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Asymmetric impact of groundwater use on groundwater droughts

机译:地下水对地下水干旱的不对称影响

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Groundwater use affects groundwater storage continuously as the removal of water changes both short-term and long-term groundwater level variation. This has implications for groundwater droughts, i.e. a below-normal groundwater level. The impact of groundwater use on groundwater droughts, however, remains unknown. Hence, the aim of this study is to investigate the impact of groundwater use on groundwater droughts in the absence of actual abstraction data. We present a methodological framework that consists of two approaches. The first approach compared groundwater droughts at monitoring sites that are potentially influenced by abstraction to groundwater droughts at sites that are known to be near natural. Observed groundwater droughts were compared in terms of drought occurrence, duration, and magnitude. The second approach investigated long-term trends in groundwater levels in all monitoring wells. This framework was applied to a case study of the UK, using four regional water management units in which groundwater levels are monitored and abstractions are licensed. Results show two asymmetric responses in groundwater drought characteristics due to groundwater use. The first response is an increase in shorter drought events and is found in three water management units where long-term annual average groundwater abstractions are smaller than recharge. The second response, observed in one water management unit where groundwater abstractions temporarily exceeded recharge, is a lengthening and intensification of groundwater droughts. Analysis of long-term (1984–2014) trends in groundwater levels shows mixed but generally positive trends, while trends in precipitation and potential evapotranspiration are not significant. The overall rising groundwater levels are consistent with changes in water use regulations and with a general reduction in abstractions during the period of investigation. We summarised our results in a conceptual typology that illustrates the asymmetric impact of groundwater use on groundwater drought occurrence, duration, and magnitude. The long-term balance between groundwater abstraction and recharge plays an important role in this asymmetric impact, which highlights the relation between short-term and long-term sustainable groundwater use.
机译:由于拆除水改变短期和长期地下水位变化,地下水用途连续影响地下水储存。这对地下水干旱有影响,即低于正常地下水位。然而,地下水对地下水干旱的影响仍然未知。因此,本研究的目的是在没有实际抽象数据的情况下调查地下水在地下水干旱上的影响。我们提出了一种由两种方法组成的方法框架。第一种方法在监测网站上比较了地下水干旱,这些地点可能受到众所周知的遗址的抽象地下水干旱的影响。在干旱发生,持续时间和幅度方面比较了观察到的地下水干旱。第二种方法调查了所有监测井地下水位的长期趋势。该框架应用于英国的案例研究,使用四个区域水管理单位,其中监测地下水位和抽象许可。结果显示由于地下水采用地下水干旱特性两种不对称反应。第一反应是较短的干旱事件的增加,并在三个水管理单元中发现,长期年平均地下水抽象小于充电。在一个水管理单元中观察到的第二反应,该水管理单元暂时超过充电,是地下水干旱的延长和强化。对地下水位的长期(1984-2014)趋势分析混合但一般阳性趋势,而沉淀和潜在蒸散的趋势并不重要。整体上升的地下水位与水使用规定的变化一致,并在调查期间随意减少抽象。我们总结了我们的结果,在概念性类型中,说明地下水在地下水发生的不对称影响,持续时间和大小。地下水抽象和充值之间的长期平衡在这种不对称的影响中起着重要作用,这突出了短期和长期可持续地下水之间的关系。

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