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教授   博士生导师   硕士生导师

性别: 男

出生日期: 1955-05-06

毕业院校: 江苏工学院

学位: 学士

所在单位: 力学与航空航天学院

学科: 流体力学. 计算力学. 航空航天力学与工程. 飞行器设计

办公地点: 大连理工大学综合实验一号楼415室

联系方式: cjwudut@dlut.edu.cn或cj_wu@163.com

电子邮箱: cjwudut@dlut.edu.cn

学术主页: : http://202.118.74.190/~cjwu/

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当前位置: 中文主页 >> 科学研究 >> 论文成果
Numerical Simulations of Two Coaxial Vortex Rings Head-on Collision

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论文类型: 期刊论文

发表时间: 2016-08-01

发表刊物: ADVANCES IN APPLIED MATHEMATICS AND MECHANICS

收录刊物: SCIE、Scopus

卷号: 8

期号: 4

页面范围: 616-647

ISSN号: 2070-0733

关键字: Three dimensional numerical simulation; vortex ring; collision; large eddy-simulation

摘要: Vortex rings have been a subject of interest in vortex dynamics due to a plethora of physical phenomena revealed by their motions and interactions within a boundary. The present paper is devoted to physics of a head-on collision of two vortex rings in three dimensional space, simulated with a second order finite volume scheme and compressible. The scheme combines non-iterative approximate Riemannsolver and piecewise-parabolic reconstruction used in inviscid flux evaluation procedure. The computational results of vortex ring collisions capture several distinctive phenomena. In the early stages of the simulation, the rings propagate under their own self-induced motion. As the rings approach each other, their radii increase, followed by stretching and merging during the collision. Later, the two rings have merged into a single doughnut-shaped structure. This structure continues to extend in the radial direction, leaving a web of particles around the centers. At a later time, the formation of ringlets propagate radially away from the center of collision, and then the effects of instability involved leads to a reconnection in which small-scale ringlets are generated. In addition, it is shown that the scheme captures several experimentally observed features of the ring collisions, including a turbulent breakdown into small-scale structures and the generation of small-scale radially propagating vortex rings, due to the modification of the vorticity distribution, as a result of the entrainment of background vorticity and helicity by the vortex core, and their subsequent interaction.

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