首页> 外国专利> METHOD FOR SIMPLIFYING THE MODELING OF A POROUS GEOLOGICAL ENVIRONMENT CROSSED BY AN IRREGULAR FRACTURE NETWORK

METHOD FOR SIMPLIFYING THE MODELING OF A POROUS GEOLOGICAL ENVIRONMENT CROSSED BY AN IRREGULAR FRACTURE NETWORK

机译:不规则断裂网络交叉的多孔地质环境建模的简化方法

摘要

P Method allows a simplified modeling of a porous heterogeneous geological medium (such as a reservoir crossed by an irregular network of cracks for example) in the form of a transposed medium or equivalent so that the transposed medium is equivalent to the original medium, relative to a specific type of physical transfer function (known for the transposed medium). It comprises: BR/ a) the formation of an image in at least two dimensions of the original geological medium in the form of a series of pixels and the association with each pixel of the series of an initial value particular for this function, BR/ b) the stepwise determination of values to be assigned for the physical transfer function to each pixel of the series (such as the minimum distance separating the pixel from the nearest crack) with reference to values of the function assigned to pixels adjacent to the image, and BR/ c) determining a physical property of the transposed medium or equivalent by identifying the values of the transfer function known for the medium transposed with the Origin medium transfer function values determined in stages. The physical transfer function may represent variations between different parts of the geological medium, for example distances or transmissivities or heat transfers (between a reservoir and a well passing through the reservoir for example), etc. BR/ Application to the determination of a transposed medium providing the same fluid recovery during a capillary imbibing process as the actual medium. / P
机译:

方法允许以转置介质或等效介质的形式简化多孔非均质地质介质(例如,由不规则裂缝网络交叉的储层)的建模,以便转置介质等效于原始介质,相对于特定类型的物理传递函数(对于转置介质而言是已知的)。它包括:
a)在原始地质介质的至少二维区域中以一系列像素的形式形成图像,并与一系列像素中的每个像素相关联以实现该功能,
b)参照分配给相邻像素的函数值,逐步确定要分配给系列中每个像素的物理传递函数的值(例如,将像素与最近的裂缝分开的最小距离) c)通过识别已知的传递函数值来确定转置介质或等效介质的物理特性,该传递函数的值已分阶段确定了原始介质传递函数值。物理传递函数可以表示地质介质不同部分之间的变化,例如距离或透射率或热传递(例如在储层和穿过储层的井之间)等。
在毛细管吸收过程中,转置的介质提供与实际介质相同的流体回收率。

著录项

  • 公开/公告号FR2757957A1

    专利类型

  • 公开/公告日1998-07-03

    原文格式PDF

  • 申请/专利权人 INSTITUT FRANCAIS DU PETROLE;

    申请/专利号FR19960016331

  • 发明设计人 SYLVAIN SARDA;BERNARD BOURBIAUX;

    申请日1996-12-30

  • 分类号G01V9/00;G01V11/00;E21B49/00;E21B47/10;

  • 国家 FR

  • 入库时间 2022-08-22 02:41:48

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