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Fremgangsmåte for modelldannelse av et lagdelt og frakturert geologisk miljö
Fremgangsmåte for modelldannelse av et lagdelt og frakturert geologisk miljö
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机译:分层和破裂地质环境模型形成的程序
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摘要
- the method comprises a modeling of the medium by the plies (s (i)) having an orientation substantially common representing the actual stack of layers, and a representation of the fractures in the form of portions of surface, such as a deformable quadrilateral, each passing through at least one of the strata, each portion of the surface being positioned and its extension, delimited by the draw while respecting the densities of fracturing n (i) per unit length of each layer, as well as the proportions (s (i / i + 1), s (i / i - 1)) of fractures through the interfaces between the layers, these densities and proportions are determined by studying the medium (observations direct, photographs, etc..). The model obtained makes it possible to flow simulations fluids likely to move through the medium. & br / - application to the study of the displacements of hydrocarbons in the underground reservoirs, for example.
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机译:-该方法包括通过层(s(i))对介质建模,所述层具有基本上共同的取向,其代表实际的层堆叠,并且以表面的一部分形式的裂缝(例如可变形的四边形)来表征裂缝,每一层都穿过至少一个地层,表面的每个部分及其延伸位置都由拉伸确定,同时考虑到每一层每单位长度的破裂密度n(i)以及比例(s( i / i + 1),s(i / i-1)穿过层间界面的裂缝,这些密度和比例是通过研究介质(直接观测,照片等)确定的。所获得的模型可以对可能通过介质流动的流体进行流动模拟。 & br />-例如,用于研究地下储层中碳氢化合物的驱替作用。
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