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Hydraulic conductivity characterization of a karst recharge area using water injection tests and electrical resistivity logging

机译:岩溶补给区水力传导特性的注水试验和电阻率测井

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摘要

Water injection tests and electrical logging are particularly useful techniques in the characterization of geological media in engineering works. In this paper these techniques in conjunction with cracks measurements obtained from drilling cores, were used in the characterization of a singular location in a karst massif. The aim of our work is to determine the hydraulic characteristics of the investigated site, as well as to establish the relationship between the data obtained by the different techniques used. Thus, electrical resistivity records and fracture data were obtained from two boreholes of 100 and 120 m depth. Hydraulic conductivity was calculated from 25 low-pressure water injection tests (LPT) carried out at different depths in both boreholes. The relationship between hydraulic conductivity and fracture frequency was not very statististically significant (R~2: 0.062–0.672; σ_(est): 0.61–1.575). Conversely, electrical resistivity and hydraulic conductivity had a great relationship (R~2: 0.725–0.935; σ_(est): 0.159–0.738), so the electrical resistivity may be related to the functionality of the fractures. Finally, the LPT is shown as a very practical tool for determining the degree of the hydraulically interconnection with the surroundings, for establishing the hydraulic conductivity profile and for obtaining a measure of soil erosionability according to the significance of the fracture washing out processes recorded.
机译:注水测试和电测井是在工程工作中表征地质介质的特别有用的技术。在本文中,这些技术结合从钻芯获得的裂缝测量结果,被用于岩溶地块奇异位置的表征。我们的工作目的是确定调查地点的水力特征,并建立通过使用不同技术获得的数据之间的关系。因此,从两个深度为100和120 m的钻孔中获得了电阻率记录和裂缝数据。通过在两个钻孔中不同深度进行的25次低压注水试验(LPT)计算出水力传导率。导水率和断裂频率之间的关系在统计学上不是很显着(R〜2:0.062-0.672;σ_(est):0.61-1.575)。相反,电阻率和水力传导率有很大的关系(R〜2:0.725-0.935;σ_(est):0.159-0.738),因此电阻率可能与裂缝的功能性有关。最后,LPT被显示为一种非常实用的工具,用于根据记录的裂缝冲洗过程的重要性来确定与周围环境的水力互连程度,建立水力传导率曲线并获得土壤侵蚀性的度量。

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