首页> 外文会议>SPE annual technical conference and exhibition;SPE 2002 >Quantification of Multi-Phase Fluid Saturations in Complex Pore Geometries From Simulations of Nuclear Magnetic Resonance Measurements
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Quantification of Multi-Phase Fluid Saturations in Complex Pore Geometries From Simulations of Nuclear Magnetic Resonance Measurements

机译:通过核磁共振测量的模拟量化复杂孔隙几何形状中的多相流体饱和度

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We develop a numerical algorithm to simulate nuclearrnmagnetic resonance (NMR) measurements in the presence ofrnconstant magnetic field gradients. The algorithm is based onrnMonte Carlo conditional random walks in restricted andrnunrestricted space. Simulations can be performed of threedimensionalrn(3D) porous media that include both arbitraryrnbimodal pore distributions and multi-phase fluid saturations.rnThe ability to account for the presence of a constant externalrnmagnetic field gradient allows us to replicate actual wellrnlogging conditions that include the effect of CMPG pulsernsequences at a microscopic level. This is accomplished byrnsimulating pulse acquisition techniques that include multiplerninter-echo times (TE) similar to those currently used by thernwell-logging industry. Benchmark examples are presented tornvalidate the accuracy and internal consistency of our algorithmrnagainst previously published results for the case of a nullrnmagnetic field gradient. Validation examples are alsornpresented against actual NMR measurements performed onrncore samples of carbonate rock formations.rnInterpretation work is focused to the petrophysicalrnassessment of both partial oil/water saturations and porernstructures exhibiting hydraulic coupling. Simulation examplesrnare designed to quantify whether the inclusion of diffusionrnunder a magnetic field gradient can improve the interpretationrnof multi-phase fluid saturations when hydraulic coupling isrnsignificant. The simulation algorithm sheds light to new NMRrndata acquisition strategies that could be used to improve therndetection and quantification of (a) fluid types, (b) complexrnfluid saturations, and (c) complex pore geometries.
机译:我们开发了一种数值算法来模拟存在恒定磁场梯度的核磁共振(NMR)测量。该算法基于有限空间和无限制空间中的蒙特卡洛条件随机游动。可以对包括任意双峰孔隙分布和多相流体饱和度的三维(3D)多孔介质进行模拟。考虑到恒定外部磁场梯度的存在的能力使我们能够复制包括CMPG效应的实际测井条件在微观水平上的脉冲序列。这是通过模拟脉冲采集技术来实现的,该技术包括类似于回波测井行业目前使用的多次回波时间(TE)。提出了基准示例,以验证我们的算法在先前磁场磁场梯度情况下的准确性和内部一致性。还给出了对碳酸盐岩岩心样品上进行的实际NMR测量的验证实例。解释工作的重点是对部分油/水饱和度和表现出水力耦合作用的孔隙结构的岩石物理评价。设计了一些仿真示例,以量化当液力耦合不明显时,在磁场梯度下包含扩散是否可以改善多相流体饱和度的解释。该模拟算法为新的NMRrndata采集策略提供了启示,该策略可用于改进对(a)流体类型,(b)复流体饱和度和(c)复孔几何形状的检测和定量。

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