Isotopic differentiation of groundwater recharge processes in a semi-arid region of southern India

被引:3
|
作者
Gopinath, Girish [1 ,2 ]
Resmi, T. R. [3 ]
Pragath, M. [1 ]
Jesiya, N. P. [1 ]
Hameed, A. Shahul [3 ]
Deshpande, R. D. [4 ]
机构
[1] CWRDM, Geomat Div, Kozhikode 673571, Kerala, India
[2] Kerala Univ Fisheries & Ocean Studies KUFOS, Dept Climate Variabilty & Aquat Ecosyst, Kochi 682508, Kerala, India
[3] CWRDM, Isotope Hydrol Div, Kozhikode 673571, Kerala, India
[4] Phys Res Lab, Geosci Div, Ahmadabad 380009, Gujarat, India
关键词
Groundwater recharge source; Different recharge processes; Coastal and inland aquifers; Stable isotopes; Tuticorin; TAMIL-NADU; ENVIRONMENTAL ISOTOPES; SEAWATER INTRUSION; COASTAL AQUIFERS; CENTRAL KERALA; RIVER-BASIN; WATER; SALINIZATION; TUTICORIN; STRONTIUM;
D O I
10.1007/s12665-021-09816-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Ensuring the availability of adequate quantity and quality of water to meet demands of domestic sector has become the prime objective for the developing countries like India. The coastal and the nearby inland region are the places of intense human activity due to urbanisation and industrialization leading to the depletion and degradation of environmental resources. The present investigation on the coastal and inland aquifers of Tuticorin, Gulf of Mannar, Tamil Nadu aims to better understand the recharge characteristics, factors controlling recharge, effect of weather parameters on recharge, source of recharge water, differences between inland and coastal recharge processes and climatic signature in groundwater isotopic composition from the hydrochemical and stable isotope data. Different mechanisms of salinization in the coastal aquifers were deduced as direct influence of the sea water and concentrations of ions by evaporation. The dissolution or leaching from the aquifer material is also imparting salinity to groundwater in this area.
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页数:12
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