International
Tables for Crystallography Volume B Reciprocal space Edited by U. Shmueli © International Union of Crystallography 2006 |
International Tables for Crystallography (2006). Vol. B. ch. 2.3, pp. 252-253
Section 2.3.6.2. Matrix algebra
aDepartment of Biological Sciences, Purdue University, West Lafayette, Indiana 47907, USA, and bCABM & Rutgers University, 679 Hoes Lane, Piscataway, New Jersey 08854-5638, USA |
The initial step in the rotation-function procedure involves the orthogonalization of both crystal systems. Thus, if fractional coordinates in the first crystal system are represented by x, these can be orthogonalized by a matrix [β] to give the coordinates X in units of length (Fig. 2.3.6.2); that is, If the point X is rotated to the point X′, then where represents the rotation matrix relating the two vectors in the orthogonal system. Finally, X′ is converted back to fractional coordinates measured along the oblique cell dimension in the second crystal by Thus, by substitution, and by comparison with (2.3.6.2) it follows that Fig. 2.3.6.2 shows the mode of orthogonalization used by Rossmann & Blow (1962). With their definition it can be shown that and where with . For a Patterson compared with itself, .
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Relationships of the orthogonal axes to the crystallographic axes . [Reprinted from Rossmann & Blow (1962).] |
Both spherical and Eulerian angles are used in evaluating the rotation function. The usual definitions employed are given diagrammatically in Figs. 2.3.6.3 and 2.3.6.4. They give rise to the following rotation matrices.
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Eulerian angles relating the rotated axes to the original unrotated orthogonal axes . [Reprinted from Rossmann & Blow (1962).] |
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Variables ψ and φ are polar coordinates which specify a direction about which the axes may be rotated through an angle κ. [Reprinted from Rossmann & Blow (1962).] |
(a) Matrix [] in terms of Eulerian angles : and (b) matrix [] in terms of rotation angle κ and the spherical polar coordinates ψ, φ: Alternatively, (b) can be expressed as where u, v and w are the direction cosines of the rotation axis given by This latter form also demonstrates that the trace of a rotation matrix is .
The relationship between the two sets of variables established by comparison of the elements of the two matrices yields Since φ and ψ can always be chosen in the range 0 to π, these equations suffice to find from any set .
References
Rossmann, M. G. & Blow, D. M. (1962). The detection of sub-units within the crystallographic asymmetric unit. Acta Cryst. 15, 24–31.Google Scholar