长江流域资源与环境 >> 2021, Vol. 30 >> Issue (4): 946-955.doi: 10.11870/cjlyzyyhj202104017

• 生态环境 • 上一篇    下一篇

江家口水库修建对下游河道水温情势影响分析

杨世伟1,李克锋1,张鹏1,梁瑞峰1* ,王远铭1   

  1. (1. 四川大学水力学与山区河流开发保护国家重点实验室,四川 成都 610065)
  • 出版日期:2021-04-20 发布日期:2021-05-17

Impacts of Jiangjiakou Reservoir on Water Temperature Regime#br#  of Downstream River Channel

YANG Shiwei 1, LI Kefeng 1, ZHANG Peng 1, LIANG Ruifeng 1, WANG Yuanming 1   

  1. (1. State Key Laboratory of Hydraulics & Mountain River Engineering, Sichuan University, Chengdu 610065, China)
  • Online:2021-04-20 Published:2021-05-17

摘要: 研究水库修建对于下泄河道水温的影响,掌控水库、下泄水温以及河道水温的变化规律,对于工程的生态环境修复以及河道生物多样性具有重要意义。采用宽度平均的立面二维水温模型对江家口水库库区水温分布及下泄水温规律进行模拟,采用纵向一维水温模型对不同水平年坝下河道的水温进行数值模拟,重点研究坝下23.6 km处鱼类国家级水产种质资源保护区内水温情势的变化。结果表明,库区水温出现明显的分层状况,导致下泄水温在河道中表现为显著的“滞冷”“滞热”现象,春夏降幅最高可达3.6℃,秋冬升幅最高可达4.1℃。通过纵向一维水温模型考虑有无支流汇入的影响下,计算了沿程水温的变化,发现由于流水河段支流汇入和太阳辐射等影响下,沿程河道水温得到有效缓解,保护区处的水温已然接近天然水温,并未显著改变保护区原有鱼类所需的水温环境,不会对保护区鱼类的正常生长繁殖产生不利影响。

Abstract: It is very important to study the influence of reservoir construction on the water temperature of the river channel and to know the changing rules of the water temperature of the reservoir, the temperature of the released water and the water temperature of the river channel. They are of great significance to the restoration of ecological environment and the biodiversity of river channel.In this paper, the laterally-averaged 2D reservoir water temperature model is used to simulate the water temperature distribution and the discharge temperature of Jiangjiakou reservoir, and the one-dimensional longitudinal temperature model is used to simulate the water temperature of downstream river waters at different years, and we focus on the research on the change of the water temperature situation in the National Aquatic germplasm resources reserve of fish at 23.6 km below the dam. The results showed that the water temperature in the reservoir is obviously stratified, resulting in the significant phenomenon of "cold-temperature stagnation" and " heated-temperature stagnation " in the river. The drop in spring and summer can be up to 3.6℃, and the increase in autumn and winter can be up to 4.1℃. By means of the one-dimensional longitudinal temperature model which is used to simulate changes in water temperature along the river with or without the influence of tributary inflow, we found that due to the water river tributary import and solar radiation influence, the water temperature along the river has effectively alleviated. The reserve 's water temperature is close to the natural water temperature, and it did not change the reserve's the original water temperature environment of fish. It will not adversely affect the normal growth and reproduction of fish in the reserve.

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