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. 255-258
Section 2.3.6.5. The fast rotation function
aDepartment of Biological Sciences, Purdue University, West Lafayette, Indiana 47907, USA, and bCABM & Rutgers University, 679 Hoes Lane, Piscataway, New Jersey 08854-5638, USA |
Unfortunately, the rotation-function computations can be extremely time-consuming by conventional methods. Sasada (1964) developed a technique for rapidly finding the maximum of a given peak by looking at the slope of the rotation function. A major breakthrough came when Crowther (1972) recast the rotation function in a manner suitable for rapid computation. Only a brief outline of Crowther's fast rotation function is given here. Details are found in the original text (Crowther, 1972) and his computer program description.
Since the rotation function correlates spherical volumes of a given Patterson density with rotated versions of either itself or another Patterson density, it is likely that a more natural form for the rotation function will involve spherical harmonics rather than the Fourier components of the crystal representation. Thus, if the two Patterson densities and are expanded within the spherical volume of radius less than a limiting value of a, then and and the rotation function would then be defined as Here is the normalized spherical harmonic of order l; is the normalized spherical Bessel function of order l; , are complex coefficients; and represents the rotated second Patterson. The rotated spherical harmonic can then be expressed in terms of the Eulerian angles as where and are the matrix elements of the three-dimensional rotation group. It can then be shown that Since the radial summation over n is independent of the rotation, and hence or The coefficients refer to a particular pair of Patterson densities and are independent of the rotation. The coefficients , containing the whole rotational part, refer to rotations of spherical harmonics and are independent of the particular Patterson densities. Since the summations over m and m′ represent a Fourier synthesis, rapid calculation is possible.
As polar coordinates rather than Eulerian angles provide a more graphic interpretation of the rotation function, Tanaka (1977) has recast the initial definition as He showed that the polar coordinates are now equivalent to , and . The rotation function can then be expressed as permitting rapid calculation of the fast rotation function in polar coordinates.
Crowther (1972) uses the Eulerian angles α, β, γ which are related to those defined by Rossmann & Blow (1962) according to , and .
References
Crowther, R. A. (1972). The fast rotation function. In The molecular replacement method, edited by M. G. Rossmann, pp. 173–178. New York: Gordon & Breach.Google ScholarRossmann, M. G. & Blow, D. M. (1962). The detection of sub-units within the crystallographic asymmetric unit. Acta Cryst. 15, 24–31.Google Scholar
Sasada, Y. (1964). The differential rotation function. Acta Cryst. 17, 611–612.Google Scholar
Tanaka, N. (1977). Representation of the fast-rotation function in a polar coordinate system. Acta Cryst. A33, 191–193.Google Scholar