Menke H P, Maes J, Geiger S
Institute for GeoEnergy Engineering, Heriot-Watt University, Edinburgh, UK.
Sci Rep. 2021 Jan 29;11(1):2625. doi: 10.1038/s41598-021-82029-2.
The permeability of a pore structure is typically described by stochastic representations of its geometrical attributes (e.g. pore-size distribution, porosity, coordination number). Database-driven numerical solvers for large model domains can only accurately predict large-scale flow behavior when they incorporate upscaled descriptions of that structure. The upscaling is particularly challenging for rocks with multimodal porosity structures such as carbonates, where several different type of structures (e.g. micro-porosity, cavities, fractures) are interacting. It is the connectivity both within and between these fundamentally different structures that ultimately controls the porosity-permeability relationship at the larger length scales. Recent advances in machine learning techniques combined with both numerical modelling and informed structural analysis have allowed us to probe the relationship between structure and permeability much more deeply. We have used this integrated approach to tackle the challenge of upscaling multimodal and multiscale porous media. We present a novel method for upscaling multimodal porosity-permeability relationships using machine learning based multivariate structural regression. A micro-CT image of Estaillades limestone was divided into small 60 and 120 sub-volumes and permeability was computed using the Darcy-Brinkman-Stokes (DBS) model. The microporosity-porosity-permeability relationship from Menke et al. (Earth Arxiv, https://doi.org/10.31223/osf.io/ubg6p , 2019) was used to assign permeability values to the cells containing microporosity. Structural attributes (porosity, phase connectivity, volume fraction, etc.) of each sub-volume were extracted using image analysis tools and then regressed against the solved DBS permeability using an Extra-Trees regression model to derive an upscaled porosity-permeability relationship. Ten test cases of 360 voxels were then modeled using Darcy-scale flow with this machine learning predicted upscaled porosity-permeability relationship and benchmarked against full DBS simulations, a numerically upscaled Darcy flow model, and a Kozeny-Carman model. All numerical simulations were performed using GeoChemFoam, our in-house open source pore-scale simulator based on OpenFOAM. We found good agreement between the full DBS simulations and both the numerical and machine learning upscaled models, with the machine learning model being 80 times less computationally expensive. The Kozeny-Carman model was a poor predictor of upscaled permeability in all cases.
孔隙结构的渗透率通常由其几何属性的随机表示来描述(例如孔径分布、孔隙率、配位数)。对于大型模型域,基于数据库的数值求解器只有在纳入该结构的粗粒化描述时,才能准确预测大规模流动行为。对于具有多模态孔隙结构的岩石(如碳酸盐岩),粗粒化尤其具有挑战性,因为其中几种不同类型的结构(例如微孔、孔洞、裂缝)相互作用。正是这些根本不同结构内部以及它们之间的连通性最终控制了较大长度尺度下的孔隙率 - 渗透率关系。机器学习技术与数值建模和有根据的结构分析相结合的最新进展,使我们能够更深入地探究结构与渗透率之间的关系。我们使用这种综合方法来应对多模态和多尺度多孔介质粗粒化的挑战。我们提出了一种使用基于机器学习的多元结构回归来粗粒化多模态孔隙率 - 渗透率关系的新方法。将埃斯塔亚德石灰岩的微观计算机断层扫描(micro-CT)图像划分为60和120个小的子体积,并使用达西 - 布林克曼 - 斯托克斯(DBS)模型计算渗透率。利用门克等人(《地球预印本》,https://doi.org/10.31223/osf.io/ubg6p ,2019年)提出的微孔率 - 孔隙率 - 渗透率关系,为包含微孔的单元格分配渗透率值。使用图像分析工具提取每个子体积的结构属性(孔隙率、相连通性、体积分数等),然后使用极端随机树回归模型将其与求解得到的DBS渗透率进行回归,以得出粗粒化的孔隙率 - 渗透率关系。然后,使用这种机器学习预测的粗粒化孔隙率 - 渗透率关系,对360体素的10个测试案例进行达西尺度流动建模,并与完整的DBS模拟、数值粗粒化的达西流动模型和科曾尼 - 卡曼模型进行基准比较。所有数值模拟均使用GeoChemFoam进行,这是我们基于OpenFOAM开发的内部开源孔隙尺度模拟器。我们发现完整的DBS模拟与数值和机器学习粗粒化模型之间具有良好的一致性,其中机器学习模型的计算成本低80倍。在所有情况下,科曾尼 - 卡曼模型对粗粒化渗透率的预测都很差。