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Method for forming a model of a formation geological, which is stressed by the dynamic and static

机译:动态和静态应力作用下的地层地质模型的形成方法

摘要

A structure is chosen a priori, with one physical dimension (k) estimated from the exploration data and a second ( sigma ) estimated from the fluid production data. The model is optimized by iterative application of an inversion of at least one of the physical dimensions, which are related by a combination function. The final model at least satisfies the combination of the two dimensions. The iterative optimization involves a simultaneous iteration of the first and second physical dimensions with optimization of a global cost function J(K, sigma ) of the two dimensions. The global cost function is the sum of terms measuring the spacing between the points of each model and the data obtained by measurement or observation or the corresponding dimension and the spacing taking into account the combination of the two dimensions. Each model is optimized by minimizing the objective function by determining its exact gradient using the adjoining state method. The production data are measured in the shaft through the underground area and the exploration data are the seismic data captured by seismic receivers in response to waves transmitted through the formation. The first physical dimension is the permeability of the medium and the second is the impedance of the medium relative to the waves.
机译:先验地选择一种结构,其中一个物理尺寸(k)从勘探数据中估算,第二个物理尺寸(sigma)从流体产量数据中估算。通过迭代应用至少一个物理维度的倒数来优化模型,该倒数与组合函数有关。最终模型至少满足两个维度的组合。迭代优化涉及第一物理维度和第二物理维度的同时迭代,同时优化二维的全局成本函数J(K,sigma)。全局成本函数是测量每个模型的点之间的距离与通过测量或观察获得的数据或相应尺寸以及考虑到两个尺寸的组合的间距的项的总和。通过使用邻接状态方法确定目标函数的精确梯度来最小化目标函数,从而优化了每个模型。在穿过地下区域的竖井中测量生产数据,而勘探数据是地震接收器响应于穿过地层传输的波而捕获的地震数据。第一个物理尺寸是介质的渗透率,第二个是介质相对于波的阻抗。

著录项

  • 公开/公告号NO20004352L

    专利类型

  • 公开/公告日2001-03-05

    原文格式PDF

  • 申请/专利权人 INSTITUT FRANCAIS DU PETROLE;

    申请/专利号NO20000004352

  • 发明设计人 GUERILLOT DOMINIQUE;PIANELO LAURENT;

    申请日2000-09-01

  • 分类号G01V1/00;G01V1/34;

  • 国家 NO

  • 入库时间 2022-08-22 01:24:40

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