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大坝建设对长江下游热条件的影响。

Impact of the Dam Construction on the Downstream Thermal Conditions of the Yangtze River.

机构信息

State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China.

出版信息

Int J Environ Res Public Health. 2020 Apr 24;17(8):2973. doi: 10.3390/ijerph17082973.

Abstract

Water temperature is an important factor in aquatic environments. Dam construction, especially the construction of multiple dams in rivers, can greatly affect the downstream water temperature. Several dams, including Wudongde, Baihetan, Xiluodu, Xiangjiaba, Three Gorges, and Gezhouba, have been constructed between Panzhihua and Yichang along the Yangtze River. The aim of this paper was to quantify the impact of these dams on the water temperature downstream. One-dimensional and two-dimensional models were used to simulate the water temperatures, and the results showed that the dams had different cumulative effects on it. For example, in January, after the construction of the Xiangjiaba and Xiluodu dams, the discharge water temperature of Xiangjiaba was 3 °C higher than the natural conditions, and after the construction of the Baihetan and Wudongde dams was completed, it increased by a further 2 °C. The natural river ran over 416 km with no dams from the Xiangjiaba dam to the Cuntan Station. With the influence of climate and tributary inflow, the impact of upstream dams on the water temperature was mitigated by more than 48% at Cuntan Station, displaying a recovery. It seemed that the cumulative effects of dams on the discharge water temperature of the Three Gorges decreased with the increase in the upstream storage capacity from March to May, and the construction of dams even had a negative effect. From September to February of the next year, the cumulative effects increased with the increase of the upstream storage capacity, but only the total storage capacity until a certain level, where no further impact was observed.

摘要

水温是水生环境的一个重要因素。水坝的建设,特别是在河流中建造多个水坝,会极大地影响下游的水温。在长江攀枝花至宜昌段,已建成了乌东德、白鹤滩、溪洛渡、向家坝、三峡和葛洲坝等几座大坝。本文旨在量化这些大坝对下游水温的影响。使用一维和二维模型来模拟水温,结果表明,大坝对水温有不同的累积影响。例如,在 1 月,向家坝和溪洛渡大坝建成后,向家坝的放水水温比自然条件高 3°C,而在白鹤滩和乌东德大坝建成后,又升高了 2°C。从向家坝大坝到寸滩站,自然河流全长 416 公里,没有大坝。在气候和支流汇入的影响下,在寸滩站,上游大坝对水温的影响降低了 48%以上,呈现出恢复的趋势。似乎随着上游库容的增加,大坝对三峡出库水温的累积效应在 3 月至 5 月期间有所降低,而且大坝的建设甚至产生了负面影响。从次年的 9 月到 2 月,随着上游库容的增加,累积效应增加,但只有在上游总库容达到一定水平时,才不会再产生影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8822/7215317/104ca4af99cf/ijerph-17-02973-g001.jpg

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