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Assessing the effects of the Three Gorges Dam and upstream inflow change on the downstream flow regime during different operation periods of the dam

机译:评估三峡大坝和上游入水量变化对大坝不同运营时期下游流态的影响

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As the largest hydroelectric dam in the world, the Three Gorges Dam (TGD) has raised wide concerns over the environmental and ecological impacts since its dramatic effect on the downstream flow regime of the Yangtze River. Since 2003, the TGD has progressed from the initial operation period to the full operation period, with different effects on the downstream flow regime over each period. Although the upstream inflow change (USIC) of the TGD is a possibly additional factor affecting the downstream flow regime, this has drawn little attention. This study aims to quantify the individual contributions of the TGD and the USIC to the changes of the downstream flow regime over different operation periods of the dam. Using the Muskingum routing model and the Xin'anjiang rainfall-run-off model, we reconstruct the discharge unregulated by the TGD for the post-TGD period from 2003 to 2015. On this basis, the effects of the TGD and the USIC on the downstream flow regime are quantitatively assessed. Benchmarked against the flow regime during the pre-TGD period from 1955 to 2002, it is found that the TGD and the USIC play considerable and comparable roles in affecting the downstream flow regime during the whole post-TGD period from 2003 to 2015. Furthermore, the TGD appears to have a limited effect on the downstream flow regime during the initial operation period from 2003 to 2008 relative to the USIC. In contrast, during the full operation period from 2009 to 2015, the TGD plays a dominant role in changing the downstream flow regime, although the effect of the USIC cannot be neglected. The findings of this study are helpful to understand the exact impacts of the TGD on the downstream flow regime, thereby facilitating the development of a rational strategy for operating the dam.
机译:作为世界上最大的水力发电大坝,三峡大坝(TGD)自从对长江下游水流态势产生巨大影响以来,已经引起了对环境和生态影响的广泛关注。自2003年以来,TGD已从初始运营期发展到整个运营期,每个时期对下游流量的影响都不同。尽管TGD的上游入流变化(USIC)是影响下游流动状态的可能附加因素,但这很少引起注意。本研究旨在量化TGD和USIC对大坝不同运营时期下游水流态变化的贡献。利用马斯金格峰路线模型和新安江降雨径流模型,我们重建了TGD后2003年至2015年不受TGD约束的排放量。在此基础上,TGD和USIC的影响下游流域进行了定量评估。以1955年至2002年TGD之前的流动状态为基准,发现TGD和USIC在2003到2015年整个TGD后的整个期间对下游流动状态产生了相当大的可比作用。此外,与USIC相比,TGD在2003年至2008年的初始运营期间似乎对下游流量状态的影响有限。相比之下,尽管USIC的影响不可忽略,但在2009年至2015年的整个运营期间,TGD在改变下游流量状态方面起着主导作用。这项研究的结果有助于理解TGD对下游水流态势的确切影响,从而有助于制定合理的大坝运行策略。

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