首页> 外文会议>International Symposium of the Society of Core Analysts >PREDICTING PERMEABILITY THROUGH 3D PORE-SPACE IMAGES RECONSTRUCTED USING MULTIPLE-POINT STATISTICS
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PREDICTING PERMEABILITY THROUGH 3D PORE-SPACE IMAGES RECONSTRUCTED USING MULTIPLE-POINT STATISTICS

机译:通过使用多点统计重建的3D孔隙空间图像预测渗透性

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Pore-scale network modeling can predict multiphase flow properties with arbitrary wetting conditions if the network represents the geology of the sample accurately.Such pore-scale modeling uses topologically disordered networks that realistically represent the pore structure.To generate the network it is first necessary to have a three-dimensional voxel-based pore-space representation that is constructed by either a direct imaging technique such as micro-CT scanning,stochastic methods,or object-based approaches.Micro-CT scanning is the most promising among these three approaches since it is the most direct.However,its resolution – a few microns – means that for many rocks,particularly carbonates,significant porosity cannot be imaged.Furthermore,alternative approaches,such as reconstruction through simulating the geological processes by which the rock was formed,such as sedimentation and diagenesis,may be problematic for many materials whose depositional and diagenetic history is uncertain or complex.Statistical reconstruction is more general and is not limited by the pore size.Statistics of the pore space are obtained from readily available experimental data such as thin-section images.Using only single and two-point statistics in the reconstruction often underestimates the pore connectivity,especially for low porosity materials.We use multiple-point statistics for pore space reconstruction that preserves higher-order information,describing the statistical relation between multiple spatial locations.This is a general method that gives images that preserve typical patterns of the void space seen in thin sections.The method is tested on a carbonate sample from the Middle East.Permeability is predicted directly on the 3D images using the lattice Boltzmann method.The numerically estimated results are in good agreement with experimentally measured permeability.Furthermore,this method provides an important input for the creation of geologically realistic networks for pore-scale modeling to predict multiphase flow properties.
机译:孔隙尺度网络建模可以预测多相流动性能,如果网络代表样品的地质准确,则可以预测多相润湿条件。uch孔径建模使用拓扑无序网络,现实地代表孔结构。要生成网络,首先是必要的具有三维体素的孔隙空间表示,通过直接成像技术,例如微型成像技术,例如微型CT扫描,随机方法或基于对象的方法.Micro-CT扫描是这三种方法中最有希望的它是最直接的。然而,它的分辨率 - 几微米 - 意味着对于许多岩石,特别是碳酸盐,不能成像。诸如通过模拟岩石形成的地质过程来重建的诸如重建的显着的孔隙率。如沉淀和成岩作用,对于许多沉积和成岩病史是不合适的许多材料可能是有问题的AIN或Complex.statistical重建更一般,并且不受孔径的限制。孔隙空间的术语是从易于获得的实验数据获得的,例如薄截面图像。仅重建中的单点和两点统计数据通常低估孔隙连接,特别是对于低孔隙率材料。我们使用孔隙空间重建的多点统计数据,以保留更高阶信息,描述多个空间位置之间的统计关系。这是一种常规方法,它给出了保持典型模式的图像在薄切片中看到的空隙。方法在中东的碳酸盐样品上测试。使用格子Boltzmann方法直接在3D图像上预测可熔化。数值估计的结果与实验测量的渗透率良好。繁殖,这方法为创建孔隙的地质现实网络提供了重要的意见-Scale建模以预测多相流动性质。

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