Abhishek Mishra, Marco Placidi, Matteo Carpentieri, Alan Robins
{"title":"深层边界层中建筑物群尾流特性研究","authors":"Abhishek Mishra, Marco Placidi, Matteo Carpentieri, Alan Robins","doi":"10.1007/s10546-023-00830-0","DOIUrl":null,"url":null,"abstract":"Abstract Wind tunnel experiments were conducted to understand the effect of building array size ( N ), aspect ratio ( AR ), and the spacing between buildings ( $$W_S$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>S</mml:mi> </mml:msub> </mml:math> ) on the mean structure and decay of their wakes. Arrays of size 3 $$\\times $$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mo>×</mml:mo> </mml:math> 3, 4 $$\\times $$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mo>×</mml:mo> </mml:math> 4,and 5 $$\\times $$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mo>×</mml:mo> </mml:math> 5, AR = 4, 6, and 8, and $$W_S$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>S</mml:mi> </mml:msub> </mml:math> = 0.5 $$W_B$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> , 1 $$W_B$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> , 2 $$W_B$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> and 4 $$W_B$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> (where $$W_B$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> is the building width) were considered. Three different wake regimes behind the building clusters were identified: near-, transition-, and far-wake regimes. The results suggest that the spatial extent of these wake regimes is governed by the overall array width ( $$W_A$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> </mml:math> ). The effects of individual buildings are observed to be dominant in the near-wake regime ( $$0<x/W_A< {0.45}$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mrow> <mml:mn>0</mml:mn> <mml:mo><</mml:mo> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo><</mml:mo> <mml:mrow> <mml:mn>0.45</mml:mn> </mml:mrow> </mml:mrow> </mml:math> ) where individual wakes appear behind each building. These wakes are observed to merge in the transition-wake region ( $${0.45}< x/W_A < 1.5$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mrow> <mml:mrow> <mml:mn>0.45</mml:mn> </mml:mrow> <mml:mo><</mml:mo> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo><</mml:mo> <mml:mn>1.5</mml:mn> </mml:mrow> </mml:math> ), forming a combined wake in which the individual contributions are no longer apparent. In the far-wake regime ( $$x/W_A > 1.5$$ <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mrow> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo>></mml:mo> <mml:mn>1.5</mml:mn> </mml:mrow> </mml:math> ), clusters’ wakes are akin to those developing downwind of a single isolated building. Accordingly, new local and global scaling parameters in the near- and far-wake regimes are introduced. The decay of the centreline velocity deficit is then modelled as a function of the three parameters considered in the experiment.","PeriodicalId":9153,"journal":{"name":"Boundary-Layer Meteorology","volume":"8 1","pages":"0"},"PeriodicalIF":2.3000,"publicationDate":"2023-10-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Wake Characterization of Building Clusters Immersed in Deep Boundary Layers\",\"authors\":\"Abhishek Mishra, Marco Placidi, Matteo Carpentieri, Alan Robins\",\"doi\":\"10.1007/s10546-023-00830-0\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract Wind tunnel experiments were conducted to understand the effect of building array size ( N ), aspect ratio ( AR ), and the spacing between buildings ( $$W_S$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>S</mml:mi> </mml:msub> </mml:math> ) on the mean structure and decay of their wakes. Arrays of size 3 $$\\\\times $$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mo>×</mml:mo> </mml:math> 3, 4 $$\\\\times $$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mo>×</mml:mo> </mml:math> 4,and 5 $$\\\\times $$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mo>×</mml:mo> </mml:math> 5, AR = 4, 6, and 8, and $$W_S$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>S</mml:mi> </mml:msub> </mml:math> = 0.5 $$W_B$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> , 1 $$W_B$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> , 2 $$W_B$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> and 4 $$W_B$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> (where $$W_B$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>B</mml:mi> </mml:msub> </mml:math> is the building width) were considered. Three different wake regimes behind the building clusters were identified: near-, transition-, and far-wake regimes. The results suggest that the spatial extent of these wake regimes is governed by the overall array width ( $$W_A$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> </mml:math> ). The effects of individual buildings are observed to be dominant in the near-wake regime ( $$0<x/W_A< {0.45}$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mrow> <mml:mn>0</mml:mn> <mml:mo><</mml:mo> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo><</mml:mo> <mml:mrow> <mml:mn>0.45</mml:mn> </mml:mrow> </mml:mrow> </mml:math> ) where individual wakes appear behind each building. These wakes are observed to merge in the transition-wake region ( $${0.45}< x/W_A < 1.5$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mrow> <mml:mrow> <mml:mn>0.45</mml:mn> </mml:mrow> <mml:mo><</mml:mo> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo><</mml:mo> <mml:mn>1.5</mml:mn> </mml:mrow> </mml:math> ), forming a combined wake in which the individual contributions are no longer apparent. In the far-wake regime ( $$x/W_A > 1.5$$ <mml:math xmlns:mml=\\\"http://www.w3.org/1998/Math/MathML\\\"> <mml:mrow> <mml:mi>x</mml:mi> <mml:mo>/</mml:mo> <mml:msub> <mml:mi>W</mml:mi> <mml:mi>A</mml:mi> </mml:msub> <mml:mo>></mml:mo> <mml:mn>1.5</mml:mn> </mml:mrow> </mml:math> ), clusters’ wakes are akin to those developing downwind of a single isolated building. Accordingly, new local and global scaling parameters in the near- and far-wake regimes are introduced. The decay of the centreline velocity deficit is then modelled as a function of the three parameters considered in the experiment.\",\"PeriodicalId\":9153,\"journal\":{\"name\":\"Boundary-Layer Meteorology\",\"volume\":\"8 1\",\"pages\":\"0\"},\"PeriodicalIF\":2.3000,\"publicationDate\":\"2023-10-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Boundary-Layer Meteorology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1007/s10546-023-00830-0\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"METEOROLOGY & ATMOSPHERIC SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Boundary-Layer Meteorology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1007/s10546-023-00830-0","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
摘要
摘要通过风洞实验研究了建筑阵列尺寸(N)、建筑展弦比(AR)和建筑间距($$W_S$$ W S)对尾迹平均结构和衰减的影响。考虑大小为3 $$\times $$ × 3,4 $$\times $$ × 4和5 $$\times $$ × 5的数组,AR = 4,6和8,$$W_S$$ ws = 0.5 $$W_B$$ wb, 1 $$W_B$$ wb, 2 $$W_B$$ wb和4 $$W_B$$ wb(其中$$W_B$$ wb为建筑物宽度)。确定了建筑群背后的三种不同的尾流状态:近尾流、过渡尾流和远尾流状态。结果表明,这些尾迹的空间范围是由总阵列宽度($$W_A$$ W A)控制的。单个建筑物的影响在近尾流状态下占主导地位($$0<x/W_A< {0.45}$$ 0 &lt;x / W &lt;0.45),每个建筑后面都有单独的尾流。观察到这些尾迹在过渡尾迹区域合并($${0.45}< x/W_A < 1.5$$ 0.45 &lt;x / W &lt;1.5),形成一个组合尾流,其中个体的贡献不再明显。远尾流状态下($$x/W_A > 1.5$$ x / W A &gt;1.5),集群的尾流类似于单个孤立建筑顺风处的尾流。因此,在近尾流和远尾流中引入了新的局部和全局尺度参数。然后将中线速度差的衰减建模为实验中考虑的三个参数的函数。
Wake Characterization of Building Clusters Immersed in Deep Boundary Layers
Abstract Wind tunnel experiments were conducted to understand the effect of building array size ( N ), aspect ratio ( AR ), and the spacing between buildings ( $$W_S$$ WS ) on the mean structure and decay of their wakes. Arrays of size 3 $$\times $$ × 3, 4 $$\times $$ × 4,and 5 $$\times $$ × 5, AR = 4, 6, and 8, and $$W_S$$ WS = 0.5 $$W_B$$ WB , 1 $$W_B$$ WB , 2 $$W_B$$ WB and 4 $$W_B$$ WB (where $$W_B$$ WB is the building width) were considered. Three different wake regimes behind the building clusters were identified: near-, transition-, and far-wake regimes. The results suggest that the spatial extent of these wake regimes is governed by the overall array width ( $$W_A$$ WA ). The effects of individual buildings are observed to be dominant in the near-wake regime ( $$00<x/WA<0.45 ) where individual wakes appear behind each building. These wakes are observed to merge in the transition-wake region ( $${0.45}< x/W_A < 1.5$$ 0.45<x/WA<1.5 ), forming a combined wake in which the individual contributions are no longer apparent. In the far-wake regime ( $$x/W_A > 1.5$$ x/WA>1.5 ), clusters’ wakes are akin to those developing downwind of a single isolated building. Accordingly, new local and global scaling parameters in the near- and far-wake regimes are introduced. The decay of the centreline velocity deficit is then modelled as a function of the three parameters considered in the experiment.
期刊介绍:
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