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首页> 外文期刊>Environmental Geology >Unravelling preferential flow paths and estimating groundwater potential in a fractured metamorphic aquifer in Taiwan by using borehole logs and hybrid DFN/EPM model
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Unravelling preferential flow paths and estimating groundwater potential in a fractured metamorphic aquifer in Taiwan by using borehole logs and hybrid DFN/EPM model

机译:利用井筒测井和DFN / EPM混合模型揭示台湾一条裂变质含水层中的优先流动路径并估算地下水位

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This paper presents a practical-oriented approach for the characterization of preferential flow paths and modeling of three-dimensional fracture network in a fractured metamorphic aquifer that can be used to effectively evaluate groundwater potential in support of groundwater resources planning and management. This approach was demonstrated by using a couple of on-site hydrogeological tests and a hybrid numerical model at the Shuangliu well field situated in the Shungliou Forest Recreation Park, Southern Taiwan. The well field experiments have demonstrated that the combined downhole logging technique can successfully identify interconnection of permeable fractures, and have proved that the preferential flow paths is strongly associated with the major fracture orientation. Cross-borehole flowmeter tests have been confirmed as a useful technique to investigate preferential flow paths between boreholes. The modeling software FracMan was applied to develop a 3-D hybrid Discrete Fracture Network/Equivalent Porous Media (DFN/EPM) model with the aid of the above field tests, outcrop data and the identified scaling properties from fracture statistical analysis. Based on few outcrop data, the proposed 3-D hybrid model can appropriately predict the fracture geometry and locations of preferential flow paths for understanding the entire network structure and flow characteristics. However, collecting outcrop data as many as possible would firmly improve the prediction results of preferential flow paths in every study region. Finally, the validated model can be used to determine groundwater storage in a water planning area. Therefore, this study provides insight into effective fractured rock aquifer characterization and modeling to deal with the heterogeneity of fractured rock and improve the accuracy of groundwater storage computation.
机译:本文提出了一种以实践为导向的方法,用于描述裂隙变质含水层中优先流动路径的特征和三维裂隙网络的建模,可用于有效评估地下水潜力,以支持地下水资源的规划和管理。通过在台湾南部双流森林游乐公园的双流井场进行了两次现场水文地质测试和一个混合数值模型,证明了这种方法。井场实验表明,组合井下测井技术可以成功地识别渗透性裂缝的互连性,并证明优先流动路径与主要裂缝方向密切相关。跨孔流量计测试已被确认为研究井眼之间优先流动路径的有用技术。借助上述现场测试,露头数据和从裂缝统计分析中确定的结垢特性,建模软件FracMan被用于开发3-D离散裂缝网络/等效多孔介质(DFN / EPM)混合模型。基于少量露头数据,提出的3-D混合模型可以适当地预测裂缝的几何形状和优先流动路径的位置,以了解整个网络结构和流动特征。但是,收集尽可能多的露头数据将牢固地改善每个研究区域中优先流动路径的预测结果。最后,经过验证的模型可用于确定水规划区的地下水存储量。因此,本研究为有效处理裂隙岩层特征和建模提供了见识,以处理裂隙岩的非均质性并提高地下水储量计算的准确性。

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