首页> 外文会议>SPE annual technical conference and exhibition;ATCE 2005 >Efficient and Accurate Estimation of Permeability and Permeability Anisotropy FromStraddle-Packer Formation Tester Measurements Using the Physics of Two-PhaseImmiscible Flow and Invasion
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Efficient and Accurate Estimation of Permeability and Permeability Anisotropy FromStraddle-Packer Formation Tester Measurements Using the Physics of Two-PhaseImmiscible Flow and Invasion

机译:使用两相不混溶流动和侵入物理,从跨包式地层测试仪测量中高效,准确地估算渗透率和渗透率各向异性

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This paper describes the successful application of a novelmethodology to estimate permeability and permeabilityanisotropy from transient measurements of pressure acquiredwith a wireline straddle-packer formation tester. Unlikestandard algorithms used for the interpretation of formationtester measurements, the methodology developed in this paperrigorously incorporates the physics of two-phase immiscibleflow as well as the process of mudcake buildup and invasion.The effects of supercharge, skin, and convective transport ofsalt are also explicitly included in the estimation algorithm.An efficient 2D (cylindrical coordinates) implicit-pressureexplicit-saturation finite-difference algorithm is used tosimulate both the process of invasion and the pressuremeasurements acquired with the straddle-packer formationtester. Initial conditions for the simulation of formation testermeasurements are determined by the spatial distributions ofpressure and fluid saturation resulting from mud-filtrateinvasion. Inversion is performed with a rigorous Levenberg-Marquardtnonlinear minimization algorithm. Sensitivityanalyses are conducted to assess non-uniqueness and theimpact of assumptions on rock-fluid and mud properties suchas fluid viscosity, capillary pressure, relative permeability,mudcake growth, and time of invasion.Applications of the estimation algorithm to noisy syntheticmeasurements include homogeneous, anisotropic, layered, andmulti-layered formations, for both low- and high-porosityrocks. We also study the effect of unaccounted impermeablebed boundaries on the inversion results. For cases where a-prioriinformation can be sufficiently constrained, ourinversion methodology provides reliable and accurateestimates of permeability and permeability anisotropy.
机译:本文介绍了一种新颖的方法的成功应用,该方法可通过电缆跨装式地层测试仪获得的瞬态压力测量值来估算渗透率和渗透率各向异性。与解释地层测试仪测量所使用的标准算法不同,本文开发的方法严格结合了两相不混溶流动的物理原理以及泥饼的形成和侵入过程,还明确包括了增压,表皮和盐的对流输运的影响高效的二维(圆柱坐标)隐式压力显式饱和度有限差分算法用于模拟侵入过程和跨式封隔器地层测试仪获得的压力测量结果。地层测试仪模拟的初始条件是由泥浆渗透引起的压力和流体饱和度的空间分布确定的。用严格的Levenberg-Marquardt非线性最小化算法进行反演。进行敏感性分析以评估非唯一性以及假设对岩石流体和泥浆特性的影响,例如流体粘度,毛细压力,相对渗透率,泥饼生长和侵入时间。估算算法在嘈杂的综合测量中的应用包括均质,各向异性,低孔隙率岩层和高孔隙率岩层的分层和多层地层。我们还研究了无法解释的不可渗透边界对反演结果的影响。对于可以充分约束先验信息的情况,我们的反演方法可提供可靠而准确的磁导率和磁导率各向异性估计。

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