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Observed Lattice Property Data
                             edly subject to the special features and limitations that the surface
                             introduces.

                             2.1 Observed Lattice Property Data


                Geometric    The geometric structure of a regular crystal lattice is determined using x-
                Structure    ray crystallography techniques, by recording the diffraction patterns of x-
                             ray photons that have passed through the crystal. From such a recorded
                             pattern (see Figure 2.1 (a)), we are able to determine the reflection planes
                             formed by the constituent atoms and so reconstruct the relative positions
                             of the atoms. This data is needed to proceed with a geometric (or, strictly
                             speaking, group-theoretic) characterization of the crystal lattice’s sym-
                             metry properties. We may also use an atomic force microscope (AFM) to
                             map out the force field that is exerted by the constituent atoms on the sur-
                             face of a crystal. From such contour plots we can reconstruct the crystal
                             structure and determine the lattice constants. We must be careful, though,
                             because we may observe special surface configurations in stead of the
                             actual bulk crystal structure, see Figure 2.1 (b).

                Elastic      The relationship between stress and strain in the linear region is via the
                Properties   elastic property tensor, as we shall shortly derive in Section 2.3.1. To
                             measure the elastic parameters that form the entries of the elastic prop-
                             erty tensor, it is necessary to form special test samples of exact geometric
                             shape that, upon mechanical loading, expose the relation between stress
                             and strain in such a way that the elastic coefficients can be deduced from
                             the measurement. The correct choice of geometry relies on the knowl-
                             edge of the crystal’s structure, and hence its symmetries, as we shall see
                             in Section 2.2.1. The most common way to extract the mechanical prop-
                             erties of crystalline materials is to measure the direction-dependent
                             velocity of sound inside the crystal, and by diffracting x-rays through the
                             crystal (for example by using a synchrotron radiation source).





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