Groundwater vulnerability mapping using the modified DRASTIC model: the metaheuristic algorithm approach

2021 ◽  
Vol 193 (1) ◽  
Author(s):  
Balaji L ◽  
Saravanan R ◽  
Saravanan K ◽  
Sreemanthrarupini N.A
Keyword(s):  
Groundwater Vulnerability ◽  
Vulnerability Mapping ◽  
Metaheuristic Algorithm ◽  
Drastic Model ◽  
Groundwater Vulnerability Mapping ◽  
Modified Drastic

Groundwater Vulnerability Mapping in Urbanized Hydrological System Using Modified Drastic Model and Sensitivity Analysis

2018 ◽  
Vol 24 (3) ◽  
pp. 293-304 ◽  
Author(s):  
Ismail Chenini ◽  
Adel Zghibi ◽  
Mohamed Haythem Msaddek ◽  
Mahmoud Dlala
Keyword(s):  
Land Use ◽  
Vadose Zone ◽  
Vulnerability Assessment ◽  
Groundwater Vulnerability ◽  
Vulnerability Index ◽  
Drastic Model ◽  
Groundwater Vulnerability Mapping ◽  
Groundwater Vulnerability Assessment ◽  
Modified Drastic ◽  
The Impact

Abstract The groundwater vulnerability assessment is normally applied to rural watersheds. However, urbanization modifies the hydrogeological processes. A modified DRASTIC model was adopted to establish a groundwater vulnerability map in an urbanized watershed. The modified DRASTIC model incorporated a land-use map, and net recharge was calculated taking into account the specificity of the urban hydrogeological system. The application of the proposed approach to the Mannouba watershed demonstrates that the groundwater vulnerability indexes range from 80 to 165. The study's results shows that 30 percent of the Mannouba watershed area has a high vulnerability index, 45 percent of the area has a medium index, and 25 percent of the study area has a low vulnerability index. To specify the effect of each DRASTIC factor on the calculated vulnerability index, sensitivity analyses were performed. Land use, topography, and soil media have an important theoretical weight greater than the effective weight. The impact of the vadose zone factor has the most important effective weight and affects the vulnerability index. The sensitivity assessment explored the variation in vulnerability after thematic layer removal. In this analysis, the removal of hydraulic conductivity and impact of vadose zone modified the vulnerability index. Groundwater vulnerability assessment in urbanized watersheds is difficult and has to consider the impact of urbanization in the hydrogeological parameters.

scholarly journals GROUNDWATER VULNERABILITY MAPPING IN MYSORE CITY USING GIS AND DRASTIC MODEL

2014 ◽  
Author(s):  
Lathamani. R Suresha. S B. Mahalingam Lathamani. R Suresha. S B. Mahalingam ◽  
Keyword(s):  
Groundwater Vulnerability ◽  
Vulnerability Mapping ◽  
Drastic Model ◽  
Groundwater Vulnerability Mapping

scholarly journals GROUNDWATER VULNERABILITY MAPPING USING A MODIFIED-DRASTIC MODEL IN AJABSHIR PLAIN, SOUTHEAST COAST OF URMIA LAKE, IRAN

2019 ◽  
Vol XLII-4/W18 ◽  
pp. 789-792
Author(s):  
M. Nakhostinrouhi ◽  
M. H. Rezaei Moghaddam
Keyword(s):  
Land Use ◽  
Water Cycle ◽  
Groundwater Resources ◽  
Groundwater Vulnerability ◽  
Urmia Lake ◽  
Drastic Model ◽  
Hydrogeological Parameters ◽  
Groundwater Vulnerability Mapping ◽  
Modified Drastic ◽  
East Azerbaijan

Abstract. Groundwater resources play an important role not only in providing drinking water but also in irrigation, industry and power generation. In general, groundwater is a part of the water cycle in nature that can be collected by wells, qanats, drains, or natural springs. In this research, the potential of groundwater vulnerability in Ajabshir plain, located in the Southwest of East Azerbaijan Province and Southeast of the Urmia Lake, Iran, is investigated using 7 hydrogeological parameters as well as land-use criterion. Depth to water map is provided using 26 boreholes. Twenty-seven drilling points are also used in generating aquifer media and impact of vadose zone maps. After providing and ranking all layers, they are multiplied by appropriate weights and overlaid to produce vulnerability map. Modified-DRASTIC model is applied to achieve the aim. According to the results, an approximately large part of the aquifer (29 percent), mostly located in the west of the plain, is covered with moderate vulnerability class. Spearman correlation coefficient is calculated 0.63 between the vulnerability and land use maps.

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