Abstract
A simple phenomenological theory of the elastic constants of sphalerite structure crystals is presented and shown to apply within reasonable errors to the known experimental constants. The theory utilizes a form for bond-stretching (α) and bending (β) forces first used by Keating, to which are added effective point-ion Coulombic forces. Also it is pointed out that regularities in the experimental elastic constants of these crystals are readily explained in terms of the ionicity fi defined by Phillips and Van Vechten. Of particular note are the shear constants which decrease markedly with ionicity. It is found that this decrease is described quantitatively by βα(1fi), which confirms the interpretation of β, since bond-bending forces should vanish in the ionic limit fi1. Other equally simple formulas for the forces in terms of only the bond length and fi are shown to predict all the constants with a rms accuracy of 10%.

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