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A Robust Method for Calculating Formation Mobility With a Formation Tester

机译:用地层测试仪计算地层流动性的稳健方法

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Determining formation mobility (permeability/viscosity) with a formation tester dates back to the introduction of the tool in the mid-1950s. Many methods have been developed over the years to calculate a formation mobility from a pressure test. Here, a rigorous method is presented that has several convenient features. It is based on a model that assumes the presence of both tool-storage and formation compressibility and so is appropriate for a fully unsteady flow induced in the formation, but it does not require the determination of either compressibility to determine the mobility. The full impact of the wellbore geometry is included (i.e., it does not assume the "spherical-flow model"). The mobility is determined by a simple, direct calculation of the measured time-dependent pressure, as opposed to methods based upon data regression or solving an inverse problem. On the other hand, this new method shares several of the restrictions common to existing techniques: It assumes that the formation contains a single phase of slightly compressible fluid. The calculated mobility characterizes the formation in the vicinity of the wellbore wall, in which formation damage is most likely to occur. This publication is dedicated to Gerard Catala, a colleague with tremendous insight.
机译:用地层测试仪确定地层的流动性(渗透率/粘度)可以追溯到1950年代中期。多年来,已经开发出许多方法来通过压力测试来计算地层迁移率。在这里,提出了一种严格的方法,它具有几个方便的功能。它基于一个模型,该模型假定同时存在工具存储和地层可压缩性,因此适用于在地层中引起的完全不稳定流动,但是它不需要确定任何可压缩性即可确定流动性。包括了井眼几何形状的全部影响(即,它不采用“球形流模型”)。与基于数据回归或解决反问题的方法相反,通过简单,直接计算所测时间相关压力来确定迁移率。另一方面,这种新方法也有一些现有技术共有的限制条件:假定地层包含一个单相的可压缩流体。计算出的迁移率是井壁附近地层的特征,其中最有可能发生地层损坏。该出版物专门献给具有深刻见解的同事Gerard Catala。

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