风力涡轮机尾流中的速度和湍流细分 - 第 1 部分:大涡流模拟研究

Erwan Jézéquel, Frederic Blondel, Valery Masson
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引用次数: 1

摘要

摘要基于运动参照系和固定参照系(MFOR 和 FFOR)的分析,提出了一种新的理论框架来分解风力涡轮机尾流中的速度场和湍流场。这种方法为基于动态尾流蜿蜒(DWM)的模型提供了理论支持,并为建立一个将蜿蜒和大气稳定性考虑在内的、完全基于物理分析的尾流模型开辟了道路。FFOR 中的平均速度和湍流被分解成不同的项,它们是 MFOR 中速度和湍流的函数。这些项可以重新组合为纯项和交叉项。在 DWM 中,前一组被模拟,而后一组被隐式忽略。不同项的形状和相对重要性是通过大涡流模拟求解器 Meso-NH 和致动器线法估算出来的。在中性、不稳定和稳定三种稳定情况下,模拟了平坦地形上的单个风力涡轮机尾流。在速度分解中,交叉项相对较低。而湍流分解方程则不然,尽管交叉项的总体量级小于纯项,但它们会重新分配湍流并引起不可忽略的不对称。这些发现强调了假定 MFOR 速度稳定的模型的局限性,如 DWM 或同行论文中开发的模型。研究还发现,随着大气稳定性的增加,纯湍流的贡献相对变大,而纯蜿蜒的贡献相对变小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Breakdown of the velocity and turbulence in the wake of a wind turbine – Part 1: Large-eddy-simulation study
Abstract. A new theoretical framework, based on an analysis in the moving and fixed frames of reference (MFOR and FFOR), is proposed to break down the velocity and turbulence fields in the wake of a wind turbine. This approach adds theoretical support to models based on the dynamic wake meandering (DWM) and opens the way for a fully analytical and physically based model of the wake that takes meandering and atmospheric stability into account, which is developed in the companion paper. The mean velocity and turbulence in the FFOR are broken down into different terms, which are functions of the velocity and turbulence in the MFOR. These terms can be regrouped as pure terms and cross terms. In the DWM, the former group is modelled, and the latter is implicitly neglected. The shape and relative importance of the different terms are estimated with the large-eddy-simulation solver Meso-NH coupled with an actuator line method. A single wind turbine wake is simulated on flat terrain, under three cases of stability: neutral, unstable and stable. In the velocity breakdown, the cross term is found to be relatively low. It is not the case for the turbulence breakdown equation where even though the cross terms are overall of lesser magnitude than the pure terms, they redistribute the turbulence and induce a non-negligible asymmetry. These findings underline the limitations of models that assume a steady velocity in the MFOR, such as the DWM or the model developed in the companion paper. It is also found that as atmospheric stability increases, the pure turbulence contribution becomes relatively larger and pure meandering relatively smaller.
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