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Modeling and mapping of groundwater potentiality zones using AHP and GIS technique: a case study of Raniganj Block, Paschim Bardhaman, West Bengal

机译:使用AHP和GIS技术对地下水潜力区进行建模和制图:以西孟加拉邦Paschim Bardhaman的Raniganj Block为例

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摘要

Water is the most significant natural resources stirring both surface water and groundwater for human civilization. This precious resource is occasionally scarce, sometimes plentiful but not uniformly concentrated, both in space and time. Groundwater is most valuable and dynamic resource that is not equally distributed. The dimensions of groundwater in an area are determined by numerous factors such as topography, lithology, geological structure, depth of weathering, slope, drainage pattern, land use and land cover (LULC), rainfall pattern. Delineation of groundwater potentiality zone is an indispensable part for the management of water resources numerous themes are included according to their relative magnitude for the potentiality mapping, these are-geology, slope gradient, LULC, soil texture, rainfall, lineament density, drainage density and groundwater fluctuation etc. The analytical hierarchical process (AHP) method has been used to find out the weights of different themes and their associated sub-themes and finally overlay analysis has been done in the geospatial environment. Groundwater potential zone is categorized as 'very poor' (18.22), 'poor' (28.39), 'moderate' (31.98), 'good' (13.24) and 'excellent' (8.17). The groundwater potential map has been validated with Dug well data for accounting the implication of this model.
机译:水是人类文明最重要的自然资源,搅动着地表水和地下水。这种珍贵的资源有时是稀缺的,有时是丰富的,但在空间和时间上都不是均匀集中的。地下水是最有价值和最有活力的资源,但分布不均。一个地区地下水的大小由许多因素决定,如地形、岩性、地质结构、风化深度、坡度、排水模式、土地利用和土地覆盖(LULC)、降雨模式。地下水潜力带的划定是水资源管理不可或缺的一部分,根据其相对大小,地下水潜力区图包括许多主题,包括地质、坡度、LULC、土壤质地、降雨量、谱线密度、排水密度和地下水波动等。采用层次分析法(AHP)找出不同主题及其相关子主题的权重,最后在地理空间环境中进行叠加分析。地下水潜力区分为“极差”(18.22%)、“差”(28.39%)、“中等”(31.98%)、“良好”(13.24%)和“优”(8.17%)。地下水潜力图已经用挖井数据进行了验证,以说明该模型的含义。

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