A multi-scale scheme for the invasion percolation of rock fracture networks with heterogeneous fracture aperture fields is proposed. Inside fractures, fluid transport is calculated on the finest scale and found to be localized in channels as a consequence of the aperture field. The channel network is characterized and reduced to a vectorized artificial channel network (ACN). Different realizations of ACNs are used to systematically calculate efficient apertures for fluid transport inside differently sized fractures as well as fracture intersection and entry properties. Typical situations in fracture networks are parameterized by fracture inclination, flow path length along the fracture and intersection lengths in the entrance and outlet zones of fractures. Using these scaling relations obtained from the finer scales, we simulate the invasion process of immiscible fluids into saturated discrete fracture networks, which were studied in previous works.
翻译:提出了将岩石断裂网络与各种碎裂孔径田进行入侵穿透的多尺度计划; 内部断裂、流体迁移是最佳规模的计算,并发现由于孔径田的缘故,在渠道中是局部的; 频道网络具有特性,并缩小为传导人工信道网络(ACN); 使用不同功率的ACN系统计算不同尺寸骨裂以及断裂交叉和进入特性内流体迁移的高效孔径; 骨裂网络的典型情况以断裂倾角、断裂道长度和断裂口和外缘的交叉长度为参数; 利用从细度中取得的这些缩放关系,我们模拟非强迫性液体进入饱和离散断裂网络的入侵过程,以前曾对这一过程进行过研究。