Book contents
- The Rock Physics Handbook
- Reviews
- The Rock Physics Handbook
- Copyright page
- Contents
- Preface to the Third Edition
- 1 Basic Tools
- 2 Elasticity and Hooke’s Law
- 3 Seismic Wave Propagation
- 4 Effective Elastic Media: Bounds and Mixing Laws
- 5 Granular Media
- 6 Fluid Effects on Wave Propagation
- 7 Empirical Relations
- 8 Flow and Diffusion
- 9 Electrical Properties
- Appendices
- References
- Index
1 - Basic Tools
Published online by Cambridge University Press: 05 March 2020
- The Rock Physics Handbook
- Reviews
- The Rock Physics Handbook
- Copyright page
- Contents
- Preface to the Third Edition
- 1 Basic Tools
- 2 Elasticity and Hooke’s Law
- 3 Seismic Wave Propagation
- 4 Effective Elastic Media: Bounds and Mixing Laws
- 5 Granular Media
- 6 Fluid Effects on Wave Propagation
- 7 Empirical Relations
- 8 Flow and Diffusion
- 9 Electrical Properties
- Appendices
- References
- Index
Summary
In this section, we use the symbol s to represent the frequency, or Fourier transform variable, following the terminology of Bracewell (1965). When x refers to time, the symbol f is often used for frequency instead of s; when x refers to space, the symbol k is often used for spatial frequency instead of s. Do not confuse this with the use of s when defining the Laplace transform (Section 1.3) or S when defining the analytic signal (Section 1.2).
- Type
- Chapter
- Information
- The Rock Physics Handbook , pp. 1 - 36Publisher: Cambridge University PressPrint publication year: 2020