
Numerical Modelling and Analysis of Fluid Flow and Deformation of Fractured Rock Masses.
Title:
Numerical Modelling and Analysis of Fluid Flow and Deformation of Fractured Rock Masses.
Author:
Zhang, Xing.
ISBN:
9780080537863
Personal Author:
Edition:
1st ed.
Physical Description:
1 online resource (301 pages)
Contents:
Front Cover -- Numerical Modelling and Analysis of Fluid Flow and Deformation of Fractured Rock Masses -- Copyright Page -- Contents -- Preface -- Chapter 1. Introduction to Modelling Deformation and Fluid Flow of Fractured Rock -- 1.1. Introduction -- 1.2. Approaches to modelling rock systems -- 1.3. Continuum models -- 1.4. Flow models -- 1.5. Discontinuum models -- 1.6. Overview of UDEC -- 1.7. Summary of numerical modelling -- Chapter 2. Modelling of Simple Rock Blocks -- 2.1. Introduction -- 2.2. Basic components of natural fracture networks -- 2.3. Model geometry and initial conditions -- 2.4. Basic behaviour of deformation and fluid flow -- 2.5. Effects of fracture geometry -- 2.6. Effects of fracture properties -- 2.7. Effects of applied boundary stresses -- 2.8. Effects of rock deformation models -- 2.9. Summary -- Chapter 3. Evaluation of 2-Dimensional Permeability Tensors -- 3.1. Introduction -- 3.2. Calculation of components of flow-rates -- 3.3. Permeability in naturally fractured rocks -- 3.4. Geometrical effects on permeability -- 3.5. Effects of stress on permeability -- 3.6. Conclusions -- Appendix 3-A 1: Input codes for example one -- Appendix 3-A2: Derivation of 2-D permeability tensor -- Chapter 4. Scaling of 2-D Permeability Tensors -- 4.1. Introduction -- 4.2. Development of the previous approach -- 4.3. Testing the concept of a representative element volume by down-scaling -- 4.4. Scaling-up of permeability -- 4.5. Effects of sample number and sample size -- 4.6. Determining the permeability of a region -- 4.7. Conclusions -- Chapter 5. Percolation Behaviour of Fracture Networks -- 5.1. Introduction -- 5.2. Modelling of 2-dimensional fracture networks -- 5.3. Density, percolation threshold and fractal dimension -- 5.4. Critical behaviour of fractured rock masses -- 5.5. Conclusions.
Chapter 6. Slip and Fluid Flow around An Extensional Fault -- 6.1. Introduction -- 6.2. Outline of modelling -- 6.3. Stress distribution and fluid flow in model A: At a shallow depth with a hydrostatic fluid pressure -- 6.4. Comparison of model A with a supra-hydrostatic fluid pressure at greater depth -- 6.5. Effects of irregularities in fault zone -- 6.6. Discussion of dynamic response of fluid-dilation interactions -- 6.7. Conclusions -- Chapter 7. Instability and Associated Localization of Deformation and Fluid Flow in Fractured Rocks -- 7.1. Introduction -- 7.2. Numerical determination of instability -- 7.3. Instability and R-ratio -- 7.4. Effects of fracture network geometry -- 7.5. Multifractal description of flow localisation -- 7.6. Permeability of three natural fracture networks before and at critical stress state -- 7.7. Effects of loading direction -- 7.8. Is the crust in a critical state? -- 7.9. Implications for mineral deposits -- 7.10. Conclusions -- Chapter 8. Grain Scale Flow of Fluid in Fractured Rocks -- 8.1. Introduction -- 8.2. Simulation of Deformation and Fracturing in Matrix Models -- 8.3. Dual Permeability Model -- 8.4. Results -- 8.5. Discussion and Conclusions -- Chapter 9. Changes of Permeability due to Excavation of Ship-Locks of the Three Gorges Project, China -- 9.1. Introduction -- 9.2. Estimation of permeability -- 9.3. Permeability before excavation -- 9.4. Modelling of the excavation of the ship-locks -- 9.5. Permeability after excavation -- 9.6. Concluding discussion -- Chapter 10. Wellbore Instability due to "Block Loosening" in Fractured Rock Masses -- 10.1. Introduction -- 10.2. Model geometry and conditions used -- 10.3. Randomly isotropic fracture geometry with constant wellbore pressure -- 10.4. Randomly isotropic fracture geometry with increased or reduced wellbore pressure.
10.5. Comparison of different fracture patterns -- 10.6. Conclusions -- Appendix 10-A1: Analytic solution for a homogeneous medium -- Summary -- References -- Index.
Abstract:
Our understanding of the subsurface system of the earth is becoming increasingly more sophisticated both at the level of the behaviour of its components (solid, liquid and gas) as well as their variations in space and time. The implementation of coupled models is essential for the understanding of an increasing number of natural phenomena and in predicting human impact on these. The growing interest in the relation between fluid flow and deformation in subsurface rock systems that characterise the upper crust has led to increasingly specialized knowledge in many branches of earth sciences and engineering. A multidisciplinary subject dealing with deformation and fluid flow in the subsurface system is emerging. While research in the subject area of faulting, fracturing and fluid flow has led to significant progress in many different areas, the approach has tended to be "reductionist", i.e. involving the isolation and simplification of phenomena so that they may be treated as single physical processes. The reality is that many processes operate together within subsurface systems, and this is particularly true for fluid flow and deformation of fractured rock masses. The aim of this book is to begin to explore how advances in numerical modelling can be applied to understanding the complex phenomena observed in such systems. Although mainly based on original research, the book also includes the fundamental principles and practical methods of numerical modelling, in particular distinct element methods. This volume explores the principles of numerical modelling and the methodologies for some of the most important problems, in addition to providing practical models with detailed discussions on various topics.
Local Note:
Electronic reproduction. Ann Arbor, Michigan : ProQuest Ebook Central, 2017. Available via World Wide Web. Access may be limited to ProQuest Ebook Central affiliated libraries.
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