Book contents
- Frontmatter
- Contents
- Preface
- 1 The basics of X-ray diffraction theory
- 2 The Patterson and heavy-atom methods
- 3 Direct methods
- 4 The basics of isomorphous replacement and anomalous scattering
- 5 Further aspects of the isomorphous replacement method
- 6 Use of anomalous scattering data
- 7 Phase extension and refinement
- 8 Multiple-beam scattering methods
- References
- Sources of non-original figures
- Index
Preface
Published online by Cambridge University Press: 24 November 2009
- Frontmatter
- Contents
- Preface
- 1 The basics of X-ray diffraction theory
- 2 The Patterson and heavy-atom methods
- 3 Direct methods
- 4 The basics of isomorphous replacement and anomalous scattering
- 5 Further aspects of the isomorphous replacement method
- 6 Use of anomalous scattering data
- 7 Phase extension and refinement
- 8 Multiple-beam scattering methods
- References
- Sources of non-original figures
- Index
Summary
When von Laue and his assistants produced their first smudgy X-ray diffraction photographs in Munich in 1912 they could not have known of the developments that would follow and the impact that these would have on such a wide range of science. Structural crystallography, the ability to find the arrangement of atoms inside crystals, has advanced over the years both theoretically and experimentally. Technical advances, such as the development of computers both for control of instruments and for complex calculations, and also the advent of high power synchrotron X-ray sources have all played their part.
In this book we bring together all the methods that have been and are being used to solve crystal structures. We broadly divide these methods into two main classes, non-physical and physical methods. In the first category we place those methods that depend on a single set of diffraction data produced by the normal Thomson scattering from the individual atoms. The Patterson methods and direct methods described in chapters 2 and 3 respectively are non-physical methods. In chapter 4 the basic principles are explained for two physical methods – isomorphous replacement, which combines the data from two or more related compounds to obtain phase information, and anomalous scattering, which uses data at wavelengths for which some of the atoms scatter anomalously, i.e. with an amplitude and phase differing from that given by the Thomson process. In chapter 5 the method of isomorphous replacement is explored in much greater depth and in chapter 6 the same is done for anomalous scattering.
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- Chapter
- Information
- Publisher: Cambridge University PressPrint publication year: 1995