Solid State Chemistry and its Applications. Anthony R. West

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Solid State Chemistry and its Applications - Anthony R. West

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halides and Γ ‐AgI. A range of III–V compounds (i.e. elements from Groups III and V of the Periodic Table) have the zinc blende structure and some, e.g. GaAs, are important semiconductors.

       Table 1.8 Some compounds with the NaCl structure, a/Å

MgO 4.213 MgS 5.200 LiF 4.0270 KF 5.347
CaO 4.8105 CaS 5.6948 LiCl 5.1396 KCl 6.2931
SrO 5.160 SrS 6.020 LiBr 5.5013 KBr 6.5966
BaO 5.539 BaS 6.386 LiI 6.00 KI 7.0655
TiO 4.177 α‐MnS 5.224 LiH 4.083 RbF 5.6516
MnO 4.445 MgSe 5.462 NaF 4.64 RbCl 6.5810
FeO 4.307 CaSe 5.924 NaCl 5.6402 RbBr 6.889
CoO 4.260 SrSe 6.246 NaBr 5.9772 RbI 7.342
NiO 4.1769 BaSe 6.600 NaI 6.473 AgF 4.92
CdO 4.6953 CaTe 6.356 TiN 4.240 AgCl 5.549
TiC 4.3285 LaN 5.30 UN 4.890 AgBr 5.7745
Schematic illustration of the sphalerite (zinc blende) structure showing (a) the unit cell contents and (b) a more extended network of corner-sharing tetrahedra.

       Figure 1.33 The sphalerite (zinc blende) structure showing (a) the unit cell contents and (b) a more extended network of corner‐sharing tetrahedra.

       1.17.1.3 Antifluorite/fluorite structure

      The antifluorite structure has ccp/fcc anions with cations in all (T+ and T) tetrahedral sites. The difference between antifluorite and fluorite is that antifluorite refers to an anion array with tetrahedral cations, whereas fluorite has the inverse arrangement with a ccp cation array and tetrahedral anions. Since the cation:anion ratio is 2:1 in antifluorite and the cation coordination is 4, the anion coordination must be 8, Fig. 1.30.

      The very different coordination environments of anions and cations leads to two entirely distinct descriptions of the structure in terms of a 3D network of either tetrahedra or cubes, Fig. 1.34; (a) corresponds to the arrangement shown in Fig. 1.29(c) and the tetrahedra are highlighted; (b) corresponds to the arrangement in Fig. 1.30(b) in which the cubic coordination arrangement is highlighted. A more extended network of corner‐and edge‐sharing cubes is shown in Fig. 1.34(c). This must surely rate as one of the world's largest models of the antifluorite structure!

      The antifluorite structure is shown by a large number of oxides and other chalcogenides of the alkali metals (Table 1.10), i.e. compounds of general formula normal upper A 2 Superscript plus Baseline normal upper X Superscript 2 minus. A group of fluorides of large, divalent cations and oxides of large tetravalent cations have the inverse, fluorite, structure, i.e. M2+F2 and M4+O2.

      From Fig. 1.34(b) and (c), an alternative way of describing the fluorite structure is as a primitive cubic array of anions in which the eight‐coordinate sites at the cube body centres are alternately empty and occupied by a cation. It should be stressed that the true lattice type of fluorite is fcc and not primitive cubic, since the primitive cubes represent only a small part (one‐eighth) of the fcc unit cell. Description of fluorite as a primitive cubic array of anions with alternate cube body centres occupied by cations shows a similarity to the CsCl structure (see later). This also has a primitive cubic array of anions, but, instead, cations occupy all the body centre sites.

       Table 1.9 Some compounds with the zinc blende (sphalerite) structure, a/Å

CuF 4.255 BeS 4.8624 β‐CdS 5.818 BN 3.616 GaP 5.448
CuCl 5.416 BeSe 5.07 CdSe 6.077 BP 4.538 GaAs 5.6534
γ‐CuBr 5.6905 BeTe 5.54 CdTe 6.481 BAs 4.777

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