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Oxford Cryosystems North America
Author(s) -
Oxford Cryosystems
Publication year - 1999
Publication title -
journal of applied crystallography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.429
H-Index - 162
ISSN - 1600-5767
DOI - 10.1107/s002188989901167x
Subject(s) - geography
crystal and non-crystalline (amorphous). All have periodicity ranging from perfect for a single-crystal to essentially nonexistential (sic) for the amorphous state.' Why a polycrystalline material is a separate state is not clari®ed. `Parallelipiped' is used in a discussion of what the authors refer to as `planar lattices' that is so involved as to obscure their signi®cance, though it is eventually de®ned correctly. There is a good discussion of Miller indices, with many examples, but there is recurring confusion between lattice points and atom site occupancy, e.g. `The motif placed on (sic) each lattice point . . . '; a `symmorphic space group exists when only a single atom or ion exists at the Bravais lattice points . . . '. Finally, to gladden the heart of every crystallographer, `The actual atomic positions are obtainable from the analysis of the lattice of a crystal.' and `Knowing the space group and equipoints . . . one can readily determine the crystal structure and arrangement of the atoms or ions in the unit cell or crystal.'. X-ray diffraction intensities and structure factors are never mentioned and although International Tables for Crystallography are mentioned once in a parenthesis in the text, there is no reference to them in the Reference section or in the index. Ch. 3 deals with crystal structures and contains sections on space ®lling by atoms, simple binary ionic crystals, more complex structures with closest packing such as perovskites and spinels, and covalent crystals. It is a standard treatment of topics found in all books dealing with solid-state chemistry. The concluding chapter deals extensively with polymorphism, thermodynamic discussion of phase changes, and various types of transformation with illustrative examples such as in quartz. There are also discussions of defects, substitution and silicate structures. But even here the very ®rst equation of the chapter has `The free energy change with temperature and pressure is given by: G E P V ÿ T S