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
8 - Flow and Diffusion
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
It was established experimentally by Darcy () that the fluid flow rate in a fluid-saturated porous medium is linearly related to the pressure gradient by the following equation
- Type
- Chapter
- Information
- The Rock Physics Handbook , pp. 525 - 576Publisher: Cambridge University PressPrint publication year: 2020