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Titlebook: Applied Hydrodynamics in Petroleum Exploration; Eric C. Dahlberg Book 1995Latest edition Springer-Verlag New York, Inc. 1995 Engineering G

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期刊全稱Applied Hydrodynamics in Petroleum Exploration
影響因子2023Eric C. Dahlberg
視頻videohttp://file.papertrans.cn/160/159856/159856.mp4
圖書封面Titlebook: Applied Hydrodynamics in Petroleum Exploration;  Eric C. Dahlberg Book 1995Latest edition Springer-Verlag New York, Inc. 1995 Engineering G
影響因子In the first edition of this book, we observed that it had been created to fill a need for a usable "self-contained volume on hydrodynamics" (and hydrogeology) that was written specifically for the petroleum industry, but could also serve the earth science community in general. When the first edition was published (1982), M. K. Hubbert, the father of petroleum hydrodynamics, was approaching the final stages of his very productive career. For this reason, the book served as a vehicle to amplify his concepts and spread and stimulate applications of some of his theories and methods throughout the exploration sectors of the petroleum industry. This was accomplished by blending discussions of Hubbert‘s concepts with some of the procedures used by industry specialists to answer practical oil and gas questions. The simple aim of the book was to bring this material to the fingertips of working geologists and geophysicists, who were "evaluating the hydrocarbon possibilities in larger exploration regions or assessing the potential of small, local subsurface oil and gas prospects. " It was also hoped that by treating areas of conceptual overlap between petroleum geology and ground water hydro
Pindex Book 1995Latest edition
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Potential Energy Variation in Fluids,sed up (converted to .) as the spring expands back to its original, presqueezed length. Potential energy is thus energy made by storing up the results of some active work. One does work in winding up tighter and tighter the spring inside a small toy car. When the car is released on the floor, the st
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Rock, Pore Space, and Fluid Systems,nment in terms of single bodies of homogeneous fluid. It is not really this way in a rock, however, since any single fluid mass is essentially interspersed within a network of intergranular pore spaces, throats, fracture openings, etc. As long as the fluids are in complete communication, the princip
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Nonnormal Formation Pressures, down to the depth of the measurement is termed ., even though for the conditions at hand it may be completely normal. The standard is assumed to be the local hydrostatic gradient from the surface, and this gradient is termed .. The relationships for different pressures measured beneath the surface
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Pressure Variation with Depth,om simple graphical plots of formation pressure against the depths (or elevation) at which they are measured. There are essentially three exploration problem areas in which such P—D plots are applied: the first concerns the prediction of pay thickness (i.e., placing oil-water, gas-water, and gas-oil
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Potentiometric Maps and Subsurface Water Flow,ion water within a particular aquifer or subsurface reservoir. The elevation of the surface at any point on it reflects (but does not exactly equal) the height to which a column of water would rise above a reference datum within a vertical tube (ignoring capillarity). This is an approximation of the
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Entrapment Potential Maps,cannot escape in any direction. One classification scheme, devised by Meissner (1984) and illustrated in Figure 11.1, proposes a three end-member system constituting a triangle. The three end-members in the scheme occupy positions at its apices: . (lower left), . (lower right), and . (top center). S
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