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首页> 外文期刊>Arabian journal of geosciences >Local impact of dust storms around a suburban building in arid and semi-arid regions: numerical simulation examples from Dubai and Riyadh, Arabian Peninsula
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Local impact of dust storms around a suburban building in arid and semi-arid regions: numerical simulation examples from Dubai and Riyadh, Arabian Peninsula

机译:干旱和半干旱地区郊区建筑物周围沙尘暴的局部影响:来自阿拉伯半岛迪拜和利雅得的数值模拟示例

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Dust storms are common in arid and semi-arid regions, e.g., the Arabian Peninsula, where undisturbed wind can either weather the rocks and transport the grains for kilometers over the landscape or even overseas, or form dunes and ripples. We used a multiphase Eulerian-Lagrangian computational fluid dynamics model to investigate the impact of dust storms in the form of density current on a 10 x 10-m building. This numerical investigation particularly applies to the suburbs of metropolis, consisting of peripheral neighborhoods of meter-scale buildings that, as suggested by our results, can strongly affect the path of the storm before impacting the Downtown. Our results of flow-building interaction on pulsating (CASE 1) versus sustained (CASE 2, reference) and long-lived (CASE 3) storm show a strong amplification of flow dynamic pressure up to a factor of about 14 in streamwise direction and a heavy grain accumulation of about 800 kg around the building. With respect to reference sustained storm, the results show a more intense pressure amplification up to about 12 for slower (CASE 4) or coarser (CASE 5) storm, but a less intense amplification up to about 3 for more dilute storm (CASE 6) in transverse direction. Maximum grain accumulation around the building is of about 4,300 kg (55 % is on building front) for coarser storm, whereas high fog in the building rear occurs for more dilute storm. These results can be useful when assessing the impact of dust storms against buildings.
机译:沙尘暴在干旱和半干旱地区很常见,例如阿拉伯半岛,那里不受干扰的风可以风化岩石,将谷物运送到整个地形上几公里甚至海外,甚至形成沙丘和涟漪。我们使用了多相欧拉-拉格朗日计算流体动力学模型来研究以密度电流形式出现的沙尘暴对10 x 10米建筑物的影响。此数值研究尤其适用于大都市的郊区,该郊区由米级建筑物的外围社区组成,正如我们的结果所暗示的那样,在影响市区之前,可以强烈影响风暴的路径。我们在脉动(案例1)与持续(案例2,参考)和长寿命(案例3)风暴之间建立流动的相互作用结果表明,流动动态压力在水流方向上强烈放大到大约14倍,并且建筑物周围堆积了约800公斤的重谷物。对于参考持续性风暴,结果显示,对于较慢的风暴(案例4)或较粗糙的风暴(案例5),压力增强更大,最高可达约12;对于较弱的风暴,情况强度较小,增强至约3(案例6)在横向。对于较粗的暴风雨,建筑物周围的最大谷物堆积量约为4,300千克(在建筑物正面为55%),而在较稀疏的暴风雨中,建筑物后部会出现高雾。这些结果在评估沙尘暴对建筑物的影响时非常有用。

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