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Permeability Upscaling for Carbonates from the Pore-Scale UsingMulti-Scale Xray-CT Images

机译:渗透性Umporti-Scale X射线X射线CT图像从孔径升高的碳酸盐

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High-resolution Xray-CT images are increasingly used to numerically derive petrophysical properties of interest at the porescale, in particular effective permeability. Current micro Xray-CT facilities typically offer a resolution of a few microns pervoxel resulting in a field of view of about 5 mm3 for a 20482 CCD. At this scale the resolution is normally sufficient to resolvepore space connectivity and transport properties. For samples exhibiting heterogeneity above the field of view of such a singlehigh resolution tomogram with resolved pore space, a second low resolution tomogram can provide a larger scale porositymap. The problem then reduces to rock-typing the low resolution Xray-CT image, deriving viable porosity-permeability trans-forms from the high resolution Xray-CT image(s) for all rock types present, and upscaling of the permeability field to derive aplug-scale permeability. In this study we characterize spatially heterogeneity using overlapping registered Xray-CT images derived at different resolu-tions spanning orders of magnitude in length scales. A 38mm diameter carbonate core is studied in detail and imaged at lowresolution - and at high resolution by taking four 5mm diameter subsets, one of which is imaged using full length helical scan-ning. Fine-scale permeability transforms are derived using direct porosity-permeability relationships, random sampling of theporosity-permeability scatter-plot as function of porosity, and structural correlations combined with stochastic simulation. Arange of these methods are applied at the coarse scale. We compare various upscaling methods including renormalization theo-ry with direct solutions using a Laplace solver and report error bounds.We find that for the heterogeneous samples permeability typically increases with scale. Conventional methods using basicaveraging techniques fail to provide truthful vertical permeability due to large permeability contrasts. The most accurate up-scaling technique is employing Darcy’s law. A key part of the study is the establishment of porosity transforms between high-resolution and low-resolution images to arrive at a calibrated porosity map to constraint permeability estimates for the wholecore.
机译:高分辨率X射线CT图像越来越多地用于在Porescale,特别是有效的渗透率下进行数值衍生利息的岩石物理特性。目前的微X射线CT设施通常提供几微米Pervoxel的分辨率,导致20482 CCD的视场约为5mm3。在此规模,分辨率通常足以解决RESITVEPORE SPACE CONCHECTIVE和传输属性。对于在具有分辨孔隙空间的这种单个高分辨率断层照片上方的视野上方的样品,第二个低分辨率断层照片可以提供更大的尺度孔隙图。然后,问题减少了摇弦键入低分辨率X射线CT图像,从存在的所有岩石类型的高分辨率X射线CT图像中导出可行的孔隙率透晶作物,并升高渗透性场以导出aplug - 渗透率。在该研究中,我们使用重叠登记的X射线CT图像在空间异质性在长度尺度的不同分辨率的不同分辨率下衍生的重叠X射线图像中的图像。通过采用四个5mm直径的子集进行38mm直径的碳酸核,并在低分辨率下成像,并以高分辨率在高分辨率下进行,其中一个是使用全长螺旋扫描宁成像。使用直接孔隙率渗透性关系来推导微垢渗透性变换,作为孔隙率的函数的本经孔隙渗透性散射图的随机取样,以及与随机模拟结合的结构相关性。这些方法的惊格以粗略施加。我们比较各种Uppaling方法,包括使用Laplace求解器的直接解决方案的重新运行方法,并使用Laplace求解器和报告错误绑定。我们发现对于异质样本的渗透率通常随着比例而增加。由于较大的渗透率对比,使用碱吸引技术的常规方法未能提供真实的垂直渗透率。最准确的上缩放技术正在采用达西法律。该研究的一个关键部分是建立高分辨率和低分辨率图像之间的孔隙率变换,以将校准的孔隙率图到达到全部的约束渗透率估计。

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