日本风电输出变化的地理平滑效应

T. Enomoto, T. Ikegami, C. Urabe, Tetsuo Saitou, K. Ogimoto
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引用次数: 3

摘要

由于大量可再生能源的产出取决于天气变化,人们越来越担心电力系统的供需操作将变得更加困难。为了研究稳定电力系统输出所需的对策,重要的是定量评估风电输出波动和变化对应的供需平衡控制,如涡轮机调速器控制、负荷频率控制和经济负荷调度控制(EDC)。随着风力发电机组安装数量的增加,这些相对于额定输出容量的波动和变化将由于地理平滑效应而减小,即多个风力发电机组的输出波动和变化将相互抵消。在本研究中,我们利用日本东北和九州电力系统的监控和数据采集系统中记录的几个风电场的实际高时间分辨率风力输出数据,定量评估了地理平滑效应。此外,我们使用各种近似曲线评估了与引入的风力有关的平滑效应,并观察到近似曲线的指数部分依赖于区域和周期。利用这些指数部分,我们观察到在较短的周期内获得了完美的平滑效果。EDC域波动的平滑效应很小,特别是在东北地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geographical smoothing effects on wind power output variation in Japan
There is a growing concern that the supply and demand operations of electric power systems will become more difficult with a large number of renewable energy sources whose outputs depend on the weather variations. To investigate the countermeasures that are required to stabilize the outputs of the power systems, it is important to quantitatively evaluate the wind power output fluctuations and variations corresponding to the supply-demand balancing controls, such as turbine governor control, load frequency control, and economic-load dispatching control (EDC). With an increasing number of wind power generators being installed, these fluctuations and variations with respect to the rated output capacity will decrease because of the geographical smoothing effects, i.e., the output fluctuations and variations of multiple wind turbines will mutually cancel one another. In this study, we quantitatively evaluate the geographical smoothing effects using the actual high time-resolution wind power output data of several wind farms that is recorded in the supervisory control and data acquisition systems of the Tohoku and Kyushu power systems in Japan. Further, we evaluate the smoothing effects pertaining to the introduced wind power using various approximation curves, and it is observed that the exponential parts of the approximation curves depend on the region and cycles. Using these exponential parts, we observe that perfect smoothing effects were obtained during the shorter periods of cycles. The smoothing effects of the fluctuations in the EDC domain are observed to be small, especially in the Tohoku region.
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