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首页> 外文期刊>Arabian journal of geosciences >Identification of potential groundwater recharge zones in Vaigai upper basin, Tamil Nadu, using GIS-based analytical hierarchical process (AHP) technique
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Identification of potential groundwater recharge zones in Vaigai upper basin, Tamil Nadu, using GIS-based analytical hierarchical process (AHP) technique

机译:使用基于GIS的层次分析法(AHP)识别泰米尔纳德邦Vaigai上盆地的潜在地下水补给区

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摘要

Groundwater recharge is an important process for the management of both surface and subsurface water resources. The present study utilizes the application of analytical hierarchical process (AHP) on geospatial analysis for the exploration of potential zones for artificial groundwater recharge along Vaigai upper basin in the Theni district, Tamil Nadu, India. The morphology of earth surface features such as geology, geomorphology, soil types, land use and land cover, drainage, lineament, and aquifers influence the groundwater recharge in either direct or indirect way. These thematic layers are extracted from Landsat ETM+ image, topographical map, and other collateral data sources. In this study, the multilayers were weighed accordingly to the magnitude of groundwater recharge potential. The AHP technique is a pair-wise matrix analytical method was used to calculate the geometric mean and normalized weight of individual parameters. Further, the normalized weighted layers are mathematically overlaid for preparation of groundwater recharge potential zone map. The results revealed that 21.8 km~2 of the total area are identified as high potential for groundwater recharge. The gentle slope areas in middle-east and central part have been moderately potential for groundwater recharge. Hilly terrains in south are considered as unsuitable zone for groundwater recharge processes.
机译:补给地下水是管理地表和地下水资源的重要过程。本研究利用分析层次分析法(AHP)在地理空间分析中的应用,探索了印度泰米尔纳德邦Theni区Vaigai上盆地潜在的人工地下水补给区。诸如地质,地貌,土壤类型,土地利用和土地覆盖,排水,地貌和含水层等地表特征的形态直接或间接地影响着地下水的补给。这些主题图层是从Landsat ETM +图像,地形图和其他附带数据源中提取的。在这项研究中,根据地下水补给潜力的大小对多层进行称重。 AHP技术是一种成对矩阵分析方法,用于计算各个参数的几何平均值和归一化权重。此外,归一化的加权层在数学上被叠加以准备地下水补给潜力区图。结果表明,总面积的21.8 km〜2被确定为具有较高的地下水补给潜力。中东和中部的缓坡地区有适度的地下水补给潜力。南部的丘陵地形被认为是不适合进行地下水补给过程的区域。

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