Introduction to Symmetry Analysis

Slides:



Advertisements
Similar presentations
Introduction Irina Surface layer and surface fluxes Anton
Advertisements

Canopy Spectra and Dissipation John Finnigan CSIRO Atmospheric Research Canberra, Australia.
Introduction to Computational Fluid Dynamics
Source: A. Mason-Jones, PhD thesis Cardiff University (2010) Moving Mesh ApproachTime-averaged Approach.
TURBULENCE MODELING A Discussion on Different Techniques used in Turbulence Modeling -Reni Raju.
Lecture 15: Capillary motion
Particle Acceleration Particle t t+dt. Physical Interpretation Total acceleration of a particle Local acceleration Convective acceleration time velocity.
Louisiana Tech University Ruston, LA Slide 1 Time Averaging Steven A. Jones BIEN 501 Monday, April 14, 2008.
Turbulent Models.  DNS – Direct Numerical Simulation ◦ Solve the equations exactly ◦ Possible with today’s supercomputers ◦ Upside – very accurate if.
Lecture 9 - Kolmogorov’s Theory Applied Computational Fluid Dynamics
Anisotropic Pressure and Acceleration Spectra in Shear Flow Yoshiyuki Tsuji Nagoya University Japan Acknowledgement : Useful discussions and advices were.
1 MECH 221 FLUID MECHANICS (Fall 06/07) Tutorial 7.
Stanford University Department of Aeronautics and Astronautics Introduction to Symmetry Analysis Brian Cantwell Department of Aeronautics and Astronautics.
Sensible heat flux Latent heat flux Radiation Ground heat flux Surface Energy Budget The exchanges of heat, moisture and momentum between the air and the.
Wolfgang Kinzelbach with Marc Wolf and Cornel Beffa
Boundary Layer Meteorology Lecture 4 Turbulent Fluxes Energy Cascades Turbulence closures TKE Budgets.
Transport Equations for Turbulent Quantities
P M V Subbarao Professor Mechanical Engineering Department I I T Delhi
Reynolds Method to Diagnosize Symptoms of Infected Flows.... P M V Subbarao Professor Mechanical Engineering Department I I T Delhi Reynolds Averaged.
FUNDAMENTAL EQUATIONS, CONCEPTS AND IMPLEMENTATION
Conservation Laws for Continua
Stanford University Department of Aeronautics and Astronautics Introduction to Symmetry Analysis Brian Cantwell Department of Aeronautics and Astronautics.
CFD Modeling of Turbulent Flows
Stanford University Department of Aeronautics and Astronautics Introduction to Symmetry Analysis Brian Cantwell Department of Aeronautics and Astronautics.
Lecture Objectives: -Define turbulence –Solve turbulent flow example –Define average and instantaneous velocities -Define Reynolds Averaged Navier Stokes.
Introduction to Fluid Mechanics
0 Local and nonlocal conditional strain rates along gradient trajectories from various scalar fields in turbulence Lipo Wang Institut für Technische Verbrennung.
1 LES of Turbulent Flows: Lecture 11 (ME EN ) Prof. Rob Stoll Department of Mechanical Engineering University of Utah Fall 2014.
Xin Xi. 1946: Obukhov Length, as a universal length scale for exchange processes in surface layer. 1954: Monin-Obukhov Similarity Theory, as a starting.
Governing equations: Navier-Stokes equations, Two-dimensional shallow-water equations, Saint-Venant equations, compressible water hammer flow equations.
Reynolds-Averaged Navier-Stokes Equations -- RANS
Lecture 8 - Turbulence Applied Computational Fluid Dynamics
Turbulent properties: - vary chaotically in time around a mean value - exhibit a wide, continuous range of scale variations - cascade energy from large.
LES of Turbulent Flows: Lecture 2 (ME EN )
Physics of turbulence at small scales Turbulence is a property of the flow not the fluid. 1. Can only be described statistically. 2. Dissipates energy.
The Stability of Laminar Flows - 2
Ch 4 Fluids in Motion.
Quantification of the Infection & its Effect on Mean Fow.... P M V Subbarao Professor Mechanical Engineering Department I I T Delhi Modeling of Turbulent.
Outline Time Derivatives & Vector Notation
Analysis of Turbulent (Infected by Disturbance) Flows
LES of Turbulent Flows: Lecture 5 (ME EN )
Basic dynamics ●The equations of motion and continuity Scaling Hydrostatic relation Boussinesq approximation ●Geostrophic balance in ocean’s interior.
Basic dynamics The equation of motion Scale Analysis
Turbulence Modeling In FLOTRAN Chapter 5 Training Manual May 15, 2001 Inventory # Questions about Turbulence What is turbulence and what are.
Scales of Motion, Reynolds averaging September 22.
1 LES of Turbulent Flows: Lecture 10 (ME EN ) Prof. Rob Stoll Department of Mechanical Engineering University of Utah Spring 2011.
Viscosità Equazioni di Navier Stokes. Viscous stresses are surface forces per unit area. (Similar to pressure) (Viscous stresses)
Turbulent Fluid Flow daVinci [1510].
Sverdrup, Stommel, and Munk Theories of the Gulf Stream
The Standard, RNG, and Realizable k- Models. The major differences in the models are as follows: the method of calculating turbulent viscosity the turbulent.
Objective Introduce Reynolds Navier Stokes Equations (RANS)
Introduction to Symmetry Analysis Chapter 2 - Dimensional Analysis
Introduction to the Turbulence Models
Chapter 4 Fluid Mechanics Frank White
Continuum Mechanics (MTH487)
CE 3305 Engineering FLUID MECHANICS
Chapter 9: Differential Analysis of Fluid Flow
Coastal Ocean Dynamics Baltic Sea Research Warnemünde
Reynolds-Averaged Navier-Stokes Equations -- RANS
The k-ε model The k-ε model focuses on the mechanisms that affect the turbulent kinetic energy (per unit mass) k. The instantaneous kinetic energy k(t)
Introduction to Fluid Mechanics
Isotropy Kinetic Energy Spectrum.
Street Canyon Modeling
CFD – Fluid Dynamics Equations
Navier - Stokes Equation
Characteristics of Turbulence:
Turbulent Kinetic Energy (TKE)
Objective Discus Turbulence
Objective Define Reynolds Navier Stokes Equations (RANS)
Turbulent properties:
Presentation transcript:

Introduction to Symmetry Analysis Chapter 13 -Similarity Rules for Turbulent Shear Flows Brian Cantwell Department of Aeronautics and Astronautics Stanford University

Reynolds number invariance

Turbulent kinetic energy spectrum

The Reynolds averaged Navier-Stokes equations Reynolds stresses

Integral length and velocity scales Dissipation scales with production

Derivation of the turbulent kinetic energy equation Momentum and continuity equations Kinetic energy equation - project the momentum equation onto the velocity vector

Decompose the flow into a mean and fluctuating part. Project the mean momentum equation onto the mean velocity vector Subtract

Dissipation of TKE equals production of TKE The turbulent kinetic energy (TKE) transport equation is Consider homogeneous shear flow All gradients of correlations are zero Dissipation of TKE equals production of TKE

Invariant group of the Euler equations

One parameter flows

Temporal similarity rules Reduced equations

Spatial similarity rules - jets Spatial similarity rules - wakes

Reynolds number scaling The idea of an eddy viscosity

Scaling of a turbulent vortex ring

Scaling of a turbulent vortex ring

Integral of the motion - the hydrodynamic impulse

Streamlines and Particle Paths

Recall that the incompressible Navier-Stokes equations are invariant under a group of arbitrary translations in space.

Instantaneous flow field in the wake of a circular cylinder as seen by two observers.

Reduced equations Particle paths Frames of reference

Particle paths in similarity coordinates do not depend on the observer

Fine scale motions responsible for kinetic energy dissipation. Recall Introduce the Taylor microscale

Introduce the Kolmogorov microscales Fine scale velocity gradients Large scale velocity gradients

Turbulent kinetic energy spectrum

Scaling the inertial subrange. Assume The wavenumber of an eddy is essentially the inverse of its length scale.

The TKE as a function of wavenumber should scale as This is the scaling of TKE first postulated by Kolmogoriv in 1941 and seems to agree with measurements in high Reynolds number flows.

Derivation of the turbulent kinetic energy equation

Turbulent kinetic energy equation Momentum and continuity equations Kinetic energy equation - project the momentum equation onto the velocity vector

Viscous and pressure terms Kinetic energy equation

Insert fluctuations and average

Project the mean momentum equation onto the mean velocity vector

Dissipation of TKE equals production of TKE The turbulent kinetic energy (TKE) transport equation is Consider homogeneous shear flow All gradients of correlations are zero Dissipation of TKE equals production of TKE