Review on Practices and State of the Art Methods on Delineation of Ground Water Potential Using GIS and Remote Sensing

Champak Babu Silwal, D. Pathak
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引用次数: 16

Abstract

Due to global increase in human population, the groundwater has been extensively used to meet the water demand for domestic as well as agricultural purpose. The number of deep and shallow wells has increased exponentially. For these purpose the groundwater potential area has to be delineated so as to delineate the area for intervention for groundwater abstraction. The determination of groundwater potential with the aquifer characteristics is not always possible due to unavailability of secondary data and from financial aspect. The delineation of groundwater potential with the integration of GIS and Remote Sensing (RS) as well as with the aid of geophysical data could be an effective approach. Groundwater delineation in mountainous region uses different hydrogeologic parameters like rainfall, slope, elevation, drainage density, lineament density, lithology/geology, land use/land cover (LULC), soil, etc., whereas in case of alluvial basins, parameters like aquifer material, soil, LULC, water table, specific yield, storage coefficient, transmissivity, etc. are used. The assignment of weight for the factors and rank for their classes are important steps in the Groundwater Potential Mapping (GPM) using GIS overlay. The weights for the different parameters have to be assigned as per their role in groundwater occurrences. Different methods like Analytical Hierarchy Process (AHP), expert’s knowledge, probability weight approach,  bivariate analysis, etc. have been used for assigning weights and ranks and the predicted potential need to be validated. Generally in mountainous aquifer, spring inventory forms the basic data for the verification. In addition, the aquifer characteristics like water table, yield, transmissivity can be used for the validation in flat lands. This method of delineation of groundwater potential is found to be appropriate with acceptable accuracy. Globally, there is increasing trend in the use of GIS and Remote Sensing for the identification of groundwater potential in recent time. Bulletin of Department of Geology, vol. 20-21, 2018, pp: 7-20
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基于GIS和遥感的地下水水势圈定方法研究进展
由于全球人口的增加,地下水已被广泛用于满足生活和农业用水需求。深井和浅井的数量呈指数级增长。为此,必须划定地下水潜力区,从而划定地下水开采干预区。由于无法获得二次数据和从财政方面考虑,确定具有含水层特征的地下水潜力并不总是可能的。利用地理信息系统与遥感相结合,结合地球物理资料进行地下水潜力圈定是一种有效的方法。山区地下水圈定使用不同的水文地质参数,如降雨、坡度、高程、排水密度、线条密度、岩性/地质、土地利用/土地覆盖(LULC)、土壤等,而冲积盆地则使用含水层物质、土壤、LULC、地下水位、比产水量、蓄水系数、透过率等参数。在利用GIS叠加进行地下水潜力制图中,因子权重的确定和类别的排序是重要的步骤。不同参数的权重必须根据它们在地下水中所起的作用来确定。不同的方法,如层次分析法(AHP),专家知识,概率权重法,双变量分析等已被用于分配权重和排名,预测潜力需要验证。一般在山地含水层中,泉水清查是验证的基础资料。此外,地下水位、产量、透过率等含水层特征可用于平地的验证。这种划定地下水潜力的方法被认为是适当的,具有可接受的精度。近年来,在全球范围内,利用地理信息系统和遥感技术对地下水潜力进行识别有越来越多的趋势。地质通报,2018年第20-21卷,pp: 7-20
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