Pore-scale simulations help in overcoming laboratory limitations with unconsolidated rock material: A multi-step reconstruction based on scanning electron and optical microscopy data

IF 4 2区 环境科学与生态学 Q1 WATER RESOURCES
Dmitry A. Kulygin , Aleksey Khlyupin , Aleksei Cherkasov , Rustem A. Sirazov , Dina Gafurova , Yan I. Gilmanov , Konstantin V. Toropov , Dmitry V. Korost , Kirill M. Gerke
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Abstract

This article explores the possibility to assess the flow and transport properties of loosely consolidated rock material—something that is very hard or impossible to achieve in the laboratory due to fragility of cores. We present two cases of weakly consolidated and unconsolidated rocks. We provide a solution based on pore-scale simulations and stochastic reconstructions using scanning electron (SEM) and grain optical microscopy images as input data. The hybrid reconstruction approach is based on 3D grain shape construction out of 2D optical images, packing of grains to match the target porosity measured from SEM imaging, and addition of clay and other cementing phases with the help of phase-recovery method. Note that standard digital rock protocol based on X-ray microtomography did not work for considered samples due to fine-grained particle size distribution (insufficient resolution of X-ray microtomography). After creation of 3D digital replicas of rock samples based on their SEM and optical microscopy images, we applied pore-scale modeling to obtain permeability and two-phase flow properties. Simulated permeability of 259 mD for the first sample was in surprisingly good agreement with laboratory measurements of 248 mD. For the second sample permeabilities deviated by an order of magnitude. After additional studies it was found that the mesh attached to the sample during measurements affected the results. After pore-scale simulations of the grain packing with the mesh we were able to achieve very good agreement with the experiment, confirming that the lab was basically exploring the properties of the mesh clogged with unconsolidated rock material. Thus, pore-scale hybrid rock structure reconstruction technique combined with pore-scale simulations was able to correct inaccurate laboratory assessment and obtain flow properties for unconsolidated rock sample. We believe the developed hybrid reconstruction technique to be robust enough to serve as a basis of the industrial technology for petrophysical studies of weakly and unconsolidated core material.

孔隙尺度模拟有助于克服实验室对未固结岩石材料的限制:基于扫描电子显微镜和光学显微镜数据的多步骤重构
本文探讨了评估松散固结岩材料的流动和传输特性的可能性--由于岩芯的脆弱性,这在实验室中很难或不可能实现。我们介绍了弱固结和未固结岩石的两种情况。我们利用扫描电子显微镜(SEM)和晶粒光学显微镜图像作为输入数据,提供了一种基于孔隙尺度模拟和随机重建的解决方案。混合重建方法基于二维光学图像的三维晶粒形状构建、晶粒堆积以匹配扫描电子显微镜成像测得的目标孔隙度,以及在相恢复方法的帮助下添加粘土和其他胶结相。需要注意的是,基于 X 射线显微层析成像技术的标准数字岩石方案并不适用于所考虑的样品,因为这些样品的粒度分布较细(X 射线显微层析成像技术的分辨率不足)。在根据扫描电镜和光学显微镜图像创建了岩石样本的三维数字复制品后,我们应用孔隙尺度建模来获取渗透率和两相流动特性。第一个样本的模拟渗透率为 259 mD,与实验室测量值 248 mD 惊人地吻合。第二个样本的渗透率则偏差了一个数量级。经过进一步研究发现,测量过程中附着在样品上的网格影响了测量结果。在对网眼的晶粒堆积进行孔隙尺度模拟后,我们的结果与实验结果非常吻合,证实实验室基本上是在探索被未固结岩石材料堵塞的网眼的特性。因此,孔隙尺度混合岩石结构重建技术与孔隙尺度模拟相结合,能够纠正不准确的实验室评估,并获得未固结岩石样本的流动特性。我们相信所开发的混合重建技术足够强大,可以作为弱和未固结岩芯材料岩石物理研究的工业技术基础。
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来源期刊
Advances in Water Resources
Advances in Water Resources 环境科学-水资源
CiteScore
9.40
自引率
6.40%
发文量
171
审稿时长
36 days
期刊介绍: Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources. Examples of appropriate topical areas that will be considered include the following: • Surface and subsurface hydrology • Hydrometeorology • Environmental fluid dynamics • Ecohydrology and ecohydrodynamics • Multiphase transport phenomena in porous media • Fluid flow and species transport and reaction processes
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