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

机译:大坝建设对长江下游热工条件的影响

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摘要

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.
机译:水温是水生环境中的重要因素。大坝的建设,特别是河流中多座大坝的建设,会极大地影响下游水温。沿长江沿岸攀枝花和宜昌之间已修建了乌东德,白鹤滩,溪洛渡,向家坝,三峡和葛洲坝等大坝。本文的目的是量化这些大坝对下游水温的影响。用一维和二维模型模拟水温,结果表明大坝对水温的累积影响不同。例如,1月,向家坝和溪洛渡大坝建设完成后,向家坝的排泄水温比自然条件高3°C,白鹤滩和乌洞德大坝建设完成后又进一步上升。 2℃。天然河长达416公里,从向家坝水坝到寸滩站没有水坝。在气候和支流流入的影响下,村滩站上游大坝对水温的影响减轻了48%以上,显示出恢复状态。大坝对三峡排放水温度的累积影响似乎随着3月至5月上游蓄水量的增加而减小,大坝的建设甚至产生了负面影响。从第二年的9月到次年的2月,累积效应随着上游存储容量的增加而增加,但是只有总存储容量才达到一定水平,在此之前没有进一步的影响。

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