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Direct numerical simulation of a turbulent flow over an axisymmetric hill

机译:轴对称山上湍流的直接数值模拟

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摘要

Direct numerical simulation (DNS) of a turbulent flow over an axisymmetric hill has been carried out toudstudy the three-dimensional flow separation and reattachment that occur on the lee-side of theudgeometry. The flow Reynolds number is ReH = 6500, based on free-stream quantities and hill heightud(H). A synthetic inflow boundary condition, combined with a data feed-in method, has been used toudgenerate the turbulent boundary layer approaching to the hill. The simulation has been run using audtypical DNS resolution of Dxþ ¼ 12:5; Dzþ ¼ 6:5, and Dyþ1ud¼ 1:0 and about 10 points in the viscousudsublayer. It was found that a separation bubble exists at the foot of the wind-side of the hill and theudincoming turbulent boundary layer flow undergoes re-laminarization process around the crest of the hill.udThese lead to a significant flow separation at the lee-side of the hill, where a very large primary separationudbubble embedded with a smaller secondary separations have been captured. The present low-Reudsimulation reveals some flow features that are not observed by high-Re experiments, thus is useful forudfuture experimental studies.
机译:已经对轴对称山丘上的湍流进行了直接数值模拟(DNS),以研究发生在测速仪背风侧的三维流动分离和重新附着。基于自由流数量和山高 ud(H),流雷诺数为ReH = 6500。综合入流边界条件与数据输入方法相结合,已被用于估算接近丘陵的湍流边界层。该模拟使用Dxþ¼12:5的 DNS典型解析度进行; Dz ¼6:5和Dyþ1ud¼1:0,在粘性 udsublayer中大约有10个点。已发现在山的风侧的脚下存在分离气泡,并且 uding的湍流边界层流在山的波峰周围经历了重新层化过程。 ud这些导致在背风处显着的流分离。 -在山坡的一侧,捕获了很大的初级分隔气泡,其中嵌有较小的次级分隔。当前的低Re模拟揭示了一些高high实验未观察到的流动特征,因此对于今后的实验研究很有用。

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  • 年度 2014
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