Geophysical and Geochemical Analyses of Flow and Deformation in Fractured Rock PDF Download
Are you looking for read ebook online? Search for your book and save it on your Kindle device, PC, phones or tablets. Download Geophysical and Geochemical Analyses of Flow and Deformation in Fractured Rock PDF full book. Access full book title Geophysical and Geochemical Analyses of Flow and Deformation in Fractured Rock by Joshua Taron. Download full books in PDF and EPUB format.
Author: Joshua Taron
Publisher:
ISBN:
Category :
Languages : en
Pages : 198
Get Book Here
Book Description
The following is a study of fluid flow and deformation in fractured rock, with particular emphasis on environments under thermal and chemical stress. Fractures are treated in the greatest detail, with constitutive modeling at pore and reservoir scale, and their impact explored with reservoir scale numerical simulation. Part I (Chapters I-IV) explores the behavior of engineered systems pushed far from equilibrium and highlights feedbacks between stress and chemistry on the evolution of the mechanical and transport properties of rocks; these observations and analyses are focused on the behavior of geothermal reservoirs. Part II (Chapters V-VI) examines the response to natural forcing and follows the complex interactions that shape processes in volcanic environments. Chapter I introduces a simulator to examine thermal, hydrologic, mechanical, and chemical processes (THMC) in deformable, fractured porous media. The combined influence of stress-enhanced dissolution, thermal-hydro-mechanical asperity strain, and mineral reaction alter the permeability of fractures during thermal, hydraulic, and chemical stimulation. Chapter II examines a prototypical enhanced geothermal system (EGS) for the relative, temporal arrival of hydro-mechanical vs. thermo-mechanical vs. chemical changes in fluid transmission as cold water is injected at geochemical disequilibrium within a heated reservoir. Chapter III develops a relationship to examine dissolution precipitation creep in crustal rocks with implicit coupling of the dissolution-diffusion-precipitation system. Long-term compaction, previously ill-constrained, is explored with two alternate methods. Chapter IV presents a model to represent these permeability change mechanisms as innately hysteretic and interlinked processes in rough contacting fractures. This model is incorporated into the numerical simulator of Chapters I and II and applied to a candidate engineered geothermal reservoir system (EGS). Utilizing a several year history of rainfall, seismic, and magma effux records, Chapter V presents a limit-equilibrium model for rainfall infiltration into a hot lava carapace to evolve stability of the dome at Soufrière Hills Volcano (SHV). Model predictions are compared to observed dome collapse events from2000-2002 . In Chapter VI histories of magma efflux and surface deformation are utilized to geodetically image magma transfer within the deep crustal plumbing system of SHV. Magma efflux is constrained with wide-aperture geodetic data to supplement a well-documented extrusion record, and these are used to explore the role of deeply sourced fluxes on short-term eruption periodicity.
Author: Joshua Taron
Publisher:
ISBN:
Category :
Languages : en
Pages : 198
Get Book Here
Book Description
The following is a study of fluid flow and deformation in fractured rock, with particular emphasis on environments under thermal and chemical stress. Fractures are treated in the greatest detail, with constitutive modeling at pore and reservoir scale, and their impact explored with reservoir scale numerical simulation. Part I (Chapters I-IV) explores the behavior of engineered systems pushed far from equilibrium and highlights feedbacks between stress and chemistry on the evolution of the mechanical and transport properties of rocks; these observations and analyses are focused on the behavior of geothermal reservoirs. Part II (Chapters V-VI) examines the response to natural forcing and follows the complex interactions that shape processes in volcanic environments. Chapter I introduces a simulator to examine thermal, hydrologic, mechanical, and chemical processes (THMC) in deformable, fractured porous media. The combined influence of stress-enhanced dissolution, thermal-hydro-mechanical asperity strain, and mineral reaction alter the permeability of fractures during thermal, hydraulic, and chemical stimulation. Chapter II examines a prototypical enhanced geothermal system (EGS) for the relative, temporal arrival of hydro-mechanical vs. thermo-mechanical vs. chemical changes in fluid transmission as cold water is injected at geochemical disequilibrium within a heated reservoir. Chapter III develops a relationship to examine dissolution precipitation creep in crustal rocks with implicit coupling of the dissolution-diffusion-precipitation system. Long-term compaction, previously ill-constrained, is explored with two alternate methods. Chapter IV presents a model to represent these permeability change mechanisms as innately hysteretic and interlinked processes in rough contacting fractures. This model is incorporated into the numerical simulator of Chapters I and II and applied to a candidate engineered geothermal reservoir system (EGS). Utilizing a several year history of rainfall, seismic, and magma effux records, Chapter V presents a limit-equilibrium model for rainfall infiltration into a hot lava carapace to evolve stability of the dome at Soufrière Hills Volcano (SHV). Model predictions are compared to observed dome collapse events from2000-2002 . In Chapter VI histories of magma efflux and surface deformation are utilized to geodetically image magma transfer within the deep crustal plumbing system of SHV. Magma efflux is constrained with wide-aperture geodetic data to supplement a well-documented extrusion record, and these are used to explore the role of deeply sourced fluxes on short-term eruption periodicity.
Author: Committee on Fracture Characterization and Fluid Flow
Publisher: National Academies Press
ISBN: 0309563488
Category : Science
Languages : en
Pages : 568
Get Book Here
Book Description
Scientific understanding of fluid flow in rock fractures--a process underlying contemporary earth science problems from the search for petroleum to the controversy over nuclear waste storage--has grown significantly in the past 20 years. This volume presents a comprehensive report on the state of the field, with an interdisciplinary viewpoint, case studies of fracture sites, illustrations, conclusions, and research recommendations. The book addresses these questions: How can fractures that are significant hydraulic conductors be identified, located, and characterized? How do flow and transport occur in fracture systems? How can changes in fracture systems be predicted and controlled? Among other topics, the committee provides a geomechanical understanding of fracture formation, reviews methods for detecting subsurface fractures, and looks at the use of hydraulic and tracer tests to investigate fluid flow. The volume examines the state of conceptual and mathematical modeling, and it provides a useful framework for understanding the complexity of fracture changes that occur during fluid pumping and other engineering practices. With a practical and multidisciplinary outlook, this volume will be welcomed by geologists, petroleum geologists, geoengineers, geophysicists, hydrologists, researchers, educators and students in these fields, and public officials involved in geological projects.
Author: Xing Zhang
Publisher: Elsevier
ISBN: 0080537863
Category : Science
Languages : en
Pages : 301
Get Book Here
Book Description
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.
Author: John M. Sharp
Publisher: CRC Press
ISBN: 1315778823
Category : Science
Languages : en
Pages : 403
Get Book Here
Book Description
Understanding of groundwater flow and solute transport in fractured rocks is vital for analysis of water resources, water quality and environmental protection, geotechnical and engineering projects, and geothermal energy production. This book includes theoretical and practical analyses using numerical modelling, geochemistry, isotopes, aquifer tests, laboratory tests, field mapping, geophysics, geological analyses, and some unique combinations of these types of investigation. Current water resource and geotechnical problems and the techniques now used are also discussed. Aimed at practicing hydrogeologists, engineers, ecologists, resource managers, students and earth scientists.
Author: Hugh Corey Heard
Publisher: American Geophysical Union
ISBN: 087590016X
Category : Science
Languages : en
Pages : 356
Get Book Here
Book Description
Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 16 (The Griggs Volume). David Tressel Griggs was born October 6, 1911, in Columbus, Ohio. His parents were Robert Fiske and Laura Amelia Tressel Griggs. His father was a widely known professor of botany and a leading ecologist and environmental conservationist at a time when these viewpoints were less familiar than they are today. David was an undergraduate at Ohio State University in 1930 when he participated in a National Geographic Society expedition, led by his father, to the Valley of Ten Thousand Smokes. This Alaskan experience and the encouragement he received from a gifted and enthusiastic teacher, Professor Edmund M. Spieker, led him to choose for his life work the application of physics to the problems of the earth. After a year of graduate studies in geology at Ohio State, David moved on in 1933 to Harvard, where a new progTam of high-pressure studies devoted to geophysical problems had just been initiated under the inspired guidance of Percy W. Bridgman, pre-eminent leader in the experimental exploration of the physics of very high pressures and in the philosophical analysis of the logical processes of scientific thinking.
Author: Robert W. Zimmerman
Publisher: John Wiley & Sons
ISBN: 1119248027
Category : Science
Languages : en
Pages : 293
Get Book Here
Book Description
FLUID FLOW IN FRACTURED ROCKS "The definitive treatise on the subject for many years to come" (Prof. Ruben Juanes, MIT) Authoritative textbook that provides a comprehensive and up-to-date introduction to fluid flow in fractured rocks Fluid Flow in Fractured Rocks provides an authoritative introduction to the topic of fluid flow through single rock fractures and fractured rock masses. This book is intended for readers with interests in hydrogeology, hydrology, water resources, structural geology, reservoir engineering, underground waste disposal, or other fields that involve the flow of fluids through fractured rock masses. Classical and established models and data are presented and carefully explained, and recent computational methodologies and results are also covered. Each chapter includes numerous graphs, schematic diagrams and field photographs, an extensive reference list, and a set of problems, thus providing a comprehensive learning experience that is both mathematically rigorous and accessible. Written by two internationally recognized leaders in the field, Fluid Flow in Fractured Rocks includes information on: Nucleation and growth of fractures in rock, with a multiscale characterization of their geometric traits Effect of normal and shear stresses on the transmissivity of a rock fracture and mathematics of fluid flow through a single rock fracture Solute transport in rocks, with quantitative descriptions of advection, molecular diffusion, and dispersion Fluid Flow in Fractured Rocks is an essential resource for researchers and postgraduate students who are interested in the field of fluid flow through fractured rocks. The text is also highly suitable for professionals working in civil, environmental, and petroleum engineering.
Author: B. Jamtveit
Publisher: Springer Science & Business Media
ISBN: 9400915330
Category : Science
Languages : en
Pages : 330
Get Book Here
Book Description
This book represents the proceedings of the 9th written by a very active group of physicists at Kongsberg seminar, held at the Norwegian Mining the University of Oslo - physicists interested in Museum located in the city of Kongsberg about complex systems in general and geo-like systems 70 km Southwest of Oslo. The Kongsberg district in particular. is known for numerous Permian vein deposits of The content of the book is organized into three native silver, and mining activity in the area lasted major parts following the introductory chapter. for more than 300 years, finally ceasing in 1957. Chapters 2 to 7 primarily treat the role of fluids The previous eight Kongsberg seminars were in specific geological environments, ranging from focused on ore-forming processes and all of these sedimentary basins (Chapters 2-3) to contact were organized by Professor Arne Bj0rlykke, now metamorphic/hydrothermal scenarios (Chapters director of the Norwegian Geological Survey. 4-5) and regional metamorphic settings (Chapters Since process-orientated research tends to break 6-7). The following four chapters (8-11) focus down the traditional barriers between the different on various properties of fluid-rock systems that geological disciplines, this seminar has always are critical in controlling flow and transport been a meeting point for people with a variety through rocks. These include: mineral solubility of geological backgrounds.
Author: National Academies of Sciences, Engineering, and Medicine
Publisher: National Academies Press
ISBN: 0309373727
Category : Science
Languages : en
Pages : 177
Get Book Here
Book Description
Fractured rock is the host or foundation for innumerable engineered structures related to energy, water, waste, and transportation. Characterizing, modeling, and monitoring fractured rock sites is critical to the functioning of those infrastructure, as well as to optimizing resource recovery and contaminant management. Characterization, Modeling, Monitoring, and Remediation of Fractured Rock examines the state of practice and state of art in the characterization of fractured rock and the chemical and biological processes related to subsurface contaminant fate and transport. This report examines new developments, knowledge, and approaches to engineering at fractured rock sites since the publication of the 1996 National Research Council report Rock Fractures and Fluid Flow: Contemporary Understanding and Fluid Flow. Fundamental understanding of the physical nature of fractured rock has changed little since 1996, but many new characterization tools have been developed, and there is now greater appreciation for the importance of chemical and biological processes that can occur in the fractured rock environment. The findings of Characterization, Modeling, Monitoring, and Remediation of Fractured Rock can be applied to all types of engineered infrastructure, but especially to engineered repositories for buried or stored waste and to fractured rock sites that have been contaminated as a result of past disposal or other practices. The recommendations of this report are intended to help the practitioner, researcher, and decision maker take a more interdisciplinary approach to engineering in the fractured rock environment. This report describes how existing tools-some only recently developed-can be used to increase the accuracy and reliability of engineering design and management given the interacting forces of nature. With an interdisciplinary approach, it is possible to conceptualize and model the fractured rock environment with acceptable levels of uncertainty and reliability, and to design systems that maximize remediation and long-term performance. Better scientific understanding could inform regulations, policies, and implementation guidelines related to infrastructure development and operations. The recommendations for research and applications to enhance practice of this book make it a valuable resource for students and practitioners in this field.
Author: Ken McCaffrey
Publisher: Geological Society of London
ISBN: 9781862390348
Category : Science
Languages : en
Pages : 340
Get Book Here
Book Description
Hydrothermal mineralization is usually structurally controlled so it is important to understand the role of faulting and fracturing in enhancing rock permeability and facilitating fluid flow and mass transfer. This is the main theme of this interdisciplinary volume and the papers included are intended to provide an overview of current ideas at the interfaces of structural geology, fluid flow and mineralization research.
Author: I. Stober
Publisher: Springer Science & Business Media
ISBN: 9401718164
Category : Science
Languages : en
Pages : 277
Get Book Here
Book Description
Hydrogeology of Crystalline Rocks deals with deep groundwater in the granite and gneiss basement of the continents. It has become evident during the past years that highly mineralized water is present in an interconnected fracture network of the basement. Thus, the upper part of the crust of the continents can be viewed as an aquifer and investigated with tools common in hydrogeology. This book presents accounts on water-conducting features of crystalline rocks and summarizes the hydraulic properties of the basement. The volume includes reviews, new data and research on the often remarkable chemical composition of deep groundwater. Microbial processes in the deep basement aquifer are probably more important than previously thought. Two contributions focus on this recent extension of research of the biosphere to greater depth in the Earth. This book represents the first multidisciplinary and integrated account of deep groundwater hydrology in crystalline basement. It is of interest to hydrologists and hydrogeologists working with water in crystalline rocks, but also to solid earth geophysicists, geochemists and petrologists with an interest in fluids in the crust. Scientists involved in nuclear waste disposal programs and geothermal energy development will find a wealth of stimulating ideas in this volume.
