硬岩含水层调查与管理的新概念:单块法

K. Yao, O. Fouché
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引用次数: 0

摘要

测量区位于前寒武纪变质-深裂带Côte科特迪瓦西南部。为了突出显示基地的公里级裂缝网络,使用了遥感技术。卫星图像处理后得到的地形图将研究区离散成块状含水层。这是研究硬岩中地下水循环的一种新方法,它允许从区域视角到局部尺度。这些区块由张开或堵塞的裂缝隔开,这些裂缝可以起到导电或防水的作用,甚至可以起到电容器的作用。几何块体参数的统计和分形分析表明,几何块体参数反映了硬岩中小裂缝(裂隙层)在地下水流动中的连通性和重要性。在小块中观察到的高产量证实了这一报告。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A new concept for hard rock aquifers survey and management: individual blocks approach
The survey area is located south-west of Côte d'Ivoire in Precambrian metamorphic and plutonic zone. To highlight the network of kilometer-scale fractures in the base, remote sensing techniques were used. The map of lineaments obtained after processing of satellite images discretized the study area into blocks aquifers. This is a new approach in the study of the circulation of groundwater in hard-rock which allows going from a regional view to a local scale. The blocks were delimited by opened or clogged fractures that can have a conducting or watertight function, even a capacitor role. Statistical and fractal analyses of the geometric block parameters showed that those ones revealed the connectivity degree and the importance of the small fractures (fissured layer) in groundwater flow in hard-rock. This report is confirmed by high yields observed in the small blocks.
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