Department of Geology and Geophysics, Indian Institute of Technology Kharagpur, 721 302, India.
Department of Geology and Geophysics, Indian Institute of Technology Kharagpur, 721 302, India; School of Environmental Science and Engineering, Indian Institute of Technology Kharagpur, 721 302, India; Applied Policy Advisory to Hydrogeosciences Group, Indian Institute of Technology, Kharagpur, 721302, India.
J Environ Manage. 2021 Jun 15;288:112384. doi: 10.1016/j.jenvman.2021.112384. Epub 2021 Mar 25.
Groundwater resources in South Asian cities are facing immense stress due to over-extraction leading to environmental, social and economic instabilities. The perennial mega rivers of Himalayas form the lifeline for South Asia, underpinning food and water security for a large population both directly and indirectly through exchange with groundwater systems. The present study delineates the spatio-temporal variation in patterns and processes of sub-hourly to annual-scale hydrological exchanges between the Ganges and its adjoining highly exploited aquifer in a urban-peri urban reach. Multivariate statistical analyses established river water-groundwater interaction in this region with ~40% loading of first principal component, i.e river water during monsoon on the shallow aquifer. The part of the aquifer detached from the main confined aquifer show an influence of precipitation (the second principal component) with loading of ~90%. Again the part of the aquifer suffering infiltration of local surface water bodies show effect of precipitation with a second principal loading of ~80%. Fourier transformation is used in the hydrograph to remove influence of heavy urbanization on the hydrographs. This study proves that the phenomenon of infiltrating river water during monsoon plays a primary role in controlling aquifer storage although contaminating the aquifer simultaneously. However, during pre and post-monsoon the flow path reversal helps in maintaining river baseflow. Cross-correlation between the river and piezometric series show increased delay of pressure head propagation of the infiltrating river waterfront, with increasing distance. These observations are also substantiated by stable isotope signatures. The present study provides an understanding of potential groundwater vulnerability resulting from waste water and irrigational contamination through river water intrusion which would eventually lead the government to implement proper water and environmental management policies towards availability of long-term sustainable water resources for the residents.
南亚城市的地下水资源正面临着巨大的压力,由于过度开采导致环境、社会和经济不稳定。喜马拉雅山的常年大河是南亚的生命线,通过与地下水系统的交换,直接和间接地为大量人口提供了粮食和水安全。本研究描绘了恒河及其毗邻高度开采含水层在城市-城郊范围内亚小时到年尺度水文交换模式和过程的时空变化。多元统计分析确定了该地区河流水-地下水相互作用,第一主成分的负载约为 40%,即季风期间浅层含水层的河水。与主承压含水层分离的含水层部分受降水(第二主成分)影响,负载约为 90%。再次,遭受当地地表水体渗透的含水层部分受降水影响,第二主负荷约为 80%。傅里叶变换用于流量图中,以消除城市化对流量图的影响。本研究证明,尽管同时污染了含水层,但季风期间渗透河水的现象在控制含水层储水方面起着主要作用。然而,在季风前和季风后,水流路径的反转有助于维持河流基流。河流和测压计系列之间的互相关显示,随着距离的增加,渗透河滨水头传播的压力延迟增加。这些观测结果也得到了稳定同位素特征的证实。本研究提供了对潜在地下水脆弱性的理解,这种脆弱性是由于废水和灌溉污染通过河水入侵造成的,这最终将促使政府实施适当的水和环境管理政策,为居民提供长期可持续水资源。