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Heat Transport and Energetics of the Earth and Rocky Planets provides a better understanding of the interior of the Earth by addressing the processes related to the motion of heat in large bodies. By addressing issues such as the effect of self-gravitation on the thermal state of the Earth, the effect of length-scales on heat transport, important observations of Earth, and a comparison to the behavior of other rocky bodies, readers will find clearly delineated discussions on the thermal state and evolution of the Earth. Using a combination of fundamentals, new developments and scientific and mathematical principles, the book summarizes the state-of-the-art. This timely reference is an important resource for geophysicists, planetary scientists, geologists, geochemists, and seismologists to gain a better understanding of the interior, formation and evolution of planetary bodies. Provides an interdisciplinary approach to the understanding of the thermal evolution of large planetary bodies, including contributed chapters from leading experts Includes relevant observations of Earth and large-scale heat transfer, a critical review of existing paradigms of the current thermal state of the Earth, and a discussion of heat flow on the other rocky planets Covers macroscopic phenomena as they pertain to deciphering the thermal structure of planetary bodies
Heat provides the energy that drives almost all geological phenomena and sets the temperature at which these phenomena operate. This book explains the key physical principles of heat transport with simple physical arguments and scaling laws that allow quantitative evaluation of heat flux and cooling conditions in a variety of geological settings and systems. The thermal structure and evolution of magma reservoirs, the crust, the lithosphere and the mantle of the Earth are reviewed within the context of plate tectonics and mantle convection - illustrating how theoretical arguments can be combined with field and laboratory data to arrive at accurate interpretations of geological observations. Appendices contain data on the thermal properties of rocks, surface heat flux measurements and rates of radiogenic heat production. This book can be used for advanced courses in geophysics, geodynamics and magmatic processes, and is a reference for researchers in geoscience, environmental science, physics, engineering and fluid dynamics.
This book includes new results of theoretical and experimental studies of various scales of the processes occurring on the earth including the lithosphere, atmosphere, and hydrosphere. Intensive development of research in these areas is due to several factors: 1) the widespread introduction of computer technology, allowing the calculation of complex phenomena; 2) the invention and improvement of a new generation of geophysical instruments such as remote observation systems based on ships, aircraft, and satellites, providing a large amount of data to objectively reflect a broad picture of the processes; and 3) the development of measurement techniques, creating opportunities for controllable and reproducible laboratory data acquisition for generation of new ideas and concepts. Their recent developments have facilitated our research and understanding of these academic fields. The book enriches the understanding of the geophysical processes taking place in various environments (lithosphere, hydrosphere, and atmosphere), including the anthropogenic one, and it further contributes to their development. This book is a valuable resource for specialists working in the oil, gas, and engineering industry to improve their understandings of the field.
"Heat provides the energy that drives almost all geological phenomena and sets the temperature at which these phenomena operate. This book explains the key physical principles of heat transport with simple physical arguments and scaling laws that allow quantitative evaluation of heat flux and cooling conditions in a variety of geological settings and systems. The thermal structure and evolution of magma reservoirs, the crust, the lithosphere and the mantle of the Earth are reviewed within the context of plate tectonics and mantle convection - illustrating how theoretical arguments can be combined with field and laboratory data to arrive at accurate interpretations of geological observations. Appendices contain data on the thermal properties of rocks, surface heat flux measurements and rates of radiogenic heat production. This book can be used for advanced courses in geophysics, geodynamics and magmatic processes, and is a reference for researchers in geoscience, environmental science, physics, engineering and fluid dynamics"--
Fluid-Solid Interactions in Upstream Oil and Gas Applications, Volume 78 delivers comprehensive understanding of fluid-rock interactions in oil and gas reservoirs and their impact on drilling, production, and reservoir hydrocarbon management. The book is arranged based on intervals of the oil and gas production process and introduces the basics of reservoir fluids and their properties, along with the rheological behavior of solid-fluid systems across all stages of the reservoir, including drilling processes, acidizing, and fracking. The reference then addresses different application-specific issues, such as solid-fluid interactions in tight reservoirs, the applications of nanoparticles, interactions during the EOR processes, and environmental concerns. Introduces the basics of reservoir fluids and their properties as well as the rheological behavior of solid-fluid systems Discusses the latest advances in molecular simulations and their reliability Highlights the environmental concerns regarding the application of fluid-solid systems
Energy at the surface of the earth : an introduction to the energetics of ecosystems
"This unusual book, published to honor Warren Bell Hamilton, comprises a diverse, cross-disciplinary collection of bold new ideas in Earth and planetary science. This volume is a rich resource for researchers at all levels looking for interesting, unusual, and off-beat ideas to investigate or set as student projects"--
(cont.) These results are diagnosed in the context of simple models and scalings which compare the strength of the atmospheric and oceanic circulations and the energy contrasts across the flows. Parallels are drawn with present and paleo climate. Finally, I produce a new estimate of the total meridional heat transport employing the method of minimum variance estimation, data from the Clouds and the Earth's Radiant Energy System instruments, and a prior estimate. This new estimate yields a peak poleward heat transport of 5.6 ± 0.8 PW at 35°N and 35°S with a northward transport of 0.1 ± 0.9 PW at the equator. This represents a 27% reduction in the standard error relative to the prior estimate. An estimate of the partition is made using direct ocean heat transport estimates with the atmospheric component computed as a residual.
This book deals with the signatures left by geodynamic proceses in the temperature field of the Earth's crust. First, it introduces briefly the established, indirect methods for interpreting the present termperature field and methods for reconstructing the thermal fields of the geological past. Then the spatial and temporal scales that are relevant for heat transport processes are described. This problem is discussed both theoretically and on the basis of data from the German Continental Deep Drilling Program (KTB). The climate of the last 200 years and the postglacial warming in central Europe are reconstructed on the basis of two sets of temperature data from shallow and deep boreholes. This book is written for an audience at an advanced undergraduate or graduate level with an understanding of basic physical principles. It avoids particular terminology, and special terms are introduced.