滇中引水输水干渠与充蓄水库水温影响研究

Study on the Effects of Water Temperature on the Main Canal and the Reservoirs of the Dianzhong Water Diversion Project

  • 摘要: 采用类比实测法对输水隧洞沿程水温变化进行分析,采用CE-QUAL-W2模型研究了最大充蓄水库九龙甸水库的水温垂向分布特征,得出以下结论:隧洞输水水温沿程增温率为-0.055℃/100km,据此计算出滇中引水输水干渠全段温降为0.4℃;滇中引水充蓄后,九龙甸水库为季节性水温分层型水库,其中3—8月出现水温分层,表层和底层最大温差为5月的5.2℃。受石鼓水源来流低温以及水温分层影响,平水年2—6月水库下泄水温比天然水温低,降低0.3~2.7℃;充蓄后水库下泄水温,较充蓄前最大偏低0.8℃,可见滇中引水充蓄对九龙甸水库的下泄水温影响不大;灌区水稻分蘖期和生长期的灌溉水温均在水稻正常水温承受范围内。

     

    Abstract: The water diversion project in Central Yunnan mainly transports water through tunnels and recharges 16 reservoirs along the line. In this paper,the water temperature variation along the water conveyance tunnel was analyzed by the method of analog measurement and the CE-QUAL-W2 model to study the vertical distribution characteristics of water temperature in Jiulongdian Reservoir. The main conclusions were as follows: the increase rate of water temperature along the tunnel was-0. 055℃/100 km,and the temperature drop of the whole section of the water conveyance main canal was calculated to be 0. 4℃ after water diversion and storage in Central Yunnan. Jiulongdian Reservoir is a seasonal water temperature stratification reservoir,in which the water temperature stratification occurs from March to August,and the maximum temperature difference between the surface layer and the bottom layer is 5. 2℃ in May. Due to the effects of low temperature and stratification of water temperature from theShigu water source,the discharge water temperature of reservoir is lower than that of natural water temperature from February to June in normal year,which decreases by 0. 3 ~ 2. 7℃ . The maximum water temperature of the reservoir is0. 8℃ lower than before. It could be seen that the water diversion and storage in Central Yunnan has little effect on the discharge water temperature of Jiulongdian Reservoir. The irrigation water temperature in the tillering and growing stages of rice in the irrigation area is within the normal water temperature range of rice growing.

     

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