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Integrated geospatial, geostatistical, and remote-sensing approach to estimate groundwater level in North-western India

机译:综合的地理空间,地统计学和遥感方法来估算印度西北部的地下水位

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The depletion of groundwater resources in Northwest India has been extensively studied. The top priority to meet the scarcity of water for irrigation, industrial and domestic purposes is supplemented by groundwater. Geostatistical modelling approach is considered to be beneficial tool for the assessment, evaluation, monitoring, and management of groundwater resources. This study is an attempt to analyze the spatio-temporal variability of groundwater level in semi-arid region of Panipat district, Haryana, India using kriging technique to fill the data gaps. Ordinary kriging was found optimal for the interpolation of groundwater levels. The results revealed that there was not much seasonal variation and also the groundwater flow direction remained almost constant in the study area during the assessment period. Spatial variability analysis showed significant variation in groundwater level and further depicted that the study area had undergone more or less decline in groundwater over the period of time. To validate the observations and results geo spatial and remote sensing techniques including normalised difference vegetation index and impervious surface relationships were worked out. It was further co-related with the rainfall data and the canal network existing in Panipat region. The integrated approach substantiated the observed results with the ground reality and helped in better understanding of the causes of declining groundwater trend in central part of Panipat.
机译:印度西北部的地下水资源枯竭已得到广泛研究。满足灌溉,工业和家庭用水短缺的首要任务是补充地下水。地统计建模方法被认为是评估,评估,监测和管理地下水资源的有益工具。这项研究是尝试使用克里金法填补数据空白,分析印度哈里亚纳邦帕尼帕特地区半干旱地区地下水位的时空变化。发现普通克里格法最适合于地下水位的插值。结果表明,在评估期内,研究区域的季节变化不大,地下水流向几乎保持恒定。空间变异性分析显示了地下水位的显着变化,并进一步描述了该研究区域在一段时间内的地下水下降或多或少。为了验证观测结果,设计了包括归一化植被指数和不透水表面关系在内的地理空间和遥感技术。它与Panipat地区现有的降雨数据和运河网络进一步相关。该综合方法以地面实际情况证实了所观察到的结果,有助于更好地了解帕尼帕特中部地下水趋势下降的原因。

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