International
Tables for Crystallography Volume E Subperiodic groups Edited by V. Kopský and D. B. Litvin © International Union of Crystallography 2006 
International Tables for Crystallography (2006). Vol. E, ch. 1.2, pp. 57
Section 1.2.1. Classification of subperiodic groups^{a}Department of Physics, University of the South Pacific, Suva, Fiji, and Institute of Physics, The Academy of Sciences of the Czech Republic, Na Slovance 2, PO Box 24, 180 40 Prague 8, Czech Republic, and ^{b}Department of Physics, Penn State Berks Campus, The Pennsylvania State University, PO Box 7009, Reading, PA 196106009, USA 
Subperiodic groups can be classified in ways analogous to the space groups. For the mathematical definitions of these classifications and their use for space groups, see Chapter 8.2 of IT A (2005). Here we shall limit ourselves to those classifications which are explicitly used in the symmetry tables of the subperiodic groups.
The subperiodic groups are classified into affine subperiodic group types, i.e. affine equivalence classes of subperiodic groups. There are 80 affine layergroup types and seven affine friezegroup types. There are 67 crystallographic and an infinity of noncrystallographic affine rodgroup types. We shall consider here only rod groups of the 67 crystallographic rodgroup types and refer to these crystallographic affine rodgroup types simply as affine rodgroup types.
The subperiodic groups are also classified into proper affine subperiodic group types, i.e. proper affine classes of subperiodic groups. For layer and frieze groups, the two classifications are identical. For rod groups, each of eight affine rodgroup types splits into a pair of enantiomorphic crystallographic rodgroup types. Consequently, there are 75 proper affine rodgroup types. The eight pairs of enantiomorphic rodgroup types are (R24), (R26); (R31), (R33); (R43), (R44); (R47), (R48); (R54), (R58); (R55), (R57); (R63), (R67); and (R64), (R66). (Each subperiodic group is given in the text by its Hermann–Mauguin symbol followed in parenthesis by a letter L, R or F to denote it, respectively, as a layer, rod or frieze group, and its sequential numbering from Parts 2 , 3 or 4 .) We shall refer to the proper affine subperiodic group types simply as subperiodic group types.
There are 27 geometric crystal classes of layer groups and rod groups, and four geometric crystal classes of frieze groups. These are listed, for layer groups, in the fourth column of Table 1.2.1.1, and for the rod and frieze groups in the second columns of Tables 1.2.1.2 and 1.2.1.3, respectively.



We further classify subperiodic groups according to the following classifications of the subperiodic group's point group and lattice group. These classifications are introduced to emphasize the relationships between subperiodic groups and space groups:

A subdivision of the monoclinic rodgroup category is made into monoclinic/inclined and monoclinic/orthogonal. Two different coordinate systems, see Table 1.2.1.2, are used for the rod groups of these two subdivisions of the monoclinic crystal system. These two coordinate systems differ in the orientation of the plane containing the nonlattice basis vectors relative to the lattice vectors. For the monoclinic/inclined subdivision, the plane containing the nonlattice basis vectors is, see Fig. 1.2.1.1, inclined with respect to the lattice basis vector. For the monoclinic/orthogonal subdivision, the plane is, see Fig. 1.2.1.2, orthogonal.

Monoclinic/orthogonal basis vectors. For the monoclinic/orthogonal subdivision, α = β = 90° and the plane containing the a and b nonlattice basis vectors is orthogonal to the lattice basis vector c. 
The subperiodic groups are described by means of a crystallographic coordinate system consisting of a crystallographic origin, denoted by O, and a crystallographic basis. The basis vectors for the threedimensional layer groups and rod groups are labelled a, b and c. The basis vectors for the twodimensional frieze groups are labelled a and b. Unlike space groups, not all basis vectors of the crystallographic basis are lattice vectors. Like space groups, the crystallographic coordinate system is used to define the symmetry operations (see Section 1.2.9) and the Wyckoff positions (see Section 1.2.11). The symmetry operations are defined with respect to the directions of both lattice and nonlattice basis vectors. A Wyckoff position, denoted by a coordinate triplet (x, y, z) for the threedimensional layer and rod groups, is defined in the crystallographic coordinate system by O + r, where r = xa + yb + zc. For the twodimensional frieze groups, a Wyckoff position is denoted by a coordinate doublet (x, y) and is defined in the crystallographic coordinate system by O + r, where r = xa + yb.
The term setting will refer to the assignment of the labels a, b and c (and the corresponding directions [100], [010] and [001], respectively) to the basis vectors of the crystallographic basis (see Section 1.2.6). In the standard setting, those basis vectors which are also lattice vectors are labelled as follows: for layer groups with their twodimensional lattice by a and b, for rod groups with their onedimensional lattice by c, and for frieze groups with their onedimensional lattice by a.
The selection of a crystallographic coordinate system is not unique. Following IT A (2005), we choose conventional crystallographic coordinate systems which have a righthanded set of basis vectors and such that symmetry of the subperiodic groups is best displayed. The conventional crystallographic coordinate systems used in the standard settings are given in the sixth column of Table 1.2.1.1 for the layer groups, and the fourth columns of Tables 1.2.1.2 and 1.2.1.3 for the rod groups and frieze groups, respectively. The crystallographic origin is conventionally chosen at a centre of symmetry or at a point of high site symmetry (see Section 1.2.7).
The conventional unit cell of a subperiodic group is defined by the crystallographic origin and by those basis vectors which are also lattice vectors. For layer groups in the standard setting, the cell parameters, the magnitude of the lattice basis vectors a and b, and the angle between them, which specify the conventional cell, are given in the seventh column of Table 1.2.1.1. The conventional unit cell obtained in this manner turns out to be either primitive or centred and is denoted by p or c, respectively, in the eighth column of Table 1.2.1.1. For rod and frieze groups with their onedimensional lattices, the single cell parameter to be specified is the magnitude of the lattice basis vector.
References
International Tables for Crystallography (2005). Vol. A. Spacegroup symmetry, edited by Th. Hahn. Heidelberg: Springer. [Previous editions: 1983, 1987, 1992, 1995 and 2002. Abbreviated as IT A (2005).]Google Scholar