| 海岸破波带内水底悬沙浓度形成机理实验研究 |
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| 引用本文： | 张洋,邹志利,薛武山,孙大鹏.海岸破波带内水底悬沙浓度形成机理实验研究[J].海洋通报,2018(2):181-191. |
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| 作者姓名： | 张洋 邹志利 薛武山 孙大鹏 |
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| 作者单位： | 大连理工大学海岸和近海工程国家重点实验室 |
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| 基金项目： | 国家自然科学基金（51079024） |
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| 摘 要： | 通过大尺度水槽波浪引起泥沙悬移的动床模型实验,研究了沙坝海岸破波带内水底悬沙浓度形成机理,通过比较时间平均水底悬沙浓度与时间平均水底波浪水质点动能或时间平均水底湍动能之间的相关性,论证了利用时间平均湍动能比利用时间平均波浪水质点动能计算时间平均水底悬沙浓度更为适用,并提出了以上时间平均水底悬沙浓度与水底湍动能之间的关系也可以用来近似表达时间变化的水底悬沙浓度与时间变化的水底湍动能之间的关系。研究针对规则波、波群和不规则波3种波浪形态进行,并分别对破波带内的爬坡区、内破波区和沙坝区3个区域实验结果进行讨论。
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| 关 键 词： | 破波带 波浪形态 悬沙浓度 湍动能 沙坝 |
| 收稿时间： | 2017/8/12 0:00:00 |
| 修稿时间： | 2017/11/2 0:00:00 |
Experimental study on the formation mechanism of bottom suspended sediment concentration in surf zone |
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| ZHANG Yang,ZOU Zhi-li,XUE Wu-shan and SUN Da-peng.Experimental study on the formation mechanism of bottom suspended sediment concentration in surf zone[J].Marine Science Bulletin,2018(2):181-191. |
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| Authors: | ZHANG Yang ZOU Zhi-li XUE Wu-shan and SUN Da-peng |
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| Institution: | State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China,State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China,State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China and State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China |
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| Abstract: | To study the formation mechanism of bottom suspended sediment concentration in surf zone, a series of experiments were conducted in a large scale wave flume for the wave conditions of regular wave, wave group and irregular wave. The correlation of bottom suspended sediment concentration with the wave kinetic energy or the turbulent kinetic energy near bottom are examined. The results show that the bottom suspended sand concentration which can be calculated in terms of the pick-up function correlates better to the turbulent kinetic energy at bottom, which contain both the wave breaking effect and bottom boundary turbulent flow effect, than to the kinetic energy of wave flow, which is a representation of the bottom shear stress. Based on this result, the superiority of the formula for the bottom concentration in terms of wave energy dissipation to that in terms of bottom shear stress is verified. |
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| Keywords: | surf zone wave type suspended sediment concentration turbulent kinetic energy sand bar |
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