An Investigation into the Distribution of Fluctuating Wind Pressure and Associated Probabilistic Characteristics of Low-Rise Buildings Impacted by the Gap between the Hillside and the Building

被引:0
|
作者
Zhong, Min [1 ,2 ]
Wang, Chao [2 ]
Lin, Minghui [3 ]
Lu, Junyu [3 ]
Wang, Xiangjun [4 ]
机构
[1] Jiangsu Open Univ, Sch Architecture & Engn, Nanjing 210036, Peoples R China
[2] Hunan Univ, Coll Civil Engn, Changsha 410082, Peoples R China
[3] Hebei Univ Architecture, Coll Civil Engn, Zhangjiakou 075000, Peoples R China
[4] Yangzhou Univ, Coll Elect Energy & Power Engn, Yangzhou 225127, Peoples R China
关键词
fluctuating wind pressure distribution; probabilistic properties; low-rise buildings; mountain form; the distance from the mountain; SURROUNDINGS;
D O I
10.3390/buildings14051435
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
In China's mountainous coastal terrain, storms can badly damage low-rise buildings. At present, it is not clear how the relative position of buildings and mountains affects the surface of low-rise buildings. The study compared these results with the wind pressure distribution without the surrounding environment. The distribution of wind pressure in different hillside landforms is examined through a wind tunnel experiment, which is also compared with the distribution in an open environment. The study examined the fluctuating coefficient as the distance between the building and the hillside changed, specifically for wind blowing at a 0 degrees angle. The investigation examined the power spectrum and wind pressure probability distribution while considering the proximity of the building to an adjacent hill. The findings indicated that as the distance between the slope and the mountain increases, the fluctuating wind pressure coefficient continues to increase, and the contour lines of the wind pressure distribution are relatively denser compared to where there is a mountain. The maximum value of the fluctuating wind pressure coefficient is 0.22, which appears at the windward roof. The roof's wind pressure coefficient fluctuated and gradually increased until it reached its peak, unaffected by the surroundings. The wind pressure on the leeward side exhibited Gaussian characteristics in its probability distribution.
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页数:39
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