首页> 外文会议>International Symposium on Advances in Isotope Hydrology and its Role in Sustainable Water Resources Management;IHS-2007 >GROUNDWATER RESOURCES FROM CARBONATEROCKS IN MOUNTAINOUS REGIONS:HYDROCHEMICAL AND ISOTOPIC SURVEY OFGROUNDWATERS IN THE WESTERN PYRENEES(FRANCE)
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GROUNDWATER RESOURCES FROM CARBONATEROCKS IN MOUNTAINOUS REGIONS:HYDROCHEMICAL AND ISOTOPIC SURVEY OFGROUNDWATERS IN THE WESTERN PYRENEES(FRANCE)

机译:山区碳酸盐岩的地下水资源:西比利牛斯(法国)地下水的化学和同位素调查

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Carbonate rock aquifers are one of the main water supply sources for the FrenchWestern Pyrenees. The discontinuous structure of these reservoirs is a main obstacle tothe development of such resources. By the way, since no other aquifer can be tapped,many communities have decided to improve their knowledge of the main springs overthe whole region. Four sites have been considered from 2003 to 2006 and have beenthe object of multidisciplinary investigations including: geological mapping, geophysicalinvestigations, dye tracing experiments and in situ hydrochemical survey. Stable isotopeshave been analysed on both rainfall ( 18O, 2H) and spring waters ( 18O, 2H, 13C, 34S) inorder to evaluate the origin of groundwaters, their residence time within the systemsand to appreciate the occurrence of exchanges with other aquifers. Finally, this studyprovides a good example of how to include hydrogeochemistry and isotopic tools in awater supply management policy.
机译:碳酸盐岩含水层是法国人的主要供水来源之一 西比利牛斯山脉。这些储层的不连续结构是影响储层的主要障碍。 开发这类资源。顺便说一句,由于没有其他的含水层可以被挖掘, 许多社区已经决定提高对主要泉水的了解 整个地区。从2003年到2006年,已经考虑了四个地点, 多学科研究的对象包括:地质制图,地球物理 调查,染料追踪实验和原位水化学调查。稳定同位素 已经对降雨(18O,2H)和泉水(18O,2H,13C,34S)进行了分析 为了评估地下水的来源,它们在系统中的停留时间 并感谢与其他含水层交换的机会。最后,这项研究 提供了一个很好的示例,说明如何在 供水管理政策。

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