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Delineation of Ground Water Recharge Zones in Hard Rock Terrain of Tamil Nadu

机译:泰米尔纳德邦硬岩地形中地下水补给区的划分

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Ground water resources diminish at alarming rates in hard rock regions as it is the primary source of irrigation as well as domestic purpose. Periodic replenishment of ground water in these areas is only through rainfall. Delineation of potential groundwater recharge zones in hard rock areas is of vital importance to enhance the recharge. Conventionally, suitable zone for groundwater recharge is deciphered using hydrogeological, geophysical and geomorphological maps, which is often time consuming anduneconomical. But, the analysis of unconfined aquifer response in terms of rise in water level due to precipitation in hard rock areas is one of the rapid and cost-effective methods. Cross-correlation of rise in water level and precipitation is established for Parambikulam-Aliyar-Palar (PAP) basin of TamilNadu, India to delineate groundwater recharge zones. The entire area is classified into various recharge zones depending on coefficient of correlation. Thus, decisions on construction of recharge structures / optimal pumping in these areas can be decided for sustainable ground water resource management to meet future demands.
机译:硬岩地区的地下水资源以惊人的速度减少,因为它是灌溉和家庭用途的主要来源。仅通过降雨定期补充这些地区的地下水。划定硬岩地区潜在的地下水补给区对于提高补给至关重要。常规地,使用水文地质,地球物理和地貌图来破译适合于地下水补给的区域,这通常是费时且不经济的。但是,根据硬岩地区降水引起的水位升高来分析无侧限含水层响应是一种快速且经济高效的方法。为印度泰米尔纳德邦的Parambikulam-Aliyar-Palar(PAP)盆地建立了水位上升与降水之间的相互关系,以描绘地下水补给区。根据相关系数,将整个区域分为多个补给区。因此,可以决定在这些地区建设补给结构/优化抽水,以实现可持续的地下水资源管理,以满足未来的需求。

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