首页> 外文会议>International Symposium on Advances in Isotope Hydrology and its Role in Sustainable Water Resources Management >GROUNDWATER RESOURCES FROM CARBONATE ROCKS IN MOUNTAINOUS REGIONS: HYDROCHEMICAL AND ISOTOPIC SURVEY OF GROUNDWATERS IN THE WESTERN PYRENEES (FRANCE)
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GROUNDWATER RESOURCES FROM CARBONATE ROCKS IN MOUNTAINOUS REGIONS: HYDROCHEMICAL AND ISOTOPIC SURVEY OF GROUNDWATERS IN THE WESTERN PYRENEES (FRANCE)

机译:来自山区碳酸盐岩石的地下水资源:西比利牛斯特地下水的水化学和同位素调查(法国)

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Carbonate rock aquifers are one of the main water supply sources for the French Western Pyrenees. The discontinuous structure of these reservoirs is a main obstacle to the 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 over the whole region. Four sites have been considered from 2003 to 2006 and have been the object of multidisciplinary investigations including: geological mapping, geophysical investigations, dye tracing experiments and in situ hydrochemical survey. Stable isotopes have been analysed on both rainfall ( 18O, 2H) and spring waters ( 18O, 2H, 13C, 34S) in order to evaluate the origin of groundwaters, their residence time within the systems and to appreciate the occurrence of exchanges with other aquifers. Finally, this study provides a good example of how to include hydrogeochemistry and isotopic tools in a water supply management policy.
机译:碳酸盐岩含水层是法国西方比利牛斯特的主要供水来源之一。这些水库的不连续结构是发展这些资源的主要障碍。顺便说一下,由于没有其他含水层,许多社区已经决定改善他们对整个地区的主弹簧的了解。从2003年到2006年被考虑了四个站点,并成为多学科调查的对象,包括:地质测绘,地球物理调查,染料追踪实验和原位水化学调查。在降雨(18O,2H)和弹簧水(18O,2H,13C,34S)上进行了稳定的同位素,以便评估地下水的起源,它们在系统内的停留时间并欣赏与其他含水层的交易所发生。最后,本研究提供了如何在供水管理政策中包括水文地球化学和同位素工具的良好示例。

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