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Identifying Major Factors Affecting Groundwater Change in the North China Plain with Grey Relational Analysis

机译:用灰色关联分析法识别影响华北平原地下水变化的主要因素

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The North China Plain (NCP) is facing a water crisis under the dual impact of natural and anthropogenic factors. Groundwater levels have declined continuously since 1960, causing a series of environmental problems that have restricted sustainable development in the region. In the present study, we first utilized a previously developed 3D groundwater model to determine changes in groundwater level in the region over the past 50 years (1961–2010). We then applied grey relational analysis (GRA) to identify and ordinate major factors that have contributed to these changes. The results show an overall decreasing trend in groundwater levels in this region over the past 50 years and an increase in the water table depth at a rate of approximately 0.36 m/a. Groundwater exploitation showed the most significant correlation with the groundwater table decline, when compared with other factors including precipitation and river leakage. Therefore, human activities should be considered the primary force driving the groundwater level down. The results of this study have implications for developing criteria that consider changes in both climate and socio-economics. Furthermore, since the NCP is one of the most water-scarce and densely populated regions in the world, the analytical approach used in and the insights gained from this study are of international interest.
机译:在自然和人为因素的双重影响下,华北平原(NCP)面临着水危机。自1960年以来,地下水位持续下降,造成了一系列环境问题,制约了该地区的可持续发展。在本研究中,我们首先利用先前开发的3D地下水模型来确定过去50年(1961-2010年)该地区地下水位的变化。然后,我们应用了灰色关联分析(GRA)来识别和协调促成这些变化的主要因素。结果表明,在过去的50年中,该地区的地下水位总体呈下降趋势,地下水位深度以约0.36 m / a的速率增加。与其他因素(包括降水和河流泄漏)相比,地下水开采与地下水位下降具有最显着的相关性。因此,应将人类活动视为推动地下水位下降的主要力量。这项研究的结果对制定考虑气候和社会经济变化的标准有影响。此外,由于NCP是世界上水资源最稀缺和人口最稠密的地区之一,因此本研究中使用的分析方法和从中获得的见识具有国际意义。

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