多孔介质
机械
颗粒沉积
流体力学
雷诺数
磁导率
压力降
材料科学
多孔性
明渠流量
流量(数学)
大涡模拟
赫尔肖流
下降(电信)
粒子(生态学)
相对渗透率
外部流动
等温流动
沉积(地质)
密闭空间
微流控
计算流体力学
达西定律
球体
岩土工程
两相流
颗粒流
流线、条纹线和路径线
雷诺应力
粒径
毛细管压力
地质学
可压缩流
作者
Shuai Zhang,Qing Ma,Weiqiang Xie,Kai Liu,Yanlin Su,Mingxin Zhao,Zefan Wang,Jinpeng Zhao,Xiaoli Liu
标识
DOI:10.1073/pnas.2613597123
摘要
Particle deposition and migration within fractures can reorganize open void space into heterogeneous fracture-confined porous media (FCPM), yet the macroscopic flow behavior of these emergent systems remains unresolved. Here, Computational Fluid Dynamics–Discrete Element Method (CFD–DEM) simulations were used to resolve particle migration and deposition, whereas a coupled free-flow and seepage-flow model was employed to characterize fluid flow in FCPM. We find that at a fixed Reynolds number, modest particle deposition can lower the overall pressure drop relative to that of the initially open fracture. At high Reynolds numbers, the pressure drops across FCPM not only exceed Darcy’s law predictions (non-Darcy behavior) but, intriguingly, can also fall below them, which is a phenomenon we term super-Darcy behavior. This counterintuitive effect arises from flow exchange between the deposited porous region and the adjacent open region, which modifies eddy formation and growth, thereby broadening the main flow channel. This effect is pronounced when the permeability of the deposited porous region lies from 1 × 10 −12 to 1 × 10 −7 m 2 , identifying a permeability window in which deposition–migration most strongly couples pore-scale structure to fracture-scale hydraulics. This study reveals how particle deposition and transport govern macroscopic flow behavior in fractured channels, offering critical insights for fluid flow control and prediction from microfluidic devices to subsurface energy reservoirs.
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