Three-Dimensional CFD Simulations of Start-Up Processes of a Pump-Turbine Considering Governor Regulation

被引:4
|
作者
Yang, Zhiyan [1 ]
Cheng, Yongguang [1 ]
Liu, Ke [1 ]
Hou, Xiaoxia [1 ]
Zhang, Xiaoxi [2 ]
Wang, Xi [3 ]
Ding, Jinghuan [4 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan 430072, Peoples R China
[2] Xiamen Univ Technol, Sch Environm Sci & Engn, Xiamen 361024, Peoples R China
[3] Anhui Jinzhai Pumped Storage Co Ltd, Jinzhai 237300, Peoples R China
[4] State Grid Xinyuan Co Ltd, Pumped Storage Power Inst Technol & Econ, Beijing 100053, Peoples R China
基金
中国国家自然科学基金;
关键词
pump-turbine; start-up; regulating system; no-load condition; s-shaped characteristic curve; FRANCIS TURBINE; LOAD REJECTION; TRANSIENT;
D O I
10.3390/en14248507
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The pumped-storage power station is an efficient stability regulator of the power grid. However, due to the instability of the pump-turbine in the S-shaped characteristic region, rotational speed fluctuation is easy to occur in the speed no-load condition, making synchronization with and connection to the grid difficult. To investigate the key factors of these difficult grid connections, the start-up processes of a practical pump-turbine under the lowest head condition were simulated by using the three-dimensional CFD method, in which the governor regulating equations with different regulating parameters were integrated successfully. The results show that the working points oscillate with the fluctuations of rotational speed, discharge, and torque, and different regulating parameters have a significant influence on the dynamic histories. In addition, the internal flow patterns, especially the backflows at the runner inlet, keep apparent values at the middle span (0.5 span) but have regular transitions near the shroud side (0.7-0.8 span). The faster the guide vanes adjust, the faster the backflows change, and the larger the macro parameters fluctuate. Overall, the instability of the start-up is the result of the periodical evolutions of backflows at the runner inlet, because the trend and period of the radial velocities at different inlet span locations are consistent with those of the discharge.
引用
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页数:19
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