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Covalent Bonding: Orbitals (cont’d)
Chapter 10 (c) Covalent Bonding: Orbitals (cont’d)
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Figure 10. 22: The structures of diamond and graphite
Figure 10.22: The structures of diamond and graphite. In each case only a small part of the entire structure is shown.
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Figure 10.23: Partial representation of the molecular orbital energies in (a) diamond and (b) a typical metal. Copyright © Houghton Mifflin Company. All rights reserved.
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Figure 10.24: The p orbitals (a) perpendicular to the plane of the carbon ring system in graphite can combine to form (b) an extensive π-bonding network. Copyright © Houghton Mifflin Company. All rights reserved.
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Figure 10.25: Graphite consists of layers of carbon atoms.
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Computer-generated model of silica.
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Figure 10. 26: (top) The structure of quartz (empirical formula SiO2)
Figure 10.26: (top) The structure of quartz (empirical formula SiO2). Quartz contains chains of SiO4 tetrahedra (bottom) that share oxygen atoms.
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Figure 10.27: Examples of silicate anions, all of which are based on SiO44- tetrahedra.
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Figure 10.28: Two-dimensional representations of (a) a quartz crystal and (b) a quartz glass.
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Figure 10.29: (a) A silicon crystal doped with arsenic, which has one more valence electron than silicon. (b) A silicon crystal doped with boron, which has one less electron than silicon.
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