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. 377-392
https://doi.org/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,bInstitut für Kristallographie, Rheinisch–Westfälische Technische Hochschule, D-52056 Aachen, Germany, and cMineralogisch-Petrologisches Institut, Universität Bonn, D-53113 Bonn, Germany This chapter forms the introduction to the treatment of twinning in Chapter 3.3 Keywords: bicrystallography; bicrystals; black and white symmetry groups; coincidence-site lattice; conjugate subgroups; cosets; daughter phase; dichromatic complexes; dichromatic groups; domain structures; domains; double cosets; equivalence classes; equivalence relation; ferroelectric domain structures; ferroic domains; mappings; normalizers; orbit; parent phases; partition; sets; stabilizers; twinning. |
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 re-entrant 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 re-entrant 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 far-reaching 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 pseudo-mériédrie (twinning by pseudo-merohedry), macles par mériédrie réticulaire [twinning by reticular (lattice) merohedry] and macles par pseudo-mériédrie réticulaire (twinning by reticular pseudo-merohedry). 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 Klassen-Neklyudova (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, Klassen-Neklyudova et al. (1948
) observed the domain structure of Rochelle salt in a polarizing microscope (see Klassen-Neklyudova, 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 point-group 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 Klassen-Neklyudova et al. (1948) and Chernysheva (1950
). A detailed description of this work in English is presented by Klassen-Neklyudova (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 point-group symmetry at the structural phase transition from a prototypic (parent, high-symmetry) phase without domains to a ferroic (distorted, low-symmetry, 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 non-ferroelastic 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 high-symmetry 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 all-important 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 group-theoretical 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 semi-infinite 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 colour-preserving symmetry operations, whereas the symmetrizing operations, which transform the black crystal into the white one and vice versa, are nontrivial colour-reversing operations. If one marks these colour-reversing operations by a prime or a star, then the symmetry group of a bicrystal has the structure of a dichromatic (black-and-white) 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 high-symmetry form into a low-symmetry 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 low-symmetry form but are missing in the high-symmetry form. The set of all low-symmetry variants recovers the symmetry of the high-symmetry 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 high-symmetry parent (prototypic) phase changes into a low-symmetry distorted (ferroic) phase. The variants of the low-symmetry 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 so-called 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 black-and-white 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 two-dimensional 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 space-group 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 zero-thickness 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 one-dimensional interface between two interfacial relaxational variants forms a line defect of the bicrystal interface. Relaxation variants of finite-thickness 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 small-angle grain boundaries, but has failed in large-angle 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 high-resolution 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 single-crystal 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 domain-structure 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 group-theoretical 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 sans-serif 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 lower-case 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 non-trivial unordered domain pair comprises two non-identical 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 identity
holds 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 non-trivial ordered pair. The ordered pair
with a reversed order of elements is called a transposed pair. In contrast to unordered pairs, initial and transposed non-trivial 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 many-to-one 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 one-to-one 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 non-empty 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 one-to-one correspondence
between G and
,
such that
In other words, the isomorphism of two groups G and
is a one-to-one 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 distance-preserving 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 GIKoBo-1 under the menu item Group Elements (see the manual for GI
KoBo-1).
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 high-symmetry group and the low-symmetry 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 GI
KoBo-1, 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 as
where the symbol
is the set-theoretical 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 left-coset 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 GIKoBo-1, 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 GI
KoBo-1, 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 GI
KoBo-1 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, self-conjugate) 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
) becomes
since 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 black-and-white patterns or structures a prime denotes an operation which exchanges black and white `colours' (the qualifier `black-and-white' concerns group operations, but not the black-and-white 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
): black-and-white, dichromatic, magnetic, anti-symmetry, 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 as
For 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 (self-inverse, ambivalent) double coset. The double coset that is disjoint with its inverse is called a non-invertible (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 non-invertible 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 GI
KoBo-1 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 GI
KoBo-1. Representations of the crystallographic groups are presented in Chapter 1.2
of this volume and in the software GI
KoBo-1 (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 three-dimensional 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 three-dimensional 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 one-to-one correspondence between points of the point space and corresponding position vectors of the vector space,
If one further selects three non-coplanar 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, and
then 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 G-set.
Example [aC] 3.2.3.9
. We shall examine the action of an isometry g on an ideal infinite crystal in the three-dimensional space. Let us choose four points (atoms) of the crystal that define three non-coplanar vectors (e.g. basic lattice translations). These vectors will specify the orientation of the crystal in space. Let g be a point-group 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 non-trivial 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 non-coplanar 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 one-to-one 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 (high-symmetry) phase and the states are crystallographically equivalent (G-equivalent) states of the distorted (low-symmetry) 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 G-set
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 G-set (see e.g. Aizu, 1970; Kerber, 1991
):
Proposition 3.2.3.13
. Consider two objects from a G-set 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 three-dimensional point space
(see Example 3.2.3.7
). The stabilizer
, called the site-symmetry 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 non-trivial 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 (high-symmetry) 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 G-set
, then one says that the objects
are G-equivalent,
, 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 G-equivalence classes. These classes are called orbits and are defined in the following way:
Definition [o] 3.2.3.18
. Let be a G-set and
an object of the set
. A G orbit of
, denoted
, is a set of all objects of
that are G-equivalent 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 G-equivalent and any object of the orbit can be chosen as a representative of this orbit. Two G orbits ,
of a G-set
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 three-dimensional 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 G-equivalent 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 low-symmetry 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 point-group-symmetry 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 order-parameter space and tensor-parameter 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 G-set 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 one-to-one 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 as
where 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 one-to-one 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 many-to-one 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 domain-structure 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 one-to-one 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 two-indices relabelling of the objects of a G orbit defined by the one-to-one 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 space-group symmetry from a parent space group with translation subgroup T and point group G to a low-symmetry 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 one-to-one 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 one-to-one 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 low-symmetry 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 low-symmetry phase and the parent phase, respectively, and
and
are the number of chemical formula units in the primitive unit cell of the low-symmetry 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 G-set. 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 domain-structure 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 G-equivalence 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 as
where 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 G-equivalent 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 one-to-one 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 low-symmetry 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
).
References
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