Page 57 - Materials Chemistry, Second Edition
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44                                              2 Solid-State Chemistry


           lattice arrangement, and is determined from electron density maps and empirical
           X-ray diffraction data. Some general trends for cationic radii are:
           1. For a given species and charge, the radius increases as the coordination number
              increases.
           2. For a given charge, the radius decreases with increasing effective nuclear charge,
              Z eff . [17]
           3. For a given species, the radius decreases with increasing ionic charge.
           4. For a given species and charge, the radius is larger for high-spin (weak field) ions
              than for low-spin (strong field) ions.
           Most inorganic chemistry texts list cut-off values for the r þ /r   ratios corres-
           ponding to the various geometries of interstitial sites (Table 2.4). For instance, the
           halite or rocksalt structure exhibited by MX (M ¼ Grp I, Mg, Pb, Ag; X ¼ F, Cl,
           Br, I) are predicted to have occupation of octahedral interstitial sites. Indeed, these

           structures are described as a fcc array of the halide ion (except for v. small F ),
           with the cation occupying all of the octahedral interstitial sites (i.e., 4 MX units
           per unit cell).
             However, it should also be pointed out that deviations in these predictions are found
           for many crystals due to covalent bonding character. In fact, the bonding character for
           compounds is rarely 100% covalent or ionic in nature, especially for inorganic species.
           For instance, consider the zinc sulfide (ZnS) crystal structure. The ionic radius ratio
           for this structure is 0.52, which indicates that the cations should occupy octahedral
           interstitial sites. However, due to partial covalent bonding character, the anions are
           closer together than would occur from purely electrostatic attraction. This results in an
           “effective radius ratio” that is decreased, and a cation preference for tetrahedral sites
           rather than octahedral. One crystal structure for this complex lattice (a-ZnS, Wurtzite
           structure – also found for b-AgI, ZnO, a-CdS, CdSe, a-SiC, GaN, AlN, oBN, and
           BeO) is shown in Figure 2.23. This is best described as a hcp lattice of sulfide ions,
           with zinc ions occupying one-half of the available tetrahedral interstitial sites. As you
           might expect, a hybrid of ionic/covalent bonding will greatly affect the physical
           properties of the solid; for instance, the hardness of ZnS is significantly greater than
           what would be expected for a purely ionic solid.
             Interestingly, zinc sulfide (b-ZnS) may also crystallize in a cubic lattice, which
           consists of a fcc array of S , with Zn occupying 1/2 of the available tetrahedral
                                  2
           sites. This structure is known as sphalerite or zincblende, and is shared with other
           compounds such as a-AgI, b-BN, CuBr, and b-CdS. When the same atom occupies
           both the fcc and tetrahedral interstitials of the sphalerite structure, it is described as
           the diamond lattice, shared with elemental forms (allotropes) of silicon, germanium,
           and tin, as well as alloys thereof. Important semiconductors such as GaAs, b-SiC,
           and InSb also adopt the sphalerite crystal structure.
             If the cation in the crystal lattice exhibits a cubic environment (coordination
           number of 8), the fluorite structure is commonly observed (Figure 2.24). Lattices
           of this variety consist of an fcc arrangement of cations, with all eight tetrahedral
           interstitial sites (e.g., (1/4, 1/4, 1/4), etc.) occupied by the anionic species. Of course,
           this will only be prevalent when the size of the anion is much smaller than the cation,
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