International
Tables for
Crystallography
Volume A
Space-group symmetry
Edited by Th. Hahn

International Tables for Crystallography (2006). Vol. A, ch. 14.2, pp. 848-849

Section 14.2.2.2. Limiting complexes and comprehensive complexes

W. Fischera and E. Kocha*

aInstitut für Mineralogie, Petrologie und Kristallographie, Philipps-Universität, D-35032 Marburg, Germany
Correspondence e-mail:  kochelke@mailer.uni-marburg.de

14.2.2.2. Limiting complexes and comprehensive complexes

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For point groups, the occurrence of limiting crystal forms is well known. In [4/m], for instance, any tetragonal prism [\{hk0\}] is a special crystal form with face symmetry m.. . In point group 4, on the other hand, the tetragonal prisms [\{hk0\}] belong, as special cases, to the set of general crystal forms [\{hkl\}], the tetragonal pyramids, and there is no difference between [\{hkl\}] and [\{hk0\}] in either the number or the symmetry of their faces. Therefore, the tetragonal prism is called a `limiting form' of the tetragonal pyramid. In a case like this, all possible sets of equivalent faces belonging to a special type of crystal form (the tetragonal prism) may also be generated as a subset of another more comprehensive type of crystal form (the tetragonal pyramid). Of course, it is not possible, by considering a tetragonal prism by itself, to decide whether it has been generated by point group [4/m] or by point group 4. This distinction can be made, however, if the tetragonal prism shows the right striations or occurs in combination with other appropriate crystal forms. Low quartz (oriented point group 321) gives a well known example: the hexagonal prism [\{10\bar{1}0\}] has the same site symmetry 1 as any trigonal trapezohedron [\{hkil\}]. Therefore, [\{10\bar{1}0\}] may be recognized as a limiting form only if the crystal shows in addition at least one trigonal trapezohedron.

A similar relation may exist between two lattice complexes. Let L be a lattice complex generated by a Wyckoff position of a space group [{\cal G}] (e.g. by [P4/mmm\ 4l\ m2m.\ x00]). An appropriate Wyckoff position of a subgroup [{\cal H}] of [{\cal G}] (e.g. [P4/m\ 4j\ m..\ xy0]) may produce not only all point configurations of L but other point configurations in addition (with different orientations of the squares in the example). The complete set then forms a second lattice complex M. Such relationships led to the following definition (Fischer & Koch, 1974,[link] 1978[link]):

If a lattice complex L forms a true subset of another lattice complex M, the lattice complex L is called a limiting complex of M and the lattice complex M a comprehensive complex of L.

The point configurations of the limiting complex L are generated within M by restrictions imposed on the coordinate or/and the metrical parameters.

In the above example, such a restriction holds for the y coordinate: the condition [y = 0] for Wyckoff position 4j of [P4/m] filters out exactly those point configurations that constitute the lattice complex [P4/mmm\ l]. The latter complex is, therefore, a limiting complex of the lattice complex [P4/m\ j]. In the present case of restricted coordinates, both complexes belong to the same crystal family and L has fewer degrees of freedom than M.

Another kind of limiting-complex relation is connected with restrictions for metrical parameters. All point configurations of the lattice complex [Pm\bar{3}m\ a] are also generated by [P4/mmm\ a] under the restriction [a = c], i.e. in special space groups of type [P4/mmm]. Here L and M have the same number of degrees of freedom, but belong to different crystal families.

Finally, the two types of parameter restrictions for limiting complexes may also occur in combination. The trivariant lattice complex with characteristic Wyckoff position [P4_{1}2_{1}2\ 8b\ xyz], for example, contains the invariant cubic lattice complex [Fm\bar{3}m\ a] as a limiting complex. The parameter restrictions necessary are [x = {1 \over 2}, y = 0, z = {1 \over 16}, c/a = 4\surd{2}].

As for a limiting form in crystal morphology, it is often impossible to decide by which symmetry (space group and Wyckoff set) a particular point configuration, regarded by itself, has been generated. If a point configuration belongs to a lattice complex that is part of a comprehensive complex, this point configuration is a member of both complexes. As a consequence, the lattice complexes do not form equivalence classes of point configurations. Only if a point configuration is inspected in combination with a sufficient number of other point configurations – like sets of symmetrically equivalent atoms in a crystal structure – does it make sense to assign this point configuration to a particular lattice complex. An example is found in the crystal structures of the spinel type. Here, the oxygen atoms occupy Wyckoff position 32e xxx in [Fd\bar{3}m] with [x \approx {3 \over 8}] (referred to origin choice 1). If x is restricted to [{3 \over 8}], the point configurations generated are those of the lattice complex [Fm\bar{3}m\ a] (formed by all face-centred cubic point lattices). If for a spinel-type structure this restriction holds exactly, the point configurations of the cations would, nevertheless, reveal the true generating symmetry of the oxygen point configuration. It has, therefore, to be considered a member of the comprehensive complex [Fd\bar{3}m\ e] rather than a member of the lattice complex [Fm\bar{3}m\ a] (which includes among others the point configuration of the copper atoms in the crystal structure of copper). For practical applications, a point configuration contained in several lattice complexes may be investigated within the complex that is the least comprehensive but still allows the physical behaviour under discussion. This corresponds to the definition of the symmetry of a crystal generally used in crystallography: the highest symmetry that can be assigned to a crystal as a whole is that of its least symmetrical property known to date.

Even though limiting-complex relations are very useful for establishing crystallochemical relationships between different crystal structures, a complete study has not yet been carried out. Apart from isolated examples in the literature, systematic treatments have been given only for special aspects: plane lattice complexes (Burzlaff et al., 1968)[link]; cubic lattice complexes (Koch, 1974)[link]; point complexes, rod complexes and layer complexes (Fischer & Koch, 1978)[link]; extraordinary orbits for plane groups (Lawrenson & Wondratschek, 1976)[link]; noncharacteristic orbits of space groups except those that are due to metrical specialization (Engel et al., 1984)[link]. The closely related concepts of limiting complexes and noncharacteristic orbits have been compared by Koch & Fischer (1985)[link].

References

Burzlaff, H., Fischer, W. & Hellner, E. (1968). Die Gitterkomplexe der Ebenengruppen. Acta Cryst. A24, 57–67.
Engel, P., Matsumoto, T., Steinmann, G. & Wondratschek, H. (1984). The non-characteristic orbits of the space groups. Z. Kristallogr. Supplement issue No. 1.
Fischer, W. & Koch, E. (1974). Eine Definition des Begriffs `Gitterkomplex'. Z Kristallogr. 139, 268–278.
Fischer, W. & Koch, E. (1978). Limiting forms and comprehensive complexes for crystallographic point groups, rod groups and layer groups. Z. Kristallogr. 147, 255–273.
Koch, E. (1974). Die Grenzformen der kubischen Gitterkomplexe. Z. Kristallogr. 140, 75–86.
Koch, E. & Fischer, W. (1985). Lattice complexes and limiting complexes versus orbit types and non-characteristic orbits: a comparative discussion. Acta Cryst. A41, 421–426.
Lawrenson, J. E. & Wondratschek, H. (1976). The extraordinary orbits of the 17 plane groups. Z. Kristallogr. 143, 471–484.








































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