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地下水足迹揭示的全球含水层水量平衡

Water balance of global aquifers revealed by groundwater footprint.

机构信息

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

出版信息

Nature. 2012 Aug 9;488(7410):197-200. doi: 10.1038/nature11295.

Abstract

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. Most assessments of global water resources have focused on surface water, but unsustainable depletion of groundwater has recently been documented on both regional and global scales. 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 calculations, and be used to assess the potential for increasing agricultural yields with renewable groundwaterref. The method could be modified to evaluate other resources with renewal rates that are slow and spatially heterogeneous, such as fisheries, forestry or soil.

摘要

地下水是一种维持生命的资源,为数以十亿计的人提供水源,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。大多数全球水资源评估都集中在地表水,但最近在区域和全球范围内都记录到地下水的不可持续消耗。目前尚不清楚全球地下水枯竭的速度与自然更新的速度以及支持生态系统所需的供应相比如何。在这里,我们定义了地下水足迹(维持地下水利用和依赖地下水的生态系统服务所需的面积),并表明人类在许多对农业至关重要的大型含水层中过度开采地下水,尤其是在亚洲和北美。我们估计,目前全球地下水足迹的规模约为含水层实际面积的 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,这意味着净全球价值是由少数过度开采的含水层驱动的。地下水足迹是第一个适合在含水层尺度上一致评估地下水利用、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,用于评估利用可再生地下水提高农业产量的潜力。该方法可以修改,以评估其他更新速度缓慢且空间异质性大的资源,如渔业、林业或土壤。

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