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Evaluation of Forchheimer equation coefficients for non-Darcy flow in deformable rough-walled fractures

机译:变形粗糙壁裂缝非达西渗流的Forchheimer方程系数评估

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This study focuses on experimental evaluation of the Forchheimer equation coefficients for non-Darcy flow in deformable rough-walled fractures. Water flow tests through twelve granite fracture samples with different roughness were conducted in a triaxial cell under confining stresses varying from 1.0 MPa to 30.0 MPa. A total of 2280 experimental data in the form of pressure gradient versus discharge were collected. Three representative types of nonlinear flow behaviors induced by inertial effect, fracture dilation and solid water interaction, respectively, were observed. Regression analyses of the experimental data show that the Forchheimer equation adequately describes the non-Darcy flow behavior induced by significant inertial effect. Based on the experimental observations, two empirical equations were proposed for parametric expression of the Forchheimer's nonlinear coefficient, one as a power function of hydraulic aperture and the other dependent on both hydraulic aperture and peak asperity of the fracture surface. A new criterion was presented for assessing the applicability of Darcy's law, which relies on the ratio of discharge or pressure gradient predicted by the Forchheimer's law incorporated with the single-parameter equation to that predicted by the Darcy's law. A sensitivity analysis was performed using the double-parameter equation for examining the dependence of the Forchheimer's nonlinear coefficient on peak asperity, demonstrating the importance of incorporating the fracture roughness in the development of non-Darcy flow models. The experimental results and the proposed models are useful for understanding and numerical modeling of the nonlinear flow behaviors in fractured aquifers. (C) 2015 Elsevier B.V. All rights reserved.
机译:这项研究的重点是对可变形粗糙壁裂缝中非达西渗流的Forchheimer方程系数进行实验评估。在三轴单元中,在1.0 MPa至30.0 MPa的限制应力下,通过十二个具有不同粗糙度的花岗岩破裂样品进行了水流测试。总共收集了2280个压力梯度与排放量关系形式的实验数据。分别观察到三种由惯性效应,断裂膨胀和固水相互作用引起的非线性流动行为。实验数据的回归分析表明,Forchheimer方程充分描述了由显着惯性效应引起的非达西流动行为。根据实验观察结果,提出了两个经验公式来对Forchheimer非线性系数进行参数化表达,一个是水力开孔的幂函数,另一个是水力开孔和断裂面的峰值粗糙度。提出了评估达西定律的适用性的新标准,该标准依赖于结合了单参数方程的Forchheimer定律预测的流量或压力梯度与达西定律预测的比率。使用双参数方程式进行了敏感性分析,以检查Forchheimer非线性系数对峰粗糙度的依赖性,这表明在开发非达西流模型时将裂缝粗糙度纳入考虑中的重要性。实验结果和所提出的模型对于理解裂缝含水层中的非线性流动行为和进行数值建模非常有用。 (C)2015 Elsevier B.V.保留所有权利。

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