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A Rock Mass Classification Scheme for Estimating Hydraulic Conductivity of Fractured Rocks

机译:岩体分类方案估算裂隙岩体的水力传导率

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This paper proposes a new application of the rock mass classification concept on the estimation of hydraulic conductivity of fractured rocks. The new rock mass classification system called as " HC-system" based on the following four parameters: rock quality designation (RQD), depth index (DI), gouge content designation (GCD), and lithology permeability index (LPI). HC-values can be calculated from borehole image data and rock core data. To verify rationality of the defined HC-system, the study collected data from the results of two hydrogeological investigation programs in three boreholes to determine a relationship between hydraulic conductivity and HC. Regression analysis was performed to estimate the dependence of HC on hydraulic conductivity. The regression results indicated that a power law relationship exists between the two variables with a coefficient of determination of 0.866. The regression equation provides a useful tool to predict hydraulic conductivity of fractured rocks based on measured HC-values. By using this regression equation, hydraulic conductivity data in a given site can be directly acquired, which removes the cost on hydraulic tests. For in-situ aquifer tests, the HC-system is a valuable new rock mass classification system for preliminary assessment of the degree of permeability in a packed-off interval of a borehole.
机译:本文提出了岩体分类概念在裂隙岩体水力传导率估算中的新应用。基于以下四个参数的新岩体分类系统称为“ HC系统”:岩石质量指定(RQD),深度指数(DI),凿岩含量指定(GCD)和岩性渗透率指数(LPI)。 HC值可以根据井眼图像数据和岩心数据进行计算。为了验证所定义的HC系统的合理性,该研究从三个钻孔的两个水文地质调查计划的结果中收集了数据,以确定水力传导率和HC之间的关系。进行回归分析以估计HC对水力传导率的依赖性。回归结果表明,两个变量之间存在幂律关系,确定系数为0.866。回归方程为基于测得的HC值预测裂隙岩的水力传导率提供了有用的工具。通过使用该回归方程,可以直接获取给定位置的水力传导率数据,从而省去了水力测试的费用。对于现场含水层测试,HC系统是一种有价值的新型岩体分类系统,可用于初步评估井眼的密集层段中的渗透率。

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