International
Tables for
Crystallography
Volume C
Mathematical, physical and chemical tables
Edited by E. Prince

International Tables for Crystallography (2006). Vol. C, ch. 2.2, pp. 31-34

## Section 2.2.3. Rotation/oscillation geometry

J. R. Helliwella

aDepartment of Chemistry, University of Manchester, Manchester M13 9PL, England

### 2.2.3. Rotation/oscillation geometry

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The main modern book dealing with the rotation method is that of Arndt & Wonacott (1977).

#### 2.2.3.1. General

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The purpose of the monochromatic rotation method is to stimulate a reflection fully over its rocking width via an angular rotation. Different relp's are rotated successively into the reflecting position. The method, therefore, involves rotation of the sample about a single axis, and is used in conjunction with an area detector of some sort, e.g. film, electronic area detector or image plate. The use of a repeated rotation or oscillation, for a given exposure, is simply to average out any time-dependent changes in incident intensity or sample decay. The overall crystal rotation required to record the total accessible region of reciprocal space for a single crystal setting, and a detector picking up all the diffraction spots, is 180° + . If the crystal has additional symmetry, then a complete asymmetric unit of reciprocal space can be recorded within a smaller angle. There is a blind region close to the rotation axis; this is detailed in Subsection 2.2.3.5.

#### 2.2.3.2. Diffraction coordinates

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Figs. 2.2.3.1(a) to (d) are taken from IT II (1959, p. 176). They neatly summarize the geometrical principles of reflection, of a monochromatic beam, in the reciprocal lattice for the general case of an incident beam inclined at an angle (μ) to the equatorial plane. The diagrams are based on an Ewald sphere of unit radius.

 Figure 2.2.3.1 | top | pdf |(a) Elevation of the sphere of reflection. O is the origin of the reciprocal lattice. C is the centre of the Ewald sphere. The incident beam is shown in the plane. (b) Plan of the sphere of reflection. R is the projection of the rotation axis on the equatorial plane. (c) Perspective diagram. P is the relp in the reflection position with the cylindrical coordinates . The angular coordinates of the diffracted beam are . (d) Stereogram to show the direction of the diffracted beam, , with DD′, normal to the incident beam and in the equatorial plane, as the projection diameter. From Evans & Lonsdale (1959).

With the nomenclature of Table 2.2.3.1:

 Table 2.2.3.1| top | pdf | Glossary of symbols used to specify quantities on diffraction patterns and in reciprocal space
 Bragg angle Angle of deviation of the reflected beam with respect to the incident beam Unit vector lying along the direction of the incident beam Unit vector lying along the direction of the reflected beam s = The scattering vector of magnitude . s is perpendicular to the bisector of the angle between and . s is identical to the reciprocal-lattice vector d* of magnitude λ/d, where d is the interplanar spacing, when d* is in the diffraction condition. In this notation, the radius of the Ewald sphere is unity. This convention is adopted because it follows that in Volume II of International Tables (p. 175). Note that in Section 2.2.1 Laue geometry the alternative convention (|d*| = 1/d) is adopted whereby the radius of each Ewald sphere is 1/λ. This allows a nest of Ewald spheres between and to be drawn Coordinate of a point P in reciprocal space parallel to a rotation axis as the axis of cylindrical coordinates relative to the origin of reciprocal space Radial coordinate of a point P in reciprocal space; that is, the radius of a cylinder having the rotation axis as axis The angular coordinate of P, measured as the angle between and [see Fig. 2.2.3.1(b)] The angle of rotation from a defined datum orientation to bring a relp onto the Ewald sphere in the rotation method (see Fig. 2.2.3.3) The angle of inclination of to the equatorial plane The angle between the projections of and onto the equatorial plane The angle of inclination of to the equatorial plane The crystal setting angles on the four-circle diffractometer (see Fig. 2.2.6.1). The used here is not the same as that in the rotation method (Fig. 2.2.3.3). This clash in using the same symbol twice is inevitable because of the widespread use of the rotation camera and four-circle diffractometer.

The equatorial plane is the plane normal to the rotation axis.

Fig. 2.2.3.1(a) gives Fig. 2.2.3.1(b) gives, by the cosine rule, and and Figs. 2.2.3.1(a) and (b) give

The following special cases commonly occur:

 (a) μ = 0, normal-beam rotation method, then and (b) μ = −ν, equi-inclination (relevant to Weissenberg upper-layer photography), then (c) μ = +ν, anti-equi-inclination (d) ν = 0, flat cone

In this section, we will concentrate on case (a), the normal-beam rotation method (μ = 0). First, the case of a plane film or detector is considered.

The notation now follows that of Arndt & Wonacott (1977) for the coordinates of a spot on the film or detector. is parallel to the rotation axis and ζ. is perpendicular to the rotation axis and the beam. IT II (1959, p. 177) follows the convention of y being parallel and x perpendicular to the rotation-axis direction, i.e. . The advantage of the notation is that the x-axis direction is then the same as the X-ray beam direction.

The coordinates of a reflection on a flat film are related to the cylindrical coordinates of a relp (ξ, ζ) [Fig. 2.2.3.2(a)] by which becomes where D is the crystal-to-film distance.

 Figure 2.2.3.2 | top | pdf |Geometrical principles of recording the pattern on (a) a plane detector, (b) a V-shaped detector, (c) a cylindrical detector.

For the case of a V-shaped cassette with the V axis parallel to the rotation axis and the film making an angle α to the beam direction [Fig. 2.2.3.2(b)], then This situation also corresponds to the case of flat electronic area detector inclined to the incident beam in a similar way.

Note that Arndt & Wonacott (1977) use ν instead of α here. We use α and so follow IT II (1959). This avoids confusion with the ν of Table 2.2.3.1. D is the crystal to V distance. In the case of the V cassettes of Enraf–Nonius, α is 60°.

For the case of a cylindrical film or image plate where the axis of the cylinder is coincident with the rotation axis [Fig. 2.2.3.2(c)] then, for in degrees, which becomes Here, D is the radius of curvature of the cylinder assuming that the crystal is at the centre of curvature.

In the three geometries mentioned here, detector-misalignment errors have to be considered. These are three orthogonal angular errors, translation of the origin, and error in the crystal-to-film distance.

The coordinates and are related to film-scanner raster units via a scanner-rotation matrix and translation vector. This is necessary because the film is placed arbitrarily on the scanner drum. Details can be found in Rossmann (1985) or Arndt & Wonacott (1977).

#### 2.2.3.3. Relationship of reciprocal-lattice coordinates to crystal system parameters

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The reciprocal-lattice coordinates, etc. used earlier, refer to an axial system fixed to the crystal, of Fig. 2.2.3.3 . Clearly, a given relp needs to be brought into the Ewald sphere by the rotation about the rotation axis. The treatment here follows Arndt & Wonacott (1977).

 Figure 2.2.3.3 | top | pdf |The rotation method. Definition of coordinate systems. [Cylindrical coordinates of a relp P (ξ, ζ, ϕ) are defined relative to the axial system X0Y0Z0 which rotates with the crystal.] The axial system XYZ is defined such that X is parallel to the incident beam and Z is coincident with axis. From Arndt & Wonacott (1977).

The rotation angle required, , is with respect to some reference `zero-angle' direction and is determined by the particular crystal parameters. It is necessary to define a standard orientation of the crystal (i.e. datum) when = 0°. If we define an axial system fixed to the crystal and a laboratory axis system XYZ with X parallel to the beam and Z coincident with the rotation axis then = 0° corresponds to these axial systems being coincident (Fig. 2.2.3.3).

The angle of the crystal at which a given relp diffracts is The two solutions correspond to the two rotation angles at which the relp P cuts the sphere of reflection. Note that , (Subsection 2.2.3.2) are independent of .

The values of x0 and y0 are calculated from the particular crystal system parameters. The relationships between the coordinates x0, y0, z0 and ξ and ζ are X0 can be related to the crystal parameters by A is a crystal-orientation matrix defining the standard datum orientation of the crystal.

For example, if, by convention, is chosen as parallel to the X-ray beam at = 0° and c is chosen as the rotation axis, then, for the general case,

If the crystal is mounted on the goniometer head differently from this then A can be modified by another matrix, M, say, or the terms permuted. This exercise becomes clear if the reader takes an orthogonal case (α = β = γ = 90°). For the general case, see Higashi (1989).

The crystal will most likely be misaligned (slightly or grossly) from the ideal orientation. To correct for this, the misorientation matrices , , and are introduced, i.e. where , , and are angles around the X0, Y0, and Z0 axes, respectively.

Hence, the relationship between X0 and h is

#### 2.2.3.4. Maximum oscillation angle without spot overlap

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For a given oscillation photograph, there is maximum value of the oscillation range, , that avoids overlapping of spots on a film. The overlap is most likely to occur in the region of the diffraction pattern perpendicular to the rotation axis and at the maximum Bragg angle. This is where relp's pass through the Ewald sphere with the greatest velocity. For such a separation between successive relp's of a*, then the maximum allowable rotation angle to avoid spatial overlap is given by where Δ is the sample reflecting range (see Section 2.2.7). is a function of , even in the case of identical cell parameters. This is because it is necessary to consider, for a given orientation, the relevant reciprocal-lattice vector perpendicular to . In the case where the cell dimensions are quite different in magnitude (excluding the axis parallel to the rotation axis), then is a marked function of the orientation.

In rotation photography, as large an angle as possible is used up to . This reduces the number of images that need to be processed and the number of partially stimulated reflections per image but at the expense of signal-to-noise ratio for individual spots, which accumulate more background since . In the case of a CCD detector system, is chosen usually to be less than Δ so as to optimize the signal-to-noise ratio of the measurement and to sample the rocking-width profile.

The value of Δ, the crystal rocking width for a given hkl, depends on the reciprocal-lattice coordinates of the hkl relp (see Section 2.2.7). In the region close to the rotation axis, Δ is large.

In the introductory remarks to the monochromatic methods used, it has already been noted that originally the rotation method involved 360° rotations contributing to the diffraction image. Spot overlap led to loss of reflection data and encouraged Bernal and Weissenberg to devise improvements. With modern synchrotron techniques, the restriction on (equation 2.2.3.30) can be relaxed for special applications. For example, since the spot overlap that is to be avoided involves relp's from adjacent reciprocal-lattice planes, the different Miller indices hkl and h + l, k, l do lead in fact to a small difference in Bragg angle. With good enough collimation, a small spot size exists at the detector plane so that the two spots can be resolved. For a standard-sized detector, this is practical for low-resolution data recording. This can be a useful complement to the Laue method where the low-resolution data are rather sparsely stimulated and also tend to occur in multiple Laue spots. Alternatively, a much larger detector can be contemplated and even medium-resolution data can be recorded without major overlap problems. These techniques are useful in some time-resolved applications. For a discussion see Weisgerber & Helliwell (1993). For regular data collection, however, narrow angular ranges are still generally preferred so as to reduce the background noise in the diffraction images and also to avoid loss of any data because of spot overlap.

#### 2.2.3.5. Blind region

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In normal-beam geometry, any relp lying close to the rotation axis will not be stimulated at all. This situation is shown in Fig. 2.2.3.4 . The blind region has a radius of and is therefore strongly dependent on dmin but can be ameliorated by use of a short λ. Shorter λ makes the Ewald sphere have a larger radius, i.e. its surface moves closer to the rotation axis. At Cu Kα for 2 Å resolution, approximately 5% of the data lie in the blind region according to this simple geometrical model. However, taking account of the rocking width Δ, a greater percentage of the data than this is not fully sampled except over very large angular ranges. The actual increase in the blind-region volume due to this effect is minimized by use of a collimated beam and a narrow spectral spread (i.e. finely monochromatized, synchrotron radiation) if the crystal is not too mosaic.

 Figure 2.2.3.4 | top | pdf |The rotation method. The blind region associated with a single rotation axis. From Arndt & Wonacott (1977).

These effects are directly related to the Lorentz factor, It is inadvisable to measure a reflection intensity when L is large because different parts of a spot would need a different Lorentz factor.

The blind region can be filled in by a rotation about another axis. The total angular range that is needed to sample the blind region is in the absence of any symmetry or in the case of mm symmetry (for example).

### References

Arndt, U. W. & Wonacott, A. J. (1977). The rotation method in crystallography. Amsterdam: North-Holland.Google Scholar
Higashi, T. (1989). The processing of diffraction data taken on a screenless Weissenberg camera for macromolecular crystallography. J. Appl. Cryst. 22, 9–18.Google Scholar
International Tables for X-ray Crystallography (1959). Vol. II. Birmingham: Kynoch Press.Google Scholar
Rossmann, M. G. (1985). Determining the intensity of Bragg reflections from oscillation photographs. Methods Enzymol. 114A, 237–280.Google Scholar
Weisgerber, S. & Helliwell, J. R. (1993). High-resolution crystallographic studies of native concanavalin A using rapid Laue data collection methods and the introduction of a monochromatic large-angle oscillation technique (LOT). J. Chem. Soc. Faraday Trans. 89, 2667–2675.Google Scholar