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Water balance of global aquifers revealed by groundwater footprint

机译:地下水足迹揭示全球含水层的水平衡

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摘要

Groundwater is a life-sustaining resource that supplies water to billions of people, plays a central part in irrigated agriculture and influences the health of many ecosystems~(1,2). Most assessments of global water resources have focused on surface water3'6, but unsustainable depletion of groundwater has recently been documented on both regional~(7,8) and global scales~(9,11). It remains unclear how the rate of global groundwater depletion compares to the rate of natural renewal and the supply needed to support ecosystems. Here we define the groundwater footprint (the area required to sustain groundwater use and groundwater-dependent ecosystem services) and show that humans are overexploiting groundwater in many large aquifers that are critical to agriculture, especially in Asia and North America. We estimate that the size of the global groundwater footprint is currently about 3.5 times the actual area of aquifers and that about 1.7 billion people live in areas where groundwater resources and/or groundwater-dependent ecosystems are under threat. That said, 80 per cent of aquifers have a groundwater footprint that is less than their area, meaning that the net global value is driven by a few heavily overexploited aquifers. The groundwater footprint is the first tool suitable for consistently evaluating the use, renewal and ecosystem requirements of groundwater at an aquifer scale. It can be combined with the water footprint and virtual water calculations12'14, and be used to assess the potential for increasing agricultural yields with renewable groundwaterref~(15). The method could be modified to evaluate other resources with renewal rates that are slow and spatially heterogeneous, such as fisheries, forestry or soil.
机译:地下水是一种维持生命的资源,可以为数十亿人供水,在灌溉农业中起着核心作用,并影响着许多生态系统的健康[1,2]。对全球水资源的大多数评估都集中在地表水3'6上,但是最近在区域(7,8)和全球范围内(9,11)都记录了地下水的不可持续消耗。尚不清楚全球地下水枯竭率与自然更新率和支持生态系统所需的供给相比。在这里,我们定义了地下水足迹(维持地下水使用和依赖地下水的生态系统服务所需的面积),并表明人类正在对农业至关重要的许多大型含水层中过度开采地下水,特别是在亚洲和北美。我们估计,目前全球地下水足迹约为蓄水层实际面积的3.5倍,约有17亿人生活在地下水资源和/或依赖地下水的生态系统受到威胁的地区。也就是说,80%的含水层的地下水足迹小于其面积,这意味着全球净值是由一些过度开采的含水层驱动的。地下水足迹是第一个适用于持续评估含水层规模的地下水的使用,更新和生态系统需求的工具。它可以与水足迹和虚拟水计算相结合12'14,并用于评估可再生地下水参考文献[15]增加农业产量的潜力。可以修改该方法,以评估更新速度缓慢且空间异质的其他资源,例如渔业,林业或土壤。

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  • 来源
    《Nature》 |2012年第7410期|p.197-200|共4页
  • 作者单位

    Department of Civil Engineering, McGill University, Montreal, Quebec H3A 0C3, Canada;

    Department of Physical Geography, Faculty of Geosciences, Utrecht University, PO Box 80115,3508 TC Utrecht,The Netherlands.;

    Department of Physical Geography, Faculty of Geosciences, Utrecht University, PO Box 80115,3508 TC Utrecht,The Netherlands. ,Deltares, PO Box 85467,3508 AL Utrecht, The Netherlands;

    Department of Physical Geography, Faculty of Geosciences, Utrecht University, PO Box 80115,3508 TC Utrecht,The Netherlands;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-18 02:54:14

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