Wind Field Characteristics of Complex Terrain Based on Experimental and Numerical Investigation

被引:6
|
作者
Zou, Yunfeng [1 ,2 ]
Yue, Peng [1 ]
Liu, Qingkuan [3 ]
He, Xuhui [1 ,2 ]
Wang, Zhen [1 ]
机构
[1] Cent South Univ, Sch Civil Engn, Changsha 410075, Peoples R China
[2] Hunan Prov Key Lab Disaster Prevent & Mitigat Rai, Changsha 410075, Peoples R China
[3] Shijiazhuang Tiedao Univ, State Key Lab Mech Behav & Syst Safety Traff Engn, Shijiazhuang 050043, Hebei, Peoples R China
来源
APPLIED SCIENCES-BASEL | 2022年 / 12卷 / 10期
基金
中国国家自然科学基金;
关键词
wind energy; island; numerical simulation; wind tunnel test; wind characteristics; BOUNDARY-LAYER-FLOW; LARGE-EDDY SIMULATIONS; TURBULENT-FLOW; 2-DIMENSIONAL HILLS; SURFACE-ROUGHNESS; SIMPLE-MODEL; AIR-FLOW; TUNNEL; TOPOGRAPHY; SEPARATION;
D O I
10.3390/app12105124
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
With the intensification of energy consumption, how to make rational and efficient use of wind energy has been studied all over the world. The construction of facilities to obtain wind energy requires an accurate assessment of the wind characteristics of the local terrain. In order to study the wind characteristics on an island in Southeast China, a 1:1300 terrain model is established, and the characteristics of mean wind and fluctuating wind are studied by numerical simulation and wind tunnel test. The results show that wind speed is affected by the incoming wind direction and local terrain. Wind speed on windward slopes and flat areas with no obstructions is higher, and wind speed on leeward slopes and valleys is lower. Then, the wind attack angle of each measuring point is mainly in the range of -10 degrees-similar to 10 degrees, which is much higher than that in flat areas. The positive and negative wind attack angles are controlled by the incoming wind direction, and the size is closely related to the local terrain. As for pulsation characteristics, the disturbance of the inflow determines the turbulence intensity. The incoming wind direction mainly affects the turbulence intensity on the hillside, while the turbulence intensity in the valley and flat area is controlled by the local terrain. In addition, the fluctuating wind speed power spectra on the island is more consistent with the von Karman spectrum, which is quite different from the Kaimal spectrum. The bandwidth on hillsides and valleys will not change with the change in inflow, but for flat areas, the bandwidth is greatly affected by the inflow direction.
引用
收藏
页数:18
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