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1.17.1.5 Bond length calculations

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It is very often desirable to be able to calculate interatomic distances in crystal structures. This is usually straightforward for crystals which have orthogonal unit cells (i.e. α = β = γ = 90°), and involves simple trigonometric calculations. For example, in the rock salt structure, the anion‐cation distance is a/2 and the anion–anion distance is . The main interatomic distances involving cations in T/O sites in an fcc/ccp anion array are shown in Fig. 1.25(c) and are summarised in Table 1.11 for the important structure types. These may be used together with the tables of unit cell dimensions, Table 1.9, etc., for calculations on specific compounds. Typical values of bond distances (to oxygen and fluorine) for all the elements are given in Appendix F, where relevant values for different coordination numbers and oxidation states are also given.

Consideration of atom arrangements in the three structure types described above shows that the concept of cp anions with cations in interstitial sites begins to break down in the fluorite structure. Thus, while the antifluorite structure of Na2O may be regarded as containing ccp O2– ions with Na+ ions in tetrahedral sites, in the fluorite structure of CaF2, it is necessary to regard the Ca2+ ions as forming the ccp array with F ions in tetrahedral sites. In CaF2 the Ca2+ ions have a eutactic ccp arrangement, but are well separated from each other; from Table 1.9 and Table 1.10, Ca–Ca = 3.86 Å, which is much larger than the diameter of a Ca2+ ion (depending on which table of ionic radii is consulted, the diameter of Ca2+ is in the range ~2.2–2.6 Å).

The F–F distance in CaF2 is 2.73 Å, which indicates that the fluorines are approximately contacting . Although the array of F ions in CaF2 is not cp but is primitive cubic, this is perhaps a more realistic way of describing the structure than as containing a eutactic ccp array of Ca2+ ions; nevertheless, both descriptions are used widely.

Solid State Chemistry and its Applications

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