Nitrate-leaching and groundwater vulnerability mapping in North Bihar, India

被引:5
作者
Gupta, Pankaj Kumar [1 ]
Kumari, Binita [2 ]
Gupta, Saurabh Kumar [2 ]
Kumar, Deepak [3 ]
机构
[1] Univ Waterloo, Fac Environm, Waterloo, ON, Canada
[2] Cent Univ Jharkhand, Dept Geoinformat, Ranchi 835205, Bihar, India
[3] GB Pant Univ Agr & Technol, Dept Soil & Water Conservat Engn, Coll Technol, Pantnagar 263153, Uttar Pradesh, India
关键词
Vadose zone; Groundwater resource; Pollution; Nitrate; Vulnerability; Clay capping; DRASTIC MODEL; AQUIFER VULNERABILITY; SHALLOW AQUIFER; HYDRAULIC CONDUCTIVITY; CONTAMINATION; VARIABILITY; TRANSPORT; DISTRICT;
D O I
10.1007/s40899-020-00405-8
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Aquifer vulnerability assessment is crucial for studying the impact of increasing pollution load scenarios on the quantification of contaminant concentration with movement of plume for protecting groundwater resources. Only a few recent studies have focused on the performance evaluation of vulnerability assessment methods using process-based modeling approach. However, the moisture flow and pollutant transport through partially saturated zone plays a crucial role under varying hydrogeological conditions, which are generally ignored in index-based methods. Thus, the objective of this research is to evaluate the vulnerability of groundwater resources to nitrate in Samastipur, Darbhanga and Madhubani districts of Bihar State, India, using soil moisture flow and solute transport modeling. Richard's equation integrated with the classical advection dispersion equation is simulated using HYDRUS 1D by incorporating a constant head and atmospheric boundary conditions. The time taken to reach the nitrate peak concentration at groundwater table is considered to estimate vulnerability index (VI). Results have shown that high risk in terms of nitrate-leaching vulnerability in southern part of study area is dominated by Gangetic kankar in subsurface. Further, high pollution risk was reported in eastern north part of study area having alluvial deposition in subsurface. The main causes of high risk were due to the short depth of water table, little discharge and more hydraulic conductivity presence in the subsurface media. Moreover, comparatively low vulnerability was observed in area having clay capping of 2-4 m from surface. This research may help in better implementation of agricultural, soil-water conservation practices and urban/industrial infrastructure development in and around the study area.
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页数:12
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