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Estimation of Hydraulic Conductivity Tensor of Nearly-horizontal Stratified Fractured Rock Mass Based on Seepage-Stress Coupling Theory
WANG Jun-zhi, CHEN Yan-guo, ZHANG Hai-feng, WAN Wei-feng
Journal of Changjiang River Scientific Research Institute ›› 2025, Vol. 42 ›› Issue (2) : 115-121.
PDF(6037 KB)
PDF(6037 KB)
Estimation of Hydraulic Conductivity Tensor of Nearly-horizontal Stratified Fractured Rock Mass Based on Seepage-Stress Coupling Theory
Quantitative evaluation of the permeability and anisotropy of fractured rock masses is crucial for engineering geological investigations in water conservancy and hydropower projects. Such evaluations provide essential technical support for designing anti-seepage curtains, foundation pit drainage systems, and predicting water inrush in hydraulic tunnels. In this paper, we introduce a method for estimating the hydraulic conductivity tensor of nearly horizontally layered fractured rock masses based on “seepage-stress” coupling theory. This method integrates conventional vertical borehole water pressure tests, horizontal directional borehole water pressure tests, and rock mass stress tests. By establishing a negative exponential function relationship between normal stress and aperture, the equivalent hydraulic aperture of the structural plane is estimated, and the hydraulic conductivity tensor of the rock mass is calculated. This method has been applied to the Guxian water resources management project on Yellow River as a case study. The anisotropy of the hydraulic conductivity in the dam site area was analyzed. Results demonstrate that, compared with conventional vertical borehole water pressure tests, the proposed method better characterizes the permeability and anisotropic properties of the rock masses. Specifically, the comprehensive permeability coefficient obtained using the proposed method is approximately 15 times that of conventional tests, providing valuable scientific guidance for the design of seepage control engineering.
fractured rock mass / hydraulic conductivity tensor / directional water pressure test / in-situ stress test / Yellow River Guxian water resources management project
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岩体结构面产状数据的统计分组是工程地质、水文地质工作中基础但十分重要的环节。常用的倾向、走向玫瑰花图和极点等密度图人为主观因素大,需借助合适的数学手段对结构面产状数据进行客观划分。基于K-means聚类方法和I Index聚类有效性检验指标,提出了一种岩体结构面自动分组方法,并开发了岩体结构面自动分组程序RDAP。通过与经典文献进行对比,验证了所提分组方法的可靠性。最后,以某工程为例,使用RDAP对实测涌水裂隙资料进行了预处理,初步计算了灌浆钻孔的最佳方位,为工程涌水的防治提供了依据。
Classifying the orientations of rock discontinuities is a fundamental but critically important routine of engineering geology and hydrogeology. The commonly-used rose diagrams of dip directions and strikes and poles to orientations are subjective. It is appreciated to resort to mathematical approaches. In this paper, an automatic grouping method is proposed based on the algorithms of <i>K</i>-means cluster analysis and cluster validity index <i>I</i>, and a Rock Discontinuities Auto-classification Program (RDAP) is developed. By comparing with Shanley and Mahtab’s result (1976), the reliability of the new grouping method or RDAP is verified. In the end, RDAP is used to cluster the gushing fractures to aid in the selection of the optimum position of grouting drillings of a project, which provides a basis for the prevention and control of water gushing.
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