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

K.M. Vidya , A.N. Manoharan , B. Suchitra , M. Shyni
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Abstract

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.

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结合遥感、地理信息系统、AHP 技术和地球物理数据,划定印度南部 Shiriya 河流域的地下水潜力区
喀拉拉邦卡萨拉戈德县的希里亚河流域(SRB)是小流域之一,雨季过后不久就面临严重缺水问题。提高什里亚河流域含水层的生产力是当务之急。本研究旨在通过加权叠加分析法确定 SRB 的地下水潜力区(GWPZ)。编制了不同的专题图层(地貌、地质、线状密度、坡度、排水密度、土地利用、土地利用变化和土壤)。根据 Saaty 量表,通过 AHP 技术对每个专题图层及其各自特征的等级和权重进行了标准化。随后,基于 GIS 的加权叠加分析生成了最终的 GWPZ 地图,将 SRB 划分为 3 个潜力区(差、中、好)。为验证 GWPZ 并了解 SRB 的地电特征,对 50 个斯伦贝谢 VES 进行了分析。水位深度数据也用于验证 GWPZ。VES 数据显示了三个不同的地电层,即表土层、红土层和风化/断裂基底,覆盖在电阻基底之上。在 SRB 中,第二层(红土)和某些区域的第三层(断裂角闪岩)起着含水层的作用。电阻率值从 50 到 200 欧姆-米不等,表明存在地下水潜势区。结合地表和地下指标对全球水源保护区的定位将更加可靠,以便进行可持续的地下水勘探和 SRB 地下水资源的管理。
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