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Assessment of recharge potential zones for groundwater development and management using geospatial and MCDA technologies in semiarid region of Western India

机译:使用地理空间和MCDA技术评估印度西部半干旱地区的地下水开发和管理补给潜力区

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Groundwater recharge potential (GWRP) plays a vital role as it directly or indirectly supports domestic, agriculture andindustrial activities by infiltrating the rainwater. The present paper touches upon the methodology delineating groundwaterrecharge potential zones by applying geospatial and multi-criteria decision analysis (MCDA) to the derived thematiclayers based on significant influence of occurrence of groundwater in semiarid watershed of Western India. The satelliteimageries and other ancillary data were utilized to generate various thematic layers, viz. slope, geology, drainage density,surface run off, geomorphology, land use/land cover soil and vadose zone. The outcome of study shows that about24.69% is having high GWRP and 24.17% of the area is moderate for recharge of groundwater, while the low and poorgroundwater recharges potential area is about 44.34% and 6.80% of total area, respectively. The validation of the studywas done by overlaying point data groundwater well yield on the output final map; it shows good correlation with result.Also, the surplus water availability was calculated based on vadose calculation according to CGWB method; it shows17.12 MCM vadose region having artificial recharge of 22.77 MCM. The total recharge is about 117.41 MCM, about 30%of the total runoff, i.e. 35.22 MCM is considered as surplus monsoon runoff available for artificial recharge. The resultshows that the use of remote sensing, geospatial and MCDA technologies are promising and efficiently recognize thesuitable regions for groundwater recharge over other conventional techniques.
机译:地下水补给潜力(GWRP)发挥着至关重要的作用,因为它直接或间接地支持了家庭,农业和通过渗透雨水进行工业活动。本文涉及描述地下水的方法学通过将地理空间和多标准决策分析(MCDA)应用于派生的主题,对潜在区域进行补给基于印度西部半干旱流域地下水发生的重大影响而形成的水层。卫星利用图像和其他辅助数据来生成各种主题层。坡度,地质,排水密度,地表径流,地貌,土地利用/土地覆盖土壤和渗流带。研究结果表明GWRP高的地区为24.69%,地下水补给的地区为24.17%,低而差的地区地下水补给潜力面积分别约为总面积的44.34%和6.80%。研究的验证通过在输出的最终地图上叠加点数据地下水井产量来完成;它与结果显示出良好的相关性。另外,根据CGWB方法,在渗流计算的基础上,计算了剩余水的利用率。表明具有人工补给的22.77 MCM的17.12 MCM渗滤区。总充值约为117.41 MCM,约占30%总径流中的35.22 MCM被认为是可供人工补给的季风剩余径流。结果表明遥感,地理空间和MCDA技术的使用是有前途的,并有效地识别了比其他常规技术更适合地下水补给的区域。

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