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黄远东,赵树夫,姜剑伟,周中华,顾 静.多孔方型人工鱼礁绕流的数值模拟研究水资源与水工程学报[J].,2012,23(5):15-18
多孔方型人工鱼礁绕流的数值模拟研究
Study on numerical simulation of water flow past a porous square artificial reef
投稿时间:2012-05-24  
DOI:10.11705/j.issn.1672-643X.2012.05.004
中文关键词:  多孔方型人工鱼礁  水流场  上升流  背涡区  数值模拟
英文关键词:porous square artificial reef  water flow field  upwelling  wake vortex region  numerical simulation
基金项目:上海市教委重点学科建设项目(J50502);上海市研究生创新基金项目(JWCXSL1102)
作者单位
黄远东 上海理工大学 环境与建筑学院,上海 200093 
赵树夫 上海理工大学 环境与建筑学院,上海 200093 
姜剑伟 上海理工大学 环境与建筑学院,上海 200093 
周中华 上海理工大学 环境与建筑学院,上海 200093 
顾 静 上海理工大学 环境与建筑学院,上海 200093 
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中文摘要:
      数值模拟得到了5种不同来流速度(0.1~0.8 m/s)下的多孔方型人工鱼礁周围的水流场。过礁体中心的铅垂面上速度分布表明:①不同来流速度下,上升流的最大速度和平均速度均分别为来流速度的0.74倍和0.12倍,上升流最大高度均为礁体高度的2.6~2.7倍,背涡区的长度和高度均分别为礁体高度的4倍和1.25倍;②在靠近礁体背流面形成水流方向与来流方向相一致的透水区。过礁体中心的水平面上速度分布表明:①不同来流速度下,背涡区的长度和宽度均分别为礁体宽度的4倍和1.8倍;②在鱼礁内部形成水流方向杂乱的旋涡区。本研究还初步比较了多孔方型人工鱼礁绕流与无孔方型人工鱼礁绕流的流场效应异同点。
英文摘要:
      Numerical simulations are performed to obtain the water flow fields around a porous square artificial reef under the five different incoming velocities (0.1~0.8m/s). The numerical results of velocity distribution on the perpendicular flow plane passing through the center of the reef show that (1) under the five different incoming velocities the maximum and average velocities of the upwelling are 0.74 and 0.12 times of the incoming velocity, respectively, the maximum height of the upwelling is about 2.6 to 2.7 times of the reef height,and the length and height of the vortex region are 4 and 1.25 times of the reef height respectively; (2) a region where the flow direction is the same as that of the incoming flow is formed near the leeward surface of the reef. The numerical results of the velocity distribution on the horizontal flow plane passing the center of the reef reveal that (1) the length and width of the wake vortex region are 4 and 1.8 times of the reef width, respectively, for each of the five different incoming velocities; (2) vortex regions are also formed inside the reef. In this study, the similarities and differences with respect to the flow characteristics are also summarized preliminarily between the flow past a square reef without holes and the flow past a porous square reef.
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