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94  •  Chapter 3    /    The Structure of Crystalline Solids

                                •  Two features of a crystal structure are
                                     Coordination number—the number of nearest-neighbor atoms, and
                                     Atomic packing factor—the fraction of solid sphere volume in the unit cell.

                       Density   •  The theoretical density of a metal (r) is a function of the number of equivalent atoms per
                  Computations    unit cell, the atomic weight, unit cell volume, and Avogadro’s number (Equation 3.8).
               Polymorphism and   •  Polymorphism is when a specific material can have more than one crystal structure.
                      Allotropy   Allotropy is polymorphism for elemental solids.

                 Crystal Systems  •  The concept of a crystal system is used to classify crystal structures on the basis of unit
                                  cell geometry—that is, unit cell edge lengths and interaxial angles. There are seven
                                  crystal systems: cubic, tetragonal, hexagonal, orthorhombic, rhombohedral (trigonal),
                                  monoclinic, and triclinic.

               Point Coordinates  • Crystallographic points, directions, and planes are specified in terms of indexing
                                  schemes. The basis for the determination of each index is a coordinate axis system
                Crystallographic
                     Directions   defined by the unit cell for the particular crystal structure.
                                     The location of a point within a unit cell is specified using coordinates that are
                Crystallographic       fractional multiples of the cell edge lengths (Equations 3.9a–3.9c).
                        Planes       Directional indices are computed in terms of differences between vector head
                                       and tail coordinates (Equations 3.10a–3.10c).
                                     Planar (or Miller) indices are determined from the reciprocals of axial intercepts
                                       (Equations 3.14a–3.14c).
                                •  For hexagonal unit cells, a four-index scheme for both directions and planes is found
                                  to be more convenient. Directions may be determined using Equations 3.11a–3.11d
                                  and 3.12a–3.12d.

               Linear and Planar   •  Crystallographic directional and planar equivalencies are related to atomic linear and
                      Densities   planar densities, respectively.
                                     Linear density (for a specific crystallographic direction) is defined as the number
                                       of atoms per unit length whose centers lie on the vector for this direction
                                       (Equation 3.16).
                                     Planar density  (for a specific crystallographic plane) is taken as the number of
                                       atoms per unit area that are centered on the particular plane (Equation 3.18).
                                • For a given crystal structure, planes having identical atomic packing yet different
                                  Miller indices belong to the same family.
                  Close-Packed   • Both FCC and HCP crystal structures may be generated by the stacking of close-
               Crystal Structures  packed planes of atoms on top of one another. With this scheme A, B, and C denote
                                  possible atom positions on a close-packed plane.
                                     The stacking sequence for HCP is ABABAB. . . .
                                     The stacking sequence for FCC is ABCABCABC. . . .
                                •  Close-packed planes for FCC and HCP are  111  and  0001 , respectively.

                  Single Crystals  •  Single crystals  are materials in which the atomic order extends uninterrupted over
                                  the entirety of the specimen; under some circumstances, single crystals may have flat
                  Polycrystalline
                      Materials   faces and regular geometric shapes.
                                •  The vast majority of crystalline solids, however, are polycrystalline, being composed
                                  of many small crystals or grains having different crystallographic orientations.
                                • A grain boundary is the boundary region separating two grains where there is some
                                  atomic mismatch.
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