1 Notes on 1.63 Advanced Environmental Fluid Mechanics Instructor: C. C. Mei, 2002
[email protected], 1 617 253 2994 October 30, 2002 Chapter 5. Rudiments of hydrodynamic instability References: Drazin: Introduction to hydrodynamic stability Chandrasekar: Hydrodynamic and hydromagnatic instability Stuart: Hydrodynamic stability,inRosenhead(ed):Laminar boundary layers Lin : Theory of Hydrodynamic stability Drazin and Reid : Hydrodynamic stability Schlichting: Boundary layer theory C.S. Yih, 1965, Dynamics of Inhomogeneous Fluids, MacMillan. −−−−−−−−−−−−−−−−−−− Various factors can be crucial to hydrodynamic instability.: shear, gravity, surface tension, heat, centrifugal force, etc. Some instabilities lead to a different flow; some to turbulence. We only discuss the linearized analysis of instability. Let us take the parallel flow as an example and outline the standard procedure of lin- earized analysis as follows: 1. Let the basic flow have velocity U(z)inthex direction. 2. Derive the linearized equation for infinitestimal perturbations and homogeneous bound- ary conditions. 3. Consider sinusoidal wave- like disturbances so that all unknowns are of the form ¯ i(kx ωt) fi = fi(z)e − 4. Reduce the partial differential equations to ordinary differential equation(s), hence obtain an eignevalue problem. 5. Solve for the eigenvalue ω for a given and real k. 6. If the eigenvalue is complex, ω = ωr +iωi, find the condition under which ωi > 0. Since iωt i(ωr+iωi)t iωrt ωit e− = e− = e− e , the flow is unstable ωi > 0 as time grows, stable if ωi < 0, and neutrally stable if ωi =0. 2 5.1 Kelvin-Helmholtz instability of flow with discon- tinuous shear and stratification.