岩体粗糙裂隙几何特征对其Forchheimer型渗流特性的影响
Effects of geometrical feature on Forchheimer-flow behavior through rough-walled rock fractures
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摘要: 为了研究岩体粗糙裂隙几何特征与其非线性渗流特性的相互关系,基于裂隙面分形特性提出了三维粗糙裂隙的几何结构表征模型,通过直接求解N-S(Navier-Stokes)方程,研究了不同开度均值、标准差和分形维数对岩体裂隙Forchheimer型渗流特性的影响规律,验证了Forchheimer方程描述流量与压力梯度非线性关系的有效性。研究结果表明:当流量较小时,随着裂隙开度均值减小、标准差增大,线性系数逐渐增大即水力开度逐渐减小,渗透能力下降,分形维数对其渗透能力的影响较小,并提出了水力开度与开度均值、标准差的经验关系式;当流量较大时,水流流态从线性流向非线性流转变,随着开度均值减小、标准差和分形维数的增大,非线性系数增大,临界雷诺数减小,测得Rec范围为11.16~39.3。Abstract: In order to study the relationship between the geometrical feature and the nonlinear flow properties of rough-walled rock fractures, a numerical model based on the fractal behavior is proposed to characterize the three-dimensional geometry of rough-walled fractures. By solving the N-S (Navier-Stokes) equation directly, the effects of mean aperture, standard deviation of aperture and different fractal dimensions on the Forchheimer flow characteristics of fractures are investigated. The Forchheimer equation is validated to describe the nonlinear relationship between the flow rate and the pressure gradient. The results show that with the lower flow rate, the linear coefficient increases and the hydraulic aperture decreases with the decreasing mean aperture and increasing standard deviation of the aperture, thus the empirical relation for the hydraulic aperture, the mean aperture and the standard deviation of aperture is put forward, while the effects of the fractal dimension almost can be ignored. On the contrary, with larger flow rate, for the flow pattern changing from linear to nonlinear flow, as the mean aperture decreases and the standard deviation of aperture and the fractal dimension increase, the nonlinear coefficient increases, and the critical Reynolds number decreases, with the range of Rec being 11.16~39.3.