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2.7 Monoclinic System

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Crystals in the monoclinic system possess a single twofold axis. Since a mirror plane is equivalent to an inverse diad, the class m (≡ ) is put into this system. Two settings are shown in Figure 2.6 for the monoclinic point groups, depending on whether the stereogram is centred on the twofold axis (the 1st setting) or whether the twofold axis is lying in the equatorial plane of the stereogram (the 2nd setting).

With respect to the convention for choosing x‐, y‐ and z‐axes for stereograms centred on the normal to the 001 planes for orthorhombic, tetragonal, and cubic crystals, the twofold axis is along the z‐axis in the 1st setting, so that the angle γ between the x‐ and y‐axes is obtuse (as for hexagonal crystals, where γ is fixed to be 120°), while α = β = 90°. In the 2nd setting, the twofold axis is along the y‐axis, so that the angle β between the x‐ and z‐axes is obtuse, while α = γ = 90°. Somewhat confusingly, both conventions are used in the scientific literature to describe the unit cells of monoclinic crystals, but it is much more common in materials science and metallurgy for the 2nd setting to be used, as we have chosen to do in Table 1.3 and Figures 1.19b and c. Irrespective of the choice of 1st or 2nd setting, the sides of the unit cells of crystals belonging to the monoclinic system are in general all unequal to one another.

The symmetry elements in the holosymmetric point group 2/m are shown in Figure 2.19 for the 2nd setting. The pole of (010) and the y‐axis coincide on the stereogram. In this figure, [001], the z‐axis, is chosen to be at the centre of the primitive and so (100) lies on the primitive 90° from (010). The x‐axis, the direction [100], which makes the obtuse angle β with [001], is necessarily in the lower hemisphere. The angle between [001] and (001) is (β − 90°), which is of course equal to the angle between the (100) pole and [100]. Poles such as {hk0} lie around the primitive because [001] lies in {hk0} planes (Weiss zone law, Eq. (1.6)).


Figure 2.19 Monoclinic stereogram centred on [001] for the 2nd setting

A pole such as (hk0) lies at angle ϕ to (010), given by:

(2.9a)

(see Figure 2.20), or equivalently (Section A3.2):

(2.9b)


Figure 2.20 A diagram from which the angle φ in Figure 2.19 between 010 and hk0 can be derived

The factor sin β arises because the x‐axis does not lie in the same plane as the plane perpendicular to the z‐axis within which the normals to (hk0) and (010) both lie. In the point group 2/m the only special form besides {010} is {h0l}, with a multiplicity of two – the planes (h0l) and (0). It is apparent that the two faces in this latter form are parallel, both lying normal to the mirror plane and parallel to the diad axis. The general form is {hkl}, with a multiplicity of four (see Figure 2.19). {hk0} and {0kl} are also general forms.

The remaining point groups in the monoclinic system are 2 and m. Again, {h0l} is a special form in both and so is {010}. However, 2 does not possess a centre, and so for this point group {010} and {00} must each be listed as separate special forms.

Crystallography and Crystal Defects

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