Assessing Groundwater Resource Vulnerability by Coupling GIS-Based DRASTIC and Solute Transport Model in Ajmer District, Rajasthan

被引:16
作者
Joshi, Pranjay [1 ]
Gupta, Pankaj Kumar [2 ]
机构
[1] GB Pant Univ Agr & Technol, Pantnagar 263145, Uttar Pradesh, India
[2] Indian Inst Technol Roorkee, Dept Hydrol, Roorkee 247667, Uttar Pradesh, India
关键词
HARD-ROCK; AQUIFER; SALINIZATION; POLLUTION; SOUTH;
D O I
10.1007/s12594-018-0958-y
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Groundwater aquifer vulnerability has been assessed by incorporating the major geological and hydrogeological factors that affect and control the groundwater contamination using GIS-based DRASTIC model along with solute transport modeling. This work demonstrates the potential of GIS to derive a vulnerability map by overlying various spatially referenced digital data layers (i.e., depth to water, net recharge, aquifer media, soil media, topography, the impact of vadose zone and hydraulic conductivity) that portrays cumulative aquifer sensitivity ratings in Kishangarh, Rajasthan. It provides a relative indication of groundwater aquifer vulnerability to contamination. The soil moisture flow and solute transport regimes of the vadose zone associated with specific hydrogeological conditions play a crucial role in pollution risk assessment of the underlying groundwater resources. An effort has been made to map the vulnerability of shallow groundwater to surface pollutants of thestudy area, using soil moisture flow and contaminant transport modeling. The classical advection-dispersion equation coupled with Richard's equation is numerically simulated at different point locations for assessing the intrinsic vulnerability of the valley. The role of soil type, slope, and the land-use cover is considered for estimating the transient flux at the top boundary from daily precipitation and evapotranspiration data of the study area. The time required by the solute peak to travel from the surface to the groundwater table at the bottom of the soil profile is considered as an indicator of avulnerability index. Results show a high vulnerability in the southern region, whereas low vulnerability is observed in the northeast and northern parts. The results have recognized four aquifer vulnerability zones based on DRASTIC vulnerability index (DVI), which ranged from 45 to 178. It has been deduced that approximately 18, 25, 34, and 23% of the area lies in negligible, low, medium and high vulnerability zones, respectively. The study may assist in decision making related to theplanning of industrial locations and the sustainable water resources development of the selected semi-arid area.
引用
收藏
页码:101 / 106
页数:6
相关论文
共 26 条
[1]  
Akhtar M M, 2014, GEOFISICA INT, V54, P67
[2]  
ALBINET M., 1970, Bull BRGM 2me Series, V3, P13
[3]  
Aller L., 1987, V600287035622 EPA
[4]  
[Anonymous], METHOD COLLECTION AN
[5]  
[Anonymous], 1984, GUID DRINK QUAL
[6]  
[Anonymous], GROUNDW PERSP PROF D
[7]  
APHA, 1985, STAND METH EX WAT WA
[8]   A GIS-based DRASTIC model for assessing aquifer vulnerability in Kakamigahara Heights, Gifu Prefecture, central Japan [J].
Babiker, IS ;
Mohamed, MAA ;
Hiyama, T ;
Kato, K .
SCIENCE OF THE TOTAL ENVIRONMENT, 2005, 345 (1-3) :127-140
[9]   Application of DRASTIC and extension theory in the groundwater vulnerability evaluation [J].
Bai, Liping ;
Wang, Yeyao ;
Meng, Fansheng .
WATER AND ENVIRONMENT JOURNAL, 2012, 26 (03) :381-391
[10]   Adverse effect of waterlogging and soil salinity on crop and land productivity in northwest region of Haryana, India [J].
Datta, KK ;
de Jong, C .
AGRICULTURAL WATER MANAGEMENT, 2002, 57 (03) :223-238