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Groundwater management options in North district of Delhi, India: A groundwater surplus region in over-exploited aquifers

机译:印度德里北区的地下水管理选择:过度开采含水层中的地下水过剩地区

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Study region North district of Delhi, India. Study focus The North district of Delhi has mostly shallow water levels and is a groundwater surplus region in contrast to the over-exploited aquifers of the region. The surface runoff and flood waters during monsoon season in the district either causes water logging in lower elevation areas or they join drains and rivers as rejected recharge. This study aims to understand groundwater dynamics of the region in perspective of the aquifer architecture and proposes groundwater management options to meet local water requirements. New hydrological insights in the region Three distinct hydrogeological domains are identified with subtle differences in groundwater occurrence. Insights are obtained in stream–aquifer interaction and baseflow to the Yamuna River is quantified. The salinity enrichment in groundwater has been attributed to water logging in clay rich formations under semi arid condition. The viability of limited dewatering of shallow aquifers and its replenishment by enhanced recharge from surface runoff and flood waters during the monsoon period have been established.
机译:研究区域印度德里北区。研究重点德里北部地区的水位主要是浅水,与该地区过度开采的含水层相比,它是一个地下水过剩的地区。在该地区的季风季节,地表径流和洪水要么导致较低海拔地区的水涝,要么由于排泄物的缺乏而与排水沟和河流汇合。这项研究旨在从含水层结构的角度了解该地区的地下水动力学,并提出满足当地水需求的地下水管理方案。该地区的新水文见解识别出三个截然不同的水文地质领域,这些地区在地下水发生方面存在细微差异。在水流相互作用中获得了见解,并对亚穆纳河的基流进行了量化。地下水中盐分的富集归因于半干旱条件下富粘土地层的水浸。在季风期间,确定了浅层含水层有限脱水的可行性,并通过增加地表径流和洪水的补给来补充水。

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