School of Economics and Center for Industrial Information and Economy, Hefei University of Technology, Hefei, Anhui 230601, PR China.
School of Economics, Hefei University of Technology, Hefei, Anhui 230601, PR China.
Sci Total Environ. 2022 Oct 15;843:156906. doi: 10.1016/j.scitotenv.2022.156906. Epub 2022 Jun 23.
Water footprints and virtual water are widely used as essential tools for water use and conservation analysis of basins worldwide. Despite the importance of water-rich basins as the main force for water-saving, water use analysis has been mainly for water-scarce basins rather than water-rich basins in the existing literature. To fill the gap, in this paper, we investigate the water footprint and virtual water trade in a water-rich basin, namely the Chaohu Lake Basin in China, from 2007 to 2017 using input-output analysis. The results show that: (1) Water use efficiency in the Chaohu Lake Basin was significantly improved. The overall trend of the water intensity was declining, decreasing by 10.21 % in 2017 versus 2012; (2) The internal and external water footprints showed an upward trend, and the growth rate of total water footprint was 36.66 %; (3) The basin was a net virtual water exporter, but the net export flows of virtual water has decreased significantly. The virtual water net export flow decreased by 0.12 billion m in 2017 versus 2012; (4) Water resources in the basin were mainly used locally, and its supply to other provinces was minimal. Compared with some water-scarce basins such as the Heihe River Basin and Haihe River Basin, the Chaohu Lake Basin shows significant gaps in the virtual water export flow per capita and behaves differently in the proportion of virtual water transfer. Based on the above findings, we conclude with some guidance and implications for local governments and policymakers.
水资源足迹和虚拟水广泛用作全球流域用水和保护分析的重要工具。尽管富水流域作为节水的主要力量非常重要,但在现有文献中,用水分析主要针对缺水流域,而不是富水流域。为了填补这一空白,本文采用投入产出分析方法,研究了一个富水流域,即中国的巢湖流域,2007 年至 2017 年的水资源足迹和虚拟水贸易。结果表明:(1)巢湖流域用水效率显著提高。水强度整体呈下降趋势,2017 年比 2012 年下降 10.21%;(2)内部和外部水资源足迹呈上升趋势,总水资源足迹增长率为 36.66%;(3)流域是净虚拟水出口区,但虚拟水净出口流量显著减少。2017 年比 2012 年,虚拟水净出口流量减少了 0.12 亿立方米;(4)流域水资源主要在当地使用,对其他省份的供应很少。与一些缺水流域,如黑河流域和海河流域相比,巢湖流域的人均虚拟水出口流量差距显著,虚拟水转移比例的表现也不同。基于上述发现,我们为地方政府和决策者提供了一些指导和启示。