上海交通大学学报 ›› 2021, Vol. 55 ›› Issue (4): 412-420.doi: 10.16183/j.cnki.jsjtu.2019.228

所属专题: 《上海交通大学学报》2021年12期专题汇总专辑 《上海交通大学学报》2021年“水利工程”专题

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线性层结环境和浸没式植被对斜坡异重流运动的影响

刘雅钰, 林颖典(), 袁野平, 贺治国   

  1. 浙江大学 海洋学院,浙江 舟山 316021
  • 收稿日期:2019-08-02 出版日期:2021-04-28 发布日期:2021-04-30
  • 通讯作者: 林颖典 E-mail:kevinlin@zju.edu.cn
  • 作者简介:刘雅钰(1995-),女,浙江省杭州市人,硕士生,主要研究方向为异重流
  • 基金资助:
    国家重点研发计划(2017YFC0405502);国家自然科学基金(11672267);国家自然科学基金(41876089);舟山市科技计划项目浙江大学海洋学院专项资助项目(2018C81034)

Effect of Linearly Stratified Environment and Submerged Vegetation on Hydrodynamic Characteristics of Downslope Gravity Currents

LIU Yayu, LIN Yingtien(), YUAN Yeping, HE Zhiguo   

  1. Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang, China
  • Received:2019-08-02 Online:2021-04-28 Published:2021-04-30
  • Contact: LIN Yingtien E-mail:kevinlin@zju.edu.cn

摘要:

开展一系列开闸式斜坡异重流水槽实验,分析线性层结和均匀水体中斜坡异重流遭遇刚性植被群的发展和演变特性.采用彩色数码相机记录异重流发展过程,并利用粒子图像测速技术(PIV)获取局部流场结构.结果表明:对于有植被工况,异重流的头部速度可分为加速、减速、二次加速及二次减速4个阶段.各阶段之间的转变位置随层结度增大而前移,但受植被密度影响不明显.在层结环境中,受植被群影响,异重流会出现“首次分离-前进-二次分离”现象.植被群削弱异重流涡度场的发展,随植被密度增大,该差异愈加显著.层结水体和植被群均会抑制异重流涡度场的发展,其中层结水体的抑制作用更强.

关键词: 层结环境, 浸没式植被, 斜坡, 异重流

Abstract:

A series of lock-exchange experiments of slope gravity currents were conducted to analyze the development and evolution characteristics of rigid vegetations in uniform and linear stratified environments. The development of gravity currents was recorded by using a digital camera, and the local flow field structure was obtained by particle image velocimetry (PIV). The results show that the head velocity of gravity currents with submerge vegetation experience the processes of acceleration, deceleration, second acceleration, and second deceleration. As the stratification degree increases, the transition points among the four stages move ahead, but the vegetation density does not significantly impact that point. In the stratified environments with the submerged vegetation patches, the phenomena of “first separated then advanced and finally separated from the slope” is observed. Vegetation can restrain the development of vorticity fields of gravity currents. When the vegetation densens, the vorticity of gravity currents will decrease more significantly. Both stratified environments and submerged vegetation patches can inhibit the development of vorticity fields of gravity currents, and the stratified water environment plays a more important role in this inhibition.

Key words: stratified environment, submerged vegetation, slope, gravity currents

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