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首页> 外文期刊>Rock Mechanics and Rock Engineering >Correlations Developed for Estimation of Hydraulic Parameters of Rough Fractures Through the Simulation of JRC Flow Channels
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Correlations Developed for Estimation of Hydraulic Parameters of Rough Fractures Through the Simulation of JRC Flow Channels

机译:通过JRC流道模拟估算粗糙裂缝水力参数的相关性

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摘要

The hydro-mechanical response of fractured rock masses is complex, due partly to the presence of fractures at different scales. Surface morphology has a significant influence on fluid flow behaviour of a fracture. Different empirical correlations and statistical models have been proposed to estimate the equivalent hydraulic aperture and determine the pressure drop along a fracture. However, the existing models suffer from not being adequately generalised to be applicable to a wide range of real fracture surfaces. To incorporate the effect of profile roughness in the hydro-mechanical behaviour of fractured rock masses, the joint roughness coefficient (JRC) is the most widely used empirical approach. However, the average JRC of two fracture walls in fluid flow analysis, as is a common practice, appears to be inappropriate. It will be shown how different combinations of pairs of JRCs could lead to a similar JRC value. Also, changing the position of the top and bottom walls of a fracture can significantly change the hydraulic response of the fracture while the average JRC is identical in both cases. In this paper, correlations are developed which are based on the simulation of JRCs using estimated fluid flow parameters of 2D fractures can be estimated. In order to widen the application range of the correlations, JRC flow channels were generated: these are 2D channels with their top and bottom walls being made from two of the JRC profiles. To estimate the JRC of linear profiles, a correlation developed between JRC and a newly developed Riemannian roughness parameter, D_(R1), is proposed. Considering ten JRC profiles, a total of 100 JRC flow channels were generated. In order to only investigate the effect of surface roughness on fluid flow, the minimum closure between the top and bottom walls of JRC flow channels were considered to be constant. Three cases with minimum closures of 0.01, 0.05 and 0.10 cm were considered in this study. All JRC flow channels were subjected to fluid analysis using FLUENT software. Based on these results, correlations were developed between the geometrical and hydraulic properties of flow channels. Analysis of several real fractures demonstrated the applicability of these correlations.
机译:裂隙岩体的水力力学响应是复杂的,部分原因是存在不同规模的裂隙。表面形态对裂缝的流体流动行为有重要影响。已经提出了不同的经验相关性和统计模型来估计等效液压孔径并确定沿裂缝的压降。但是,现有模型的不足之处在于不能广泛推广到适用于各种实际断裂面的情况。为了将轮廓粗糙度的影响纳入裂隙岩体的流体力学行为中,节理粗糙度系数(JRC)是使用最广泛的经验方法。但是,按照常规做法,在流体流动分析中,两个裂缝壁的平均JRC似乎是不合适的。将显示成对的JRC对的不同组合如何导致相似的JRC值。同样,改变裂缝的顶壁和底壁的位置可以显着改变裂缝的水力响应,而两种情况下的平均JRC值相同。在本文中,开发了相关性,这些相关性基于JRC的模拟,可以使用2D裂缝的估计流体流量参数进行估计。为了拓宽相关性的应用范围,生成了JRC流道:这些是二维通道,其顶壁和底壁由两个JRC轮廓制成。为了估计线性轮廓的JRC,提出了JRC与新开发的黎曼粗糙度参数D_(R1)之间的相关性。考虑十个JRC轮廓,总共生成了100个JRC流道。为了仅研究表面粗糙度对流体流动的影响,JRC流道的顶壁和底壁之间的最小闭合被认为是恒定的。在本研究中考虑了3个最小闭合度分别为0.01、0.05和0.10 cm的情况。使用FLUENT软件对所有JRC流道进行了流体分析。基于这些结果,在流动通道的几何和水力特性之间建立了相关性。对几个实际裂缝的分析证明了这些相关性的适用性。

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