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首页> 外文期刊>Environmental earth sciences >Delineation of groundwater potential zones using GIS and multi influence factor (MIF) techniques: a study of district Swat, Khyber Pakhtunkhwa, Pakistan
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Delineation of groundwater potential zones using GIS and multi influence factor (MIF) techniques: a study of district Swat, Khyber Pakhtunkhwa, Pakistan

机译:利用GIS和多影响因子(MIF)技术描绘地下水潜在区域:巴基斯坦开伯尔-普赫图赫瓦省斯瓦特地区的研究

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摘要

The efficient groundwater utilization, planning and management, is inconceivable without the proper recognition of potential zones. The present study aimed to assess the groundwater potentiality in district Swat, Khyber Pakhtunkhwa Province, Pakistan. The weighted overlay analysis methodology is used in this paper. A total of seven influence factors were used in the present study, viz. slope, drainage density, geology, rainfall, soil, land use/land cover and lineament density. The weight and score of each influencing factor is computed using multi influence factor (MIF) techniques. Within each influencing factor the subclasses were assigned a weightage of (A) (major effect) and (B) (minor effect) depending upon their effectiveness to the recharge of aquifers and groundwater potentiality. The combined weightage of both major and minor effects (A + B) was considered for computing the relative effect which was used to compute the score of each subclass within each influencing factor. The thematic layers were then integrated with weighted overlay using ArcGIS 10.2.1 and groundwater potential zone were delineated. The delineated groundwater potential zones were classified into four categories, i.e., (1) poor, (2) good, (3) high and (4) very high potentiality. The findings revealed that very high groundwater potential zone cover an area of 342.57 km(2) (6.7%), high 1506 km(2) (29%), good 2384.8 km(2) (45.91%) and poor 960.28 km(2) (18.48% of total area). The results of this paper are believed to be useful for effective groundwater harvesting and management and can also be used as helping material for future research work.
机译:如果没有正确识别潜在的区域,那么有效的地下水利用,规划和管理是不可想象的。本研究旨在评估巴基斯坦开伯尔-普赫图赫瓦省斯瓦特地区的地下水潜力。本文采用加权叠加分析方法。本研究共使用了七个影响因素,即。坡度,排水密度,地质,降雨,土壤,土地利用/土地覆盖率和线粒体密度。使用多影响因子(MIF)技术计算每个影响因子的权重和分数。在每个影响因素中,根据子类对含水层补给的有效性和地下水潜力,将其分配为(A)(主要影响)和(B)(次要影响)权重。考虑主要效果和次要效果(A + B)的组合权重,以计算相对效果,该相对效果用于计算每个影响因素中每个子类的得分。然后使用ArcGIS 10.2.1将主题图层与加权叠加层集成在一起,并划定地下水潜在区域。划定的地下水潜在地带分为四类,即(1)较差,(2)良好,(3)高和(4)极高的潜力。调查结果表明,极高的地下水潜在区覆盖面积342.57 km(2)(6.7%),高1506 km(2)(29%),良好2384.8 km(2)(45.91%)和较差的960.28 km(2) )(占总面积的18.48%)。相信本文的结果对于有效的地下水收集和管理是有用的,也可以用作将来研究工作的帮助材料。

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