资源环境科技发展态势分析平台

A fundamental understanding of the fluid movement and dynamic partitioning process at fracture intersections is important to accurately predict water infiltration and contaminant transport in networks of fractures. We present an experimental study on the flow-splitting behavior at a T-shaped intersection. Different combinations of apertures of the vertical (b(v)) and horizontal (b(h)) fractures are considered. Experimental results confirm that the gravity-driven flow in the vertical fracture transitions from droplet to rivulet mode as the flow rate increases. We quantify the flow dynamics through the intersection and especially focus on the partitioning efficiency (eta) defined as the percentage of flow partitioned into the horizontal fracture. We identify three regimes of flow partitioning at the intersection for the case of b(v) < b(h): total partitioning (eta -> 1), splitting or partial bypass (0 < eta < 1), and total bypass (eta -> 0). The total bypass regime is associated with the rivulet mode with a flow rate higher than similar to 1.5 ml/min. We find a simple relationship between eta and the flow rate Q for droplet flow, eta = min(1, C(h)Q(-1)), where C-h is a threshold flow rate below which droplets almost completely imbibe into the horizontal fracture, leading to eta -> 1. A force balance analysis links C-h to a critical droplet length for the transition from complete partitioning to path splitting. The obtained relationship is further supported by numerical simulations of droplet flow through intersections. The results and analysis from this study may provide insights and physical constraints on construction of reduced order unsaturated flow models based on simplified discrete fracture networks.