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Method for 4D water permeability analysis of geological features fluid storage

机译:地质特征储液4D透水率分析方法

摘要

(57) Abstract This invention the filter does the micro-earthquake activity which is induced while producing the fluid resource from storage, classifies, it is something in order to analyze, makes the direct 4 dimensional measurement of important other oil stratum stones and rocks physical quality possible for everything or the many component of water permeability field, and the analysis and monitoring of storage. The seismic activity which it is related to water permeability field is arranged symmetrically the fill point inside the optional well which is used because of this object (Figure 1) to in regard, it is identified two general circular internal that space and depending upon time position. The conical axis is parallel vis-a-vis the largest compressed stress direction of initial load field. When it increases, seismic activity the fill point (Figure 2) from moves fluid pressure to facing outside rapidly. Seismic activity moves in markedly bigger portable ratio, than portable ratio of the flow of diffusivity of darcy type covers the distance which is measured at the unit of kilometer. Seismic activity occurs by the fracture which aeromechanics is connected vis-a-vis the fill well, includes the water permeability field which it is related to that well. You can use the map of the water permeability field which is identified by this expedient, even in order to guide filling up, developing of succession and arranging the fill well. Furthermore, this invention makes that the latent hazard for field inhurasutorakuchiya by making the observation of be active deformation field possible, is recognized possible. In addition, this invention forms the important expedient of 4D be active earthquake analysis of the place where movement of the fluid is monitored by estimating fluid route.
机译:(57)<摘要>本发明的过滤器具有从储存中产生流体资源时引起的微地震活动,进行分类,以进行分析,对其他重要的油层石进行直接的4维测量和岩石的物理质量可能适用于渗水领域的所有事物或许多组成部分,以及对存储的分析和监控。与透水率场有关的地震活动被对称地布置在可选井内的填充点上,由于该对象(图1)而使用该可选井,因此确定了两个大致的圆形内部空间和时间位置。圆锥轴相对于初始载荷场的最大压缩应力方向平行。当它增加时,地震活动的填充点(图2)从将流体压力迅速移动到面向外部。地震活动以显着更大的可移动比率移动,比达西式扩散流的可移动比率覆盖以千米为单位测量的距离。地震活动是由与填充井相对应的航空力学连接的裂缝引起的,包括与该井有关的渗透率场。您可以使用此方法确定的透水率场图,甚至可以指导填充,演替发展和布置填充井。进而,本发明通过观察主动变形场,从而能够认识到对田间潜伏的潜在危害。另外,本发明形成了4D的重要权宜之计,即通过估计流体路径来监测流体运动的地方的主动地震分析。

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