首页> 外文期刊>Indian Journal of Ecology >Spatial Analysis of Groundwater Fluctuation in Nathusari Chopta Block of Sirsa District (Haryana, India) using Geospatial Technology
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Spatial Analysis of Groundwater Fluctuation in Nathusari Chopta Block of Sirsa District (Haryana, India) using Geospatial Technology

机译:利用地理空间技术,南萨拉区(印度哈里亚纳邦哈里亚纳纳邦)地下水波动的空间分析

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摘要

The present research demonstrates the spatial-temporal changing in the groundwater leveLof the study area i.e., Nathusari Chopta block of Sirsa district. The 15 locations of dug-wells were taken to observe the ground water level of pre-monsoon and monsoon season for two decades (1996-2018). The fluctuations in the groundwater level during two decades in the area were also analysed. The interpolation technique of geospatial technology was used to analyse and mapping of the ground water level and its fluctuation. The groundwater level of two decades showed a range from 1.28 meter below ground level to 29.4 m (bgl) over the locations. The ground water fluctuation of the area had upwelling trained as result showed that upto 6 meter water table rose during the period. The study showed uprising trend in average groundwater level from 12.37 m bgl in 1996 to 7.56 m bgl in year 2018. The changes in the groundwater level were more prominent in centre, North-east and West as rising trends in the area. The probable reason for this trend may be the poor groundwater quality in western and northeastern parts of the area hampering the farmers from its use. The central part of area is most affected by water table rising problem and most of the area suffers from Waterlogging and soil salinity. The major aim of the study was to find out the spatial and temporal changes in the seasonal groundwater level and its fluctuations.
机译:本研究表明,Sirsa区的Nathusari Chopta Block of Sirsa区的地下水等级中的空间变化。挖掘井的15个地点被认为观察季风和季风季节的地下水位二十年(1996-2018)。还分析了该地区二十年的地下水位水平的波动。地理空间技术的插值技术用于分析和绘制地下水位及其波动。地下水位二十年的地面显示在地上1.28米以下的范围为29.4米(BGL)。该地区的地下水波动已升高,因为结果显示,在此期间高达6米的水位桌。该研究表明,2016年1996年的12.37米BGL的平均地下水位的起义趋势从12.37米BGL到7.56米BG1。地下水位的变化在中心,东北和西部更加突出,是该地区的上升趋势。这种趋势的可能原因可能是西部和东北部门的地下水质量差,阻碍了农民的使用。地区的中心部分受水工作台上升的影响最大,而且大部分地区患有涝盐和土壤盐度。该研究的主要目的是找出季节性地下水位的空间和时间变化及其波动。

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