Remote Sensing and GIS Based Groundwater Potential & Recharge Zones Mapping Using Multi-Criteria Decision Making Technique
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  • 作者:Rajat Agarwal ; P. K. Garg
  • 关键词:RS ; GIS ; AHP ; GWPZ ; GWRZ ; MCDM
  • 刊名:Water Resources Management
  • 出版年:2016
  • 出版时间:January 2016
  • 年:2016
  • 卷:30
  • 期:1
  • 页码:243-260
  • 全文大小:3,236 KB
  • 参考文献:Agarwal E, Agarwal R, Garg RD, Garg PK (2013a) Delineation of groundwater potential zone. An AHP/ANP approach Journal of Earth System Science 122(3):887–898CrossRef
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  • 作者单位:Rajat Agarwal (1)
    P. K. Garg (2)

    1. Geomatics Engineering Group, Department of Civil Engineering, Indian Institute of Technology (IIT), Roorkee, 247667, India
    2. Uttarakhand Technical University, Dehradun, India
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Hydrogeology
    Geotechnical Engineering
    Meteorology and Climatology
    Civil Engineering
    Environment
  • 出版者:Springer Netherlands
  • ISSN:1573-1650
文摘
Remote Sensing (RS) and Geographical Information System (GIS) play a crucial role to understand the division of groundwater, an important resource of water supply all over the world. In this present study, groundwater potential and recharge zone maps, are delineated for Loni and Morahi watersheds, Unnao and Rae Bareli district, Uttar Pradesh, India using RS, GIS and Multi-Criteria Decision Making (MCDM) techniques. The Satty’s Analytical Hierarchical Process (AHP) is used as a MCDM technique to normalise the weights of various thematic layers and their classes for delineating the groundwater potential and recharge zone maps. Thematic layers were integrated using weighted overlay in a GIS environment to generate groundwater potential and recharge zone maps. The output potential map is further classified into five zones on the basis of their histograms, viz., ‘very poor’, ‘poor’, ‘good’, ‘very good’ and ‘excellent’. The area falling in the excellent zone is about 150.93 km2 (7.06 % of the total study area), which covers a major portion of the Ganga river. It discriminates the areas where the terrain is suitable for groundwater storage. However, the area falling in the very poor zone is about 372.03 km2 (17.42 % of the total study area) and covers the Loni river south-eastern portion and some areas in north-eastern sides. Groundwater recharge map is classified into four zones namely; ‘most suitable’, ‘moderately suitable’, ‘poorly suitable’ and ‘not suitable’. Yield data of the 40 pumping wells are used to verify the groundwater potential zone map, and the results were found to be good.

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