nonzero in the ferroic phase thus fully accounts for the symmetry descent at the transition.
In a continuum description, a role analogous to is played by a principal tensor parameter (see Section 3.1.3 ). Its stabilizer in the parent point group G equals the point group of the first single domain state ,
This contrasts with the secondary order parameter (secondary tensor parameter in a continuum description). Its stabilizer is an intermediate group , i.e. the appearance of would lead only to a partial symmetry descent with .
Example [sS] 3.2.3.17 . The stabilizer of a subgroup from Example [aS] 3.2.3.11 is the normalizer defined in Section 3.2.3.2.5:
In general, a stabilizer, which is a subgroup of G, is an example of a structure which is induced by a group action on the group G. On the other hand, a group action exerts a partition of the set into equivalence classes called orbits.
The group action allows one to specify the equivalence relation and the partition of a set into equivalence classes introduced in Section 3.2.3.1 [see (3.2.3.6)]. If G is a group and are two objects of a Gset , then one says that the objects are Gequivalent, , if there exists an operation that transforms into , In our applications, the group G is most often a crystallographic group. In this situation we shall speak about crystallographically equivalent objects. Exceptionally, G will be the group of all isometries (full orthogonal group in three dimensions); then we shall talk about symmetrically equivalent objects.
The relation is an equivalence relation on a set and therefore divides a set into Gequivalence classes. These classes are called orbits and are defined in the following way:
Definition [o] 3.2.3.18 . Let be a Gset and an object of the set . A G orbit of , denoted , is a set of all objects of that are Gequivalent with ,
Important note: The object of the orbit is called the representative of the orbit . If the group G is known from the context, one simply speaks of an orbit of .
Any two objects of an orbit are Gequivalent and any object of the orbit can be chosen as a representative of this orbit. Two G orbits , of a Gset are either identical or disjoint. The set can therefore be partitioned into disjoint orbits, Different groups G produce different partitions of the set .
Example [oP] 3.2.3.19 . If X is a point in threedimensional point space and G is a crystallographic point group (see Example [aP] 3.2.3.7), then the orbit consisting of all crystallographically equivalent points is called a point form [see IT A (2005), Part 10 ]. If the group is a space group , then is called the a crystallographic orbit of X with respect to . In this case, the crystallographic orbit is an infinite set of points due to the infinite number of translations in the space group [see IT A (2005), Part 8 ]. In this way, the infinite set of points of the point space is divided into an infinite number of disjoint orbits.
Example [oC] 3.2.3.20 . Let be a domain state from Example [aC] 3.2.3.9. The orbit , where G is the parent phase symmetry, assembles all Gequivalent domain states, The existence of several equivalent states is the main characteristic feature of domain states. Domain states of the orbit represent all possible variants of the lowsymmetry phase with the same energy and the same chance of appearance in the domain structure. Structurally, they represent the crystal structure in all distinguishable orientations (and also positions in a microscopic description) related by isometries of the group G. If G contains rotoinversions and if is an enantiomorphic structure, then the orbit also comprises the enantiomorphic form of .
Example [oT] 3.2.3.21 . Let be a principal tensor parameter of the pointgroupsymmetry descent (see Example [sT] 3.2.3.16). The orbit consists of all points in the tensor space of the principal tensor parameter that are crystallographically equivalent with respect to G,
Example [oS] 3.2.3.22 . The orbit of a subgroup in Example [aS] 3.2.3.11 is the set of all subgroups conjugate under G to ,
From Proposition 3.2.3.13 and from Example [oS] 3.2.3.22, it follows that stabilizers of objects from one orbit constitute the orbit (3.2.3.66) of all subgroups conjugate under G. One can thus associate with each orbit an orbit of conjugate subgroups of G. The set of all objects with stabilizers from one orbit of conjugate subgroups is called a stratum of in the set (Michel, 1980; Kerber, 1999). In crystallography, the term Wyckoff position is used for the stratum of points of the point space (IT A , 2005).
The notion of a stratum can be also applied to the classification of orbits of domain states treated in Example [oC] 3.2.3.22. Let G be the symmetry of the parent phase and the set of all states of the crystal. Orbits of domain states with stabilizers from one orbit of conjugate subgroups of G, , are of the `same type' and form a stratum of domain states. Domain states of different orbits belonging to the same stratum differ in the numerical values of parameters describing the states but have the same crystallographic and topological properties. All possible strata that can be formed from a given parent phase with symmetry G can be identified with all different orbits of subgroups of G.
In a similar manner, points of the orderparameter space and tensorparameter space from Examples [sC] 3.2.3.16 and [oT] 3.2.3.21 can be divided into strata which are characterized by the orbits of possible stabilizers.
Next, we formulate three propositions that are essential in the symmetry analysis of domain structures presented in Section 3.4.2 .
Proposition 3.2.3.23 . Let G be a finite group, a Gset and the stabilizer of an object of the set . The objects of the orbit and the left cosets of the decomposition of G, are in a onetoone correspondence,
(See e.g. Kerber, 1991, 1999; Kopský, 1983; Lang, 1965.) The derivation of the bijection (3.2.3.69) consists of two parts:
We note that the orbit depends on the stabilizer of the object and not on the `eigensymmetry' of .
From Proposition 3.2.3.23 follow two corollaries:
Corollary 3.2.3.24 . The order n of the orbit equals the index of the stabilizer in G, where the last part of the equation applies to point groups only.
Corollary 3.2.3.25 . All objects of the orbit can be generated by successive application of representatives of all left cosets in the decomposition of G [see (3.2.3.68)] to the object , . The orbit can therefore be expressed explicitly aswhere the operations (left transversal to in G) are the representatives of left cosets in the decomposition (3.2.3.68).
Example [oP] 3.2.3.26 . The number of equivalent points of the point form (G orbit of the point X) is called a multiplicity of this point, The multiplicity of a point of general position equals the order of the group G, since in this case , a trivial group. Then points of the orbit and the operations of G are in a onetoone correspondence. The multiplicity of a point of special position is smaller than the order , , and the operations of G and the points of the orbit are in a manytoone correspondence. Points of a stratum have the same multiplicity; one can, therefore, talk about the multiplicity of the Wyckoff position [see IT A (2005)]. If G is a space group, the point orbit has to be confined to the volume of the primitive unit cell (Wondratschek, 1995).
Example [oC] 3.2.3.27 . Corollaries 3.2.3.24 and 3.2.3.25 applied to domain states represent the basic relations of domainstructure analysis. According to (3.2.3.71), the index n of the stabilizer in the parent group G gives the number of domain states in the orbit and the relations (3.2.3.72) and (3.2.3.68) give a recipe for constructing domain states of this orbit.
Example [oT] 3.2.3.28 . If is a principal tensor parameter associated with the symmetry descent , then there is a onetoone correspondence between the elements of the orbit of single domain states and the elements of the orbit of the principal order parameter (points) (see Example [oT] 3.2.3.21), Therefore, single domain states of the orbit can be represented by the principal tensor parameter of the orbit .
Example [oS] 3.2.3.29 . Consider a subgroup of a group G. Since the stabilizer of in G is the normalizer (see Example [sS] 3.2.3.17), the number m of conjugate subgroups is, according to (3.2.3.71), where the last part of the equation applies to point groups only. The orbit of conjugate subgroups is where the operations are the representatives of left cosets in the decomposition
Proposition 3.2.3.30 . Let be a G orbit from Proposition 3.2.3.23 and an intermediate group, A successive decomposition of G into left cosets of and into left cosets of [see (3.2.3.25)] introduces a twoindices relabelling of the objects of a G orbit defined by the onetoone correspondence where are the representatives of the decompositions of G into left cosets of , and are the representatives of the decompositions of into left cosets of ,
The index n of in G can be expressed as a product of indices m and d [see (3.2.3.26)], If G is a finite group, then the index n can be expressed in terms of orders of groups G, and :
When one chooses , then the members of the orbit can be arranged into an array,
The set of objects of the jth row of this array forms an orbit with the representative , where The intermediate group thus induces a splitting of the orbit into m suborbits , : Aizu (1972) denotes this partitioning factorization of species.
The relation (3.2.3.79) is just the application of the correspondence (3.2.3.69) of Proposition 3.2.3.23 on the successive decomposition (3.2.3.25). Derivation of the second part of Proposition 3.2.3.30 can be sketched in the following way: where the relation (3.2.3.70) is used.
We note that the described partitioning of an orbit into suborbits depends on the choice of representative of the first suborbit and that the number of conjugate subgroups may be equal to or smaller than the number m of suborbits (see Example [oS] 3.2.3.34).
Each intermediate group in Proposition 3.2.3.30 can usually be associated with a certain attribute, e.g. a secondary order parameter, which specifies the suborbits.
Example [oP] 3.2.3.31 . Let G be a point group and a point of general position in the point space. A symmetry descent to a subgroup is accompanied by a splitting of the orbit of equivalent points into suborbits each consisting of equivalent points. The first suborbit is , the others are , , , , where are representatives of left cosets of in the decomposition of G [see (3.2.3.80)].
Splitting of orbits of points of general position is a special case in which . Splitting of orbits of points of special position is more complicated if (see Wondratschek, 1995).
Example [oC] 3.2.3.32 . Let us consider a phase transition accompanied by a lowering of spacegroup symmetry from a parent space group with translation subgroup T and point group G to a lowsymmetry space group with translation subgroup U and point group F. There exists a unique intermediate group , called the group of Hermann, which has translation subgroup T and point group (see e.g. Hahn & Wondratschek, 1994; Wadhawan, 2000; Wondratschek & Aroyo, 2001).
The decomposition of into left cosets of , corresponding to (3.2.3.80), is in a onetoone correspondence with the decomposition of G into left cosets of F, since and have the same translation subgroup and and have the same point group. Therefore, the index .
Since and have the same point group F, the decomposition of into left cosets of , corresponding to (3.2.3.81), is in a onetoone correspondence with the decomposition of into left cosets of , Representatives are translations. The corresponding vectors lead from the origin of a `superlattice' primitive unit cell of the lowsymmetry phase to lattice points of located within or on the side faces of this `superlattice' primitive unit cell (Van Tendeloo & Amelinckx, 1974). The number of these vectors is equal to the ratio , where and are the volumes of the primitive unit cell of the lowsymmetry phase and the parent phase, respectively, and and are the number of chemical formula units in the primitive unit cell of the lowsymmetry phase and the parent phase, respectively.
There is another useful formula for expressing . The primitive basis vectors of are related to the primitive basis vectors of by a linear relation, where are integers. The volumes of primitive unit cells are and . Using (3.2.3.90), one gets , where is the determinant of the matrix of the coefficients . Hence the index .
Thus we get for the index N of in
Each suborbit, represented by a row in the array (3.2.3.84), contains all basic (microscopic) domain states that are related by pure translations. These domain states exhibit the same tensor properties, i.e. they belong to the same ferroic domain state.
Example [sT] 3.2.3.33 . Let us consider a phase transition with a symmetry descent with an orbit of domain states. Let be an intermediate group, , and the principal order parameter associated with the symmetry descent [cf. (3.2.3.58)], . Since is an intermediate group, the quantity represents a secondary order parameter of the symmetry descent . The G orbit of is As in Example [oT] 3.2.3.28, there is a bijection between left cosets of the decomposition of G into left cosets of [see (3.2.3.80)] and the G orbit of secondary order parameters (3.2.3.92). One can, therefore, associate with the suborbit the value of the secondary order parameter , A suborbit is thus comprised of objects of the orbit with the same value of the secondary order parameter .
Example [oS] 3.2.3.34 . Let us choose for the intermediate group the normalizer . Then the suborbits equal where are representatives of left cosets in the decomposition of , and are representatives of the decomposition (3.2.3.77). The suborbit consists of all objects with the same stabilizer ,
Propositions 3.2.3.23 and 3.2.3.30 are examples of structures that a group action induces from a group G on a Gset. Another important example is a permutation representation of the group G which associates operations of G with permutations of the objects of the orbit [see e.g. Kerber (1991, 1999); for application of the permutation representation in domainstructure analysis and domain engineering, see e.g. Fuksa & Janovec (1995, 2002)].
An ordered pair is formed by two objects from the orbit . Let denote the set of all ordered pairs that can be formed from the objects of the orbit . The group action of group G on the set is defined by the following relation:The requirements (3.2.3.47) to (3.2.3.49) are fulfilled, mapping (3.2.3.97) defines an action of group G on the set .
The group action (3.2.3.97) introduces the Gequivalence of ordered pairs: Two ordered pairs and are crystallographically equivalent (with respect to the group G), , if there exists an operation that transforms into ,
An orbit of ordered pairs comprises all ordered pairs crystallographically equivalent with . One can choose as a representative of the orbit an ordered pair with the first member since there is always an operation such that . The orbit assembles all ordered pairs with the first member . This orbit can be expressed aswhere the identity [see relation (3.2.3.70)] has been used.
Thus the double coset contains all operations from G that produce all ordered pairs with the first member that are Gequivalent with . If one chooses that is not contained in the double coset , then the ordered pair must belong to another orbit . Hence to distinct double cosets there correspond distinct classes of ordered pairs with the first member , i.e. distinct orbits of ordered pairs. Since the group G can be decomposed into disjoint double cosets [see (3.2.3.36)], one gets
Proposition 3.2.3.35 . Let G be a group and a set of all ordered pairs that can be formed from the objects of the orbit . There is a onetoone correspondence between the G orbits of ordered pairs of the set and the double cosets of the decomposition This bijection allows one to express the partition of the set of all ordered pairs into G orbits, where is the set of representatives of double cosets in the decomposition (3.2.3.100) (Janovec, 1972).
Proposition 3.2.3.35 applies directly to pairs of domain states (domain pairs) and allows one to find transposition laws that can appear in the lowsymmetry phase (see Section 3.4.3 ).
For more details and other applications of group action see e.g. Kopský (1983), Lang (1965), Michel (1980), Opechowski (1986), Robinson (1982), and especially Kerber (1991, 1999).
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