Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8883364 | Advances in Water Resources | 2018 | 41 Pages |
Abstract
Dynamic capillary pressure (DCP) effects, which is vital for predicting multiphase flow behavior in porous media, refers to the injection rate dependence capillary pressure observed during non-equilibrium displacement experiments. However, a clear picture of the effects of microscale fractures on DCP remains elusive. This study quantified the effects of microscale fractures on DCP and simulated pore-scale force and saturation change in fractured porous media using the multiphase lattice Boltzmann method (LBM). Eighteen simulation cases were carried out to calculate DCP as a function of wetting phase saturation. The effects of viscosity ratio and fracture orientation, aperture and length on DCP and DCP coefficient Ï were investigated, where Ï refers to the ratio of the difference of DCP and static capillary pressure (SCP) over the rate of wetting-phase saturation change versus time. Significant differences in Ï values were observed between unfractured and fractured porous media. The Ï values of fractured porous media were 1.1â
â¯Ãâ¯104â
Paâ
ms to 5.68 â¯Ãâ¯105â
Paâ
ms, which were one or two orders of magnitude lower than those of unfractured porous media with a value of 4 â¯Ãâ¯106â
Pa.â
ms. A horizontal fracture had greater effects on DCP and Ï than a vertical fracture, given the same fracture aperture and length. This study suggested that a microscale fracture might result in large magnitude changes in DCP for two-phase flow.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Mingming Tang, Shuangfang Lu, Hongbin Zhan, Guo Wenqjie, Huifang Ma,