摘要
本文对Lagrange坐标系下的边界层方程进行了数值模拟。研究了静止流场中的线涡诱导的非定常边界层流动。数值结果表明,随着边界层接近分离,确实出现了有限时间奇性。流动在驻定点附近很窄的区域内堆积,并在垂直壁面方向迅速增长,形成一脉冲似的突跃。基于此现象讨论了非定常分离的性质和三种分离模式。采用Lagrange方法能很好地说明有限时间奇性,便干精确地给出分离的定义和判据,而且物理常清楚。Lagrange方法有着明显的解析和计算上的优点。
The unsteady boundary layer due to a rectilinear vortexabove a plane wall in a stagnant fluid are considered using the classicalboundary layer equations in Lagrange coordinates.The calculated re-sults show that as thc boundary-layer flow evolves toward eruption,the spon-taneous generation of a finite time singularity does indeed occur, and theflow focuses into a narrow band near the stationary point in the stream-wise direction,but which grows explosively in the direction normal tothe wall.This developing spike is formed.On the basis of this phenom-enon,we discusscd three kinds of the physical picture of unsteady separa-tion. It is clear that the Lagrangce method is best suited to show thesingularity developed at finite time. It convenient to determine the un-steady separation definitely and to provide a clear and unambiguous cri-terion for the evolution of the separation point physical implication ofthem is very clear.The Lagrange method may have significant analytialand computational advantages.
出处
《空气动力学学报》
CSCD
北大核心
1994年第2期144-151,共8页
Acta Aerodynamica Sinica
关键词
非定常流动
分离流动
数值模拟
unsteady flow,separated flow, numcrical simulation.