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Crustal Permeability.
Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures.
| Call Number: | Libro Electrónico |
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| Main Author: | |
| Other Authors: | |
| Format: | Electronic eBook |
| Language: | Inglés |
| Published: |
Newark :
Wiley,
2016.
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| Subjects: | |
| Online Access: | Texto completo |
Table of Contents:
- Cover ; Title Page ; Copyright ; Dedication ; Contents ; List of contributors ; About the companion websites ; Chapter 1 Introduction ; Motivation and background ; Nomenclature: porosity, permeability, hydraulic conductivity, and relative permeability.
- Static versus dynamic permeability Contents of this book ; Data structures to integrate and extend existing knowledge ; Acknowledgments ; Chapter 2 DigitalCrust
- a 4D data system of material properties for transforming research on crustal fluid flow ; Motivation.
- Data integration to transform science The DigitalCrust vision ; An action plan ; Concluding remarks ; Acknowledgments ; Part I The physics of permeability ; Chapter 3 The physics of permeability.
- Chapter 4 A pore-scale investigation of the dynamic response of saturated porous media to transient stresses Introduction ; Background ; Methods ; Results ; Discussion ; Conclusions ; Acknowledgments.
- Chapter 5 Flow of concentrated suspensions through fractures: small variations in solid concentration cause significant in-plane velocity variations Introduction ; Overview of experiments ; Image analysis ; Experimental results ; Computational simulations ; Concluding remarks.