摘要
根据博斯腾湖1956-2008年实测水位、入湖水量资料,分析了入湖水量与博斯腾湖水位变化关系,采用相关方法计算了博斯腾湖汛期设计入湖水量,并指出博斯腾湖水位的变化主要影响因素为汛期入湖水量,并不是短历时场次洪水,以此为计算基础,得出结论:博斯腾湖最大输水能力下,100年一遇洪水位为1048.6 m,50年一遇洪水位1 048.47 m,可为博斯腾湖水量调度、东、西泵站等输水工程的运行管理提供一定的参考价值。
According to the measured water level and water input data of the Bosten Lake from 1956 to 2008, this paper analyzed the relationship between the water input and the change of water level in Bo- sten Lake, calculated the design water input in flood season of Bosten Lake by using correlative method. It pointed that main influence factors of changing water level of Bosten Lake is the water flowing into the lake in flood season, not the flood of short duration event. On the basis of calculation, it got the conclu- sion that in Bosten Lake, the flood level one in 100 years under the maximum water capacity is 1048.6 m,that of one in 50 years is 1048.47m. The result can provide some reference value for water al- location , operation and management of delivery project of east, west pumping station at Bosten Lake.
出处
《水资源与水工程学报》
2013年第4期199-202,共4页
Journal of Water Resources and Water Engineering
关键词
湖水位
汛期入湖水量
博斯腾湖
开都河
lake water level
water input lake in flood season
Bosten Lake
Kaidu River
