利用遥感、地理信息系统和模糊-AHP 方法划分印度南部 Ponnai 子盆地的地下水潜力区

Water Supply Pub Date : 2024-04-22 DOI:10.2166/ws.2024.084
Sankar Loganathan, Mahenthiran S.
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引用次数: 0

摘要

地下水是满足家庭、灌溉和工业需求的重要水源。由于城市化和工业化,地下水的数量和质量正在迅速下降。应妥善处理硬岩地区的地下水资源,最大限度地提高其利用率。这项工作旨在通过结合遥感(RS)、地理信息系统(GIS)和模糊分析层次过程(FAHP),在帕拉尔河流域(Ponnai 子流域)的一部分划定地下水潜力区(GWPZ)。在绘制 GWPZ 地图时,考虑了地质、土地利用/土地覆被 (LULC)、地貌、坡度、土壤、降雨、线状密度 (LD)、排水密度 (DD)、归一化植被指数 (NDVI)、地形湿润指数 (TWI) 和地形位置指数 (TPI) 等影响地下水的因素。根据 FAHP 技术对这些参数进行了权重分配,得到的地下水潜势图被划分为:极差(13.5%)、差(21.76%)、中等(31.5%)、好(20.66%)和非常好(8.54%)。GWPZ 图与 Ponnai 子流域的实际水井产量进行了验证。这项研究工作将为有效利用地下水和长期可持续管理 Ponnai 子流域含水层提供指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Demarcation of groundwater potential zones in Ponnai sub-basin, Southern India using remote sensing, GIS and fuzzy-AHP approaches
Groundwater is an essential source for household, irrigation and industry needs. The amount of groundwater and its quality are rapidly declining because of urbanization and industrialization. Groundwater resources in hard rock regions should be handled properly to maximize their utilization. This work aims to demarcate the Groundwater Potential Zones (GWPZ) in a part of the Palar River Basin (Ponnai sub-basin) by combining Remote Sensing (RS), Geographic Information System (GIS) and Fuzzy-Analytical Hierarchy Process (FAHP). The factors which influence the groundwater like geology, Land use/land cover (LULC), geomorphology, slope, soil, rainfall, Lineament Density (LD), Drainage density (DD), Normalized Difference Vegetation Index (NDVI), Topographic Wetness Index (TWI) and Topographic Position Index (TPI) are considered for mapping of GWPZ. The weightage is allocated to these parameters on the basis of the FAHP technique and the obtained groundwater potential map was classified as, very poor (13.5%), poor (21.76%), moderate (31.5%), good (20.66%) and very good (8.54%). The GWPZ map was validated with the actual well yield of the Ponnai sub-basin. The research work will serve as a guideline for the effective use of groundwater and long-term sustainable management of the aquifer in the Ponnai sub-basin.
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