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峡谷地形平均风速特性与加速效应
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Research on Mean Wind Speed Characteristics and Speed-up Effect in Canyon Terrain
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    摘要:

    采用计算流体力学(CFD)方法建立多个数值模型,通过与风洞试验的对比分析验证了数值模拟结果的可靠性,较系统地研究并详细分析了峡谷长度、山顶间距、山脉坡度3种地貌因素对平均风加速效应的影响.结果表明:山脉顶部加速效应主要受山脉坡度的影响,在近地面内坡度越大加速效应越明显;峡谷内部加速效应受多种地貌因素影响且变化趋势较为复杂,必须考虑峡谷侧坡边界层的影响和流动的三维效应,当峡谷长度越短、山顶间距越小、山脉坡度越大时,迎风谷口处在近地面内的加速效应越明显.最后计算出典型峡谷的风压地形修正系数,并与我国建筑结构荷载规范进行对比.

    Abstract:

    Multiple numerical models were established by Computational Fluid Dynamics (CFD) method, and the reliability of the numerical results was also verified by the comparison with that of a wind tunnel test. The CFD analysis was then systematically carried out to study the influence of three geomorphological factors, the length of the canyon, distance between two peaks, and slope of the mountain, on the mean wind speed-up effect. The analysis results showed that the speed-up effect at the mountaintop was significantly affected by the slope of the mountain. The larger the slope was, the more significant the speed-up effect was in the near surface. Furthermore, the speed-up effect inside the canyon was influenced by the multiple geomorphological factors, and the variation trends were complicated. Therefore, the influence of the side slope boundary layer of the canyon and the three-dimensional effect of airflow should be considered. When the length of the canyon and the distance between two peaks decreased, and the slope of the mountain increased, the speed-up effect at the windward canyon entrance was more obvious in the near surface. Finally, the wind pressure terrain correction coefficient of the typical canyon was calculated and compared with the prescription of Chinese design code for building structures.

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楼文娟,刘萌萌,李正昊,章李刚,卞 荣.峡谷地形平均风速特性与加速效应[J].湖南大学学报:自然科学版,2016,43(7):8~15

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  • 在线发布日期: 2016-08-11
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