H23B-1591
Effect of roughness on water flow through a single rough fracture
Tuesday, 15 December 2015
Poster Hall (Moscone South)
Zhou Chen1, Zhifang Zhou2, Jinguo WANG2, Qiaona Guo2 and Zhi Dou3, (1)Hohai University, Nanjing, China, (2)Hohai University, School of Earth Science and Engineering, Nanjing, China, (3)Hohai University, Toronto, ON, Canada
Abstract:
A single fracture (SF) usually has rough surfaces with points of contact. Though relative roughness was considered in quantifying flow through a single rough fracture (SRF) previously, additional factors such as the distribution of rough elements and bending degree of streamlines are rarely considered before. Semi-empirical friction factor (f) and discharge per unit width (q) equations are first deduced based on the consideration of relative roughness, roughness elements distribution and streamline reattachment length in this study. A horizontal SRF model is set up and a series of experiments and simulations are performed. Main conclusions are drawn: recirculation of streamlines occurred in the rough element and its intensity increases with the entering angle of the streamlines into the element and Reynolds number (Re); streamlines are discontinuously distributed when asperity height is large, leading to departure from Darcy’s law (non-linear flow); the non-linearity of flow increases with the asperity height and Re; the relative roughness for not affecting water flow through a SRF should be much less than 0.033, a benchmark value commonly used previously for neglecting the roughness effect; the revised f and q equations under laminar flow through a SRF are shown to be better than previously proposed equations.