Combination of remote sensing, GIS, AHP techniques and geophysical data to delineate groundwater potential zones in the Shiriya River Basin, South India

• Published in: Geosystems and geoenvironment 2024-11, Vol.3 (4), p.100294, Article 100294
• Main Authors: Vidya, K.M., Manoharan, A.N., Suchitra, B., Shyni, M.
• Format: Article
• Language: English
• Subjects: AHP; Geophysical survey; Groundwater potential; Shiriya River Basin; Weighted overlay analysis
• ISSN: 2772-8838; 2772-8838
• DOI: 10.1016/j.geogeo.2024.100294

•Groundwater potential map using analytical hierarchy process.•Pairwise comparison matrix assigned weights to thematic layers.•Groundwater potential zones of Shiriya River Basin classified into three.•Validated the map using groundwater level and vertical electrical sounding data. Shiriya River Basin (SRB) of Kasaragod district, Kerala, is one of the minor river basins that faces acute water shortage soon after the rainy season. Increasing the aquifer productivity of the SRB is the need of the hour. The present study is performed to determine the groundwater potential zones (GWPZ) of the SRB through Weighted Overlay Analysis. Different thematic layers (Geomorphology, Geology, Lineament density, Slope, Drainage density, LULC, and Soil) were prepared. Based on Saaty's scale, the rank and weightage assigned to each thematic layer and their respective features were standardized through the AHP techniques. Subsequently, GIS-based Weighted Overlay Analysis generated the ultimate GWPZ map, dividing SRB into 3 potential zones (poor, moderate, and good). To validate the GWPZ and understand the geoelectric characteristics of the SRB, 50 Schlumberger VES were performed and analyzed. Depth to water level data is also used to validate the GWPZ. The VES data indicated three distinct geoelectric layers, the topsoil, laterite, and weathered/fractured basement, overlying the resistive basement. In the SRB second layer (laterite) and, in some regions, the third layer (fractured charnockite) functions as an aquifer. The presence of groundwater potential region is indicated by resistivity values ranging from 50 to 200 ohm-m. The combination of surface and subsurface indicators of GWPZ will be much more reliable in locating the site for sustainable groundwater exploration and management of SRB groundwater resources. [Display omitted]