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Wind-sand coupling movement induced by strong typhoon and its influences on aerodynamic force distribution of the wind turbine

机译:强台风引起的风沙耦合运动及其对风力涡轮机气动力分布的影响

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摘要

The strong turbulence characteristic of typhoon not only will significantly change flow field characteristics surrounding the large-scale wind turbine and aerodynamic force distribution on surface, but also may cause morphological evolution of coast dune and thereby form sand storms. A 5MW horizontal-axis wind turbine in a wind power plant of southeastern coastal areas in China was chosen to investigate the distribution law of additional loads caused by wind-sand coupling movement of coast dune at landing of strong typhoons. Firstly, a mesoscale Weather Research and Forecasting (WRF) mode was introduced in for high spatial resolution simulation of typhoon "Megi". Wind speed profile on the boundary layer of typhoon was gained through fitting based on nonlinear least squares and then it was integrated into the user-defined function (UDF) as an entry condition of small-scaled CFD numerical simulation. On this basis, a synchronous iterative modeling of wind field and sand particle combination was carried out by using a continuous phase and discrete phase. Influencing laws of typhoon and normal wind on moving characteristics of sand particles, equivalent pressure distribution mode of structural surface and characteristics of lift resistance coefficient were compared. Results demonstrated that: Compared with normal wind, mesoscale typhoon intensifies the 3D aerodynamic distribution mode on structural surface of wind turbine significantly. Different from wind loads, sand loads mainly impact on 30 degrees ranges at two sides of the lower windward region on the tower. The ratio between sand loads and wind load reaches 3.937% and the maximum sand pressure coefficient is 0.09. The coupling impact effect of strong typhoon and large sand particles is more significant, in which the resistance coefficient of tower is increased by 9.80% to the maximum extent. The maximum resistance coefficient in typhoon field is 13.79% higher than that in the normal wind field.
机译:台风的强劲湍流特性不仅将显着改变大规模风力涡轮机的流场特征和表面上的空气动力分布,也可能导致海岸沙丘的形态演变,从而形成沙尘暴。选择了中国东南沿海地区风电厂的5MW水平轴风力涡轮机,探讨了海岸沙丘风砂耦合运动造成的额外载荷的分布定律。首先,引入了Mescre天气研究和预测(WRF)模式,用于台风“Megi”的高空间分辨率仿真。通过基于非线性最小二乘的拟合来获得台风边界层上的风速轮廓,然后将其集成到用户定义的函数(UDF)中作为小缩放的CFD数值模拟的进入条件。在此基础上,通过使用连续相和离散相来进行风场和砂颗粒组合的同步迭代建模。对砂颗粒的移动特性影响台风和正常风量,结构表面等效压力分布和提升性系数特性。结果表明:与正常风相比,Mescle Typhoon显着加强了风力涡轮机结构表面的3D空气动力学分配模式。与风荷载有不同,砂荷主要影响塔上下迎风区域的两侧的30度范围。砂荷载和风力荷载之间的比率达到3.937%,最大砂压系数为0.09。强斜台和大砂颗粒的耦合冲击效果更为显着,其中塔的电阻系数增加了9.80%至最大程度。台风场的最大电阻系数高于正常风场中的13.79%。

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