派博傳思國際中心

標(biāo)題: Titlebook: Applied Hydrodynamics in Petroleum Exploration; Eric C. Dahlberg Book 1995Latest edition Springer-Verlag New York, Inc. 1995 Engineering G [打印本頁]

作者: 惡夢    時間: 2025-3-21 17:02
書目名稱Applied Hydrodynamics in Petroleum Exploration影響因子(影響力)




書目名稱Applied Hydrodynamics in Petroleum Exploration影響因子(影響力)學(xué)科排名




書目名稱Applied Hydrodynamics in Petroleum Exploration網(wǎng)絡(luò)公開度




書目名稱Applied Hydrodynamics in Petroleum Exploration網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Applied Hydrodynamics in Petroleum Exploration被引頻次




書目名稱Applied Hydrodynamics in Petroleum Exploration被引頻次學(xué)科排名




書目名稱Applied Hydrodynamics in Petroleum Exploration年度引用




書目名稱Applied Hydrodynamics in Petroleum Exploration年度引用學(xué)科排名




書目名稱Applied Hydrodynamics in Petroleum Exploration讀者反饋




書目名稱Applied Hydrodynamics in Petroleum Exploration讀者反饋學(xué)科排名





作者: Permanent    時間: 2025-3-21 21:06

作者: 山羊    時間: 2025-3-22 01:40
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
作者: 凈禮    時間: 2025-3-22 08:09
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
作者: IOTA    時間: 2025-3-22 10:32
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
作者: 表狀態(tài)    時間: 2025-3-22 15:29
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
作者: 指令    時間: 2025-3-22 17:31
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
作者: 拖債    時間: 2025-3-22 22:05

作者: CLEAR    時間: 2025-3-23 02:36

作者: grounded    時間: 2025-3-23 07:29
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
作者: homeostasis    時間: 2025-3-23 12:46

作者: 細(xì)絲    時間: 2025-3-23 17:02
Productive Market-Oriented Enterprisester. The heavier the fluid, the shorter the column required to balance a particular internal pressure. For example, the height of a column of dense brine required to offset a given pressure in a formation might be only 90% that of a column of fresh water.
作者: 流浪    時間: 2025-3-23 18:28
Potentiometric Maps and Subsurface Water Flow,ter. The heavier the fluid, the shorter the column required to balance a particular internal pressure. For example, the height of a column of dense brine required to offset a given pressure in a formation might be only 90% that of a column of fresh water.
作者: misanthrope    時間: 2025-3-24 01:05

作者: Mucosa    時間: 2025-3-24 02:32

作者: Fallibility    時間: 2025-3-24 10:17

作者: Encumber    時間: 2025-3-24 12:00

作者: Clumsy    時間: 2025-3-24 14:53
Entrapment Potential Cross Sections,ressure, within the formation water, is at the highest point in the reservoir, which is the crest of the structure. The equipressure planes are oriented horizontally, as illustrated by the dashed lines in Figure 10.2.
作者: antiandrogen    時間: 2025-3-24 22:16
https://doi.org/10.1007/978-1-4842-8628-9 interfaces); the second concerns subsurface correlation and the prediction of prospective reservoir trends; the third involves the recognition of subsurface barriers and the definition of geologic pressure systems and placement of boundaries with respect to over- and underpressuring.
作者: 織布機(jī)    時間: 2025-3-25 02:16
(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
作者: 不來    時間: 2025-3-25 06:47

作者: spondylosis    時間: 2025-3-25 09:17
https://doi.org/10.1007/978-981-15-2121-8e, he showed that the slope on the potentiometric surface in the vicinity of the hydrocarbon accumulation that reflects the water flow is numerically related to the tilt on the hydrocarbon-water contact by a factor determined by the contrast between the densities of the underlying dynamic water phase and the overlying static oil or gas phase.
作者: tenosynovitis    時間: 2025-3-25 14:22

作者: Amorous    時間: 2025-3-25 18:35

作者: 揭穿真相    時間: 2025-3-25 23:10
Pressure Variation with Depth, interfaces); the second concerns subsurface correlation and the prediction of prospective reservoir trends; the third involves the recognition of subsurface barriers and the definition of geologic pressure systems and placement of boundaries with respect to over- and underpressuring.
作者: 防水    時間: 2025-3-26 03:53

作者: 使長胖    時間: 2025-3-26 04:49
Fluids, Pressures, and Gradients,To facilitate the following treatment of the subject of applied hydrodynamics in petroleum exploration and formation pressure geology, it is necessary to review some of the basic attributes of fluids. We will then be able to discuss the way fluids respond to external and internal influences in different subsurface geohydrologic environments.
作者: BLANK    時間: 2025-3-26 11:48
https://doi.org/10.1007/978-3-658-43594-3 within the geologic units concerned. Most of the available pressure data come from drill stem tests (DSTs), which have been routinely run by the industry for the past thirty years or so, and from repeat formation testing (RFT) tools, which have only recently begun to be commonly used in petroleum e
作者: Obvious    時間: 2025-3-26 13:48

作者: miracle    時間: 2025-3-26 18:02
https://doi.org/10.1007/978-1-4842-8628-9sed 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
作者: 免除責(zé)任    時間: 2025-3-26 22:39
https://doi.org/10.1007/978-1-4842-8628-9nment 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
作者: Habituate    時間: 2025-3-27 05:02

作者: Trigger-Point    時間: 2025-3-27 06:20

作者: 鼓掌    時間: 2025-3-27 10:39

作者: Fracture    時間: 2025-3-27 13:45

作者: 空洞    時間: 2025-3-27 20:15
https://doi.org/10.1007/978-981-15-2121-8erence elevations at which levels of potential energy for oil or gas can be easily calculated, and the points at which the Z traces intersect the top of the unit correspond to structure contours. The “contour interval” is ΔZ. Since the system is hydrostatic, the buoyancy vector and the gravity vecto
作者: Factual    時間: 2025-3-27 22:26

作者: SCORE    時間: 2025-3-28 03:14

作者: Campaign    時間: 2025-3-28 06:27
https://doi.org/10.1007/978-1-4612-4258-1Engineering Geology; Erd?llagerst?tte; Hydrogeologie; Hydrogeology; petroleum geology
作者: Kernel    時間: 2025-3-28 14:25

作者: 彎曲的人    時間: 2025-3-28 15:19
Formation Pressure Measurements and Data, within the geologic units concerned. Most of the available pressure data come from drill stem tests (DSTs), which have been routinely run by the industry for the past thirty years or so, and from repeat formation testing (RFT) tools, which have only recently begun to be commonly used in petroleum exploration.
作者: BRIEF    時間: 2025-3-28 22:14

作者: 網(wǎng)絡(luò)添麻煩    時間: 2025-3-29 01:38
http://image.papertrans.cn/a/image/159856.jpg
作者: 從屬    時間: 2025-3-29 03:13

作者: eardrum    時間: 2025-3-29 08:18
Computer Operating System Securitych the rate of pressure increase is the greatest) is vertical, attributable to gravitational weight of the overlying fluids, as discussed earlier. All internal forces are oriented vertically, buoyancy being the major one. (Anyone who has swum to the bottom of a deep swimming pool has felt the effects of this gradient in the form of “squeeze.”)
作者: Gleason-score    時間: 2025-3-29 13:32
Book 1995Latest editioneologists 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
作者: 路標(biāo)    時間: 2025-3-29 17:05

作者: 絕緣    時間: 2025-3-29 20:45
The Weakest Security Link—Peoplets that are “over- pressured” for the locality. On the other hand, pressures B, H, and G fall to the lower left of the standard normal gradient and are low for their depth, so the units concerned would be classed as “underpressured.” These terms are relative and only locally meaningful.




歡迎光臨 派博傳思國際中心 (http://www.pjsxioz.cn/) Powered by Discuz! X3.5
内江市| 清远市| 锦屏县| 黔南| 平谷区| 岳西县| 孝感市| 鄂托克前旗| 元朗区| 沁阳市| 紫云| 孝义市| 青州市| 崇左市| 迭部县| 房山区| 巴楚县| 大洼县| 建宁县| 宜丰县| 上蔡县| 息烽县| 景东| 宜兰市| 通江县| 荔波县| 边坝县| 聂荣县| 诸城市| 澎湖县| 绵阳市| 普宁市| 襄城县| 泽州县| 萨嘎县| 闸北区| 威信县| 平舆县| 仲巴县| 克东县| 崇州市|