Answers to Homework #9

Similar documents
Computational Fluid Dynamics 2

Turbulence (January 7, 2005)

Eddy viscosity. AdOc 4060/5060 Spring 2013 Chris Jenkins. Turbulence (video 1hr):

Governing Equations for Turbulent Flow

Fundamental Concepts of Convection : Flow and Thermal Considerations. Chapter Six and Appendix D Sections 6.1 through 6.8 and D.1 through D.

Exercises in Combustion Technology

LES of Turbulent Flows: Lecture 3

Chapter 7. Basic Turbulence

DAY 19: Boundary Layer

Lecture 2. Turbulent Flow

External Forced Convection. Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display.

Introduction to Turbulence and Turbulence Modeling

6. Laminar and turbulent boundary layers

TURBULENCE IN FLUIDS AND SPACE PLASMAS. Amitava Bhattacharjee Princeton Plasma Physics Laboratory, Princeton University

Applied Computational Fluid Dynamics

Principles of Convection

Turbulence - Theory and Modelling GROUP-STUDIES:

AER1310: TURBULENCE MODELLING 1. Introduction to Turbulent Flows C. P. T. Groth c Oxford Dictionary: disturbance, commotion, varying irregularly

7.6 Example von Kármán s Laminar Boundary Layer Problem

Isotropic homogeneous 3D turbulence

Physical Properties of Fluids

Project Topic. Simulation of turbulent flow laden with finite-size particles using LBM. Leila Jahanshaloo

Masters in Mechanical Engineering. Problems of incompressible viscous flow. 2µ dx y(y h)+ U h y 0 < y < h,

Masters in Mechanical Engineering Aerodynamics 1 st Semester 2015/16

Note the diverse scales of eddy motion and self-similar appearance at different lengthscales of the turbulence in this water jet. Only eddies of size

Turbulent energy density and its transport equation in scale space

Summary of Dimensionless Numbers of Fluid Mechanics and Heat Transfer

Tutorial School on Fluid Dynamics: Aspects of Turbulence Session I: Refresher Material Instructor: James Wallace

Chapter 7: External Forced Convection

ESCI 485 Air/sea Interaction Lesson 2 Turbulence Dr. DeCaria

Chapter 7: External Forced Convection. Dr Ali Jawarneh Department of Mechanical Engineering Hashemite University

Before we consider two canonical turbulent flows we need a general description of turbulence.

An Introduction to Theories of Turbulence. James Glimm Stony Brook University

Numerical Heat and Mass Transfer

Small-Scale Statistics and Structure of Turbulence in the Light of High Resolution Direct Numerical Simulation

FLUID MECHANICS PROF. DR. METİN GÜNER COMPILER

CHAPTER 4 BOUNDARY LAYER FLOW APPLICATION TO EXTERNAL FLOW

BAE 820 Physical Principles of Environmental Systems

Generated by CamScanner from intsig.com

MOMENTUM TRANSPORT Velocity Distributions in Turbulent Flow

LECTURE 1 THE CONTENTS OF THIS LECTURE ARE AS FOLLOWS:

Simulating Drag Crisis for a Sphere Using Skin Friction Boundary Conditions

Quantum Turbulence, and How it is Related to Classical Turbulence

Energy spectrum of isotropic magnetohydrodynamic turbulence in the Lagrangian renormalized approximation

External Flow and Boundary Layer Concepts

Outlines. simple relations of fluid dynamics Boundary layer analysis. Important for basic understanding of convection heat transfer

Multiscale Computation of Isotropic Homogeneous Turbulent Flow

MHD turbulence in the solar corona and solar wind

Unit operations of chemical engineering

PIPE FLOW. General Characteristic of Pipe Flow. Some of the basic components of a typical pipe system are shown in Figure 1.

Chapter 7 The Time-Dependent Navier-Stokes Equations Turbulent Flows

Isotropic homogeneous 3D turbulence

Fluid Mechanics. Chapter 9 Surface Resistance. Dr. Amer Khalil Ababneh

Modeling of turbulence in stirred vessels using large eddy simulation

Table of Contents. Foreword... xiii. Preface... xv

Boundary layer flows The logarithmic law of the wall Mixing length model for turbulent viscosity

Turbulence. 2. Reynolds number is an indicator for turbulence in a fluid stream

Problem 4.3. Problem 4.4

Dynamics and Statistics of Quantum Turbulence in Quantum Fluid

Laminar Flow. Chapter ZERO PRESSURE GRADIENT

6 VORTICITY DYNAMICS 41

Signature: (Note that unsigned exams will be given a score of zero.)

FORMULA SHEET. General formulas:

UNIT II CONVECTION HEAT TRANSFER

150A Review Session 2/13/2014 Fluid Statics. Pressure acts in all directions, normal to the surrounding surfaces

Chapter 1: Basic Concepts

HEAT TRANSFER BY CONVECTION. Dr. Şaziye Balku 1

UNIT II Real fluids. FMM / KRG / MECH / NPRCET Page 78. Laminar and turbulent flow

B.1 NAVIER STOKES EQUATION AND REYNOLDS NUMBER. = UL ν. Re = U ρ f L μ

Direct numerical simulation of forced MHD turbulence at low magnetic Reynolds number

Turbulent Rankine Vortices

CEE 3310 Dimensional Analysis & Similitude, Oct. 22,

Turbulence: Basic Physics and Engineering Modeling

Figure 3: Problem 7. (a) 0.9 m (b) 1.8 m (c) 2.7 m (d) 3.6 m

Phone: , For Educational Use. SOFTbank E-Book Center, Tehran. Fundamentals of Heat Transfer. René Reyes Mazzoco

Direct and Large Eddy Simulation of stably stratified turbulent Ekman layers

Turbulence models and excitation of solar oscillation modes

OUTCOME 2 - TUTORIAL 1

The lattice Boltzmann equation (LBE) has become an alternative method for solving various fluid dynamic

Chapter 10. Solids and Fluids

Turbulentlike Quantitative Analysis on Energy Dissipation in Vibrated Granular Media

Subgrid models for large-eddy simulation using unstructured grids in a stabilized finite element framework

ROLE OF LARGE SCALE MOTIONS IN TURBULENT POISEUILLE AND COUETTE FLOWS

2 GOVERNING EQUATIONS

What s important: viscosity Poiseuille's law Stokes' law Demo: dissipation in flow through a tube

CHME 302 CHEMICAL ENGINEERING LABOATORY-I EXPERIMENT 302-V FREE AND FORCED CONVECTION

ENGR Heat Transfer II

ESS Turbulence and Diffusion in the Atmospheric Boundary-Layer : Winter 2017: Notes 1

primitive equation simulation results from a 1/48th degree resolution tell us about geostrophic currents? What would high-resolution altimetry

meters, we can re-arrange this expression to give

Frictional Losses in Straight Pipe

Predicting natural transition using large eddy simulation

Mass Transfer in Turbulent Flow

CONVECTIVE HEAT TRANSFER

A two-fluid model of turbulent two-phase flow for simulating turbulent stratified flows

Turbulent Boundary Layers & Turbulence Models. Lecture 09

Active Control of Separated Cascade Flow

Turbulent drag reduction by streamwise traveling waves

Scale interactions and scaling laws in rotating flows at moderate Rossby numbers and large Reynolds numbers

ME 431A/538A/538B Homework 22 October 2018 Advanced Fluid Mechanics

Transcription:

Answers to Homework #9 Problem 1: 1. We want to express the kinetic energy per unit wavelength E(k), of dimensions L 3 T 2, as a function of the local rate of energy dissipation ɛ, of dimensions L 2 T 3 (velocity square per unit time) and of the wavenumber k (dimension L 1 ). To eliminate the time dimension, divide E(k) by ɛ 2/3 : E(k)/ɛ 2/3 now has dimension L 3 4/3 = L 5/3. Therefore E(k)k 5/3 /ɛ 2/3 is a dimensionless parameter. This can be written: E(k) ɛ 2/3 k 5/3. This seemingly simple relation, usually called Kolmogorov s 5/3 law, is an excellent illustration of the power of dimensional analysis. It is verified experimentally, as shown on the figure below. Note that some assumptions are required to justify that E(k) should only depend on ɛ and k (and not on viscosity or on the length scale of the problem). These assumptions originate from the idea of a turbulent energy cascade: energy is injected into the flow at a macroscopic length scale, and is dissipated at small scales by viscosity; between these two scales there exists an energy cascade by which the kinetic energy of the large turbulent eddies is transfered to smaller eddies at a constant dissipation rate ɛ. It is in this intermediate range, called inertial subrange, that the 5/3 law is valid. 1

2. Again, use dimensional analysis. The dimensions of ν t are L 2 /T. It is straightforward to see that from ν t, (length) and ɛ the following dimensionless parameter can be constructed: Π = ν t /(ɛ 1/3 4/3 ). Therefore: ν t ɛ 1/3 4/3. 3. E(k) is the kinetic energy density per unit wavenumber (and per unit mass). To obtain the total amount of kinetic energy contained in all the filtered out eddies (i.e. in all the wavenumber k ), integrate E(k) from to infinity: [ ] k 2/3 K(k ) and since = 2π/, Problem 2: E(k)dk = ɛ 2/3 k 5/3 dk = ɛ 2/3 K( ) 3 ɛ 2/3 2/3 2 (2π). 2/3 2/3 = 3 2 ɛ 2/3 k 2/3 max 1. We use the following values: L = 1 m, U = 1 m/s, and v = 1.5 10 5 m 2 /s. For the laminar boundary layer (White, pp. 235): δ L 5.0 L ReL 0.0194 m., For the turbulent boundary layer (White, pp. 430): δ T 0.16 x Re 1/7 L 0.033 m. In general, δ L x 1/2 (slow growth, like a parabola), and δ T growth). x 6/7 (almost linear 2. Transition form laminar to turbulent boundary layer occurs near Re x 5 10 5, which in our case corresponds to x 3 m. Unless the boundary layer is tripped, transition will not occur before the end of the plate. 3. The total drag (per unit depth) on the plate is obtained by integrating the wall friction over the length of the plate: D = 1 1 m 2 ρu 2 C f (x)dx. In the laminar case, C f 0.664Re 1/2 x, therefore (using ρ = 1 kg/m 3 ): x=0 D L = 0.664(1.5 10 5 ) 1/2 [ x ] 1 m x=0 2.57 10 3 N/m. In the turbulent case, C f 0.027Rex 1/7, from which: D T = 1 [ ] x 2 0.027(1.5 10 5 ) 1/7 6/7 1 m 3.22 10 3 N/m. 6/7 In general, D L x 1/2, while D T x 6/7. 2 x=0

4. The heat transfer equivalent of the wall friction coefficient is the Stanton number, defined as follows: q w C h = ρuc p (T w T e ). For laminar flow, the Reynolds analogy leads to: C L h C f 2P r 2/3, while for turbulent flow, it can be written (cf. White pp. 485): C T h C f /2 1 + 13(P r 2/3 1)(C f /2) 1/2. These expressions can be used to integrate q w over the length of the plate in order to get the precise heat flux across the surface of the plate. To assess the heat transfer capabilities, let s simply evaluate the Stanton numbers in both cases at x = 1 m; using Re L = 67, 000 and P r = 0.7: C L h 1.63 10 3 and C T h 3.23 10 3 Therefore, the heat transfer capability of the turbulent boundary layer is twice that of the laminar case. 5. If the flow velocity is doubled, the boundary layer thicknesses change as follows: δ L = δ L / 2 0.0137 m, δ T = δ T /2 1/7 0.0299 m. The transition stills occurs at the same Reynolds number. If U is doubled, this means that it occurs at half the original distance, i.e. around 1.5 m (still no transition on the plate). The drag depends on U as U 3/2 in the laminar case, and U 13/7 in the turbulent case, therefore: D L = 23/2 D L 7.27 10 3 N/m, D T = 213/7 D T 1.17 10 2 N/m. The dependence of the heat transfer on U is not as simple for the turbulent case (no simple scaling due to the term involving C f in the denominator). The new values of C h are Ch L 1.15 10 3 and Ch T 2.9 10 3. Note however that the actual heat transfer is obtained by multiplying C h by ρuc p T, which is itself multiplied by 2 when the flow velocity is doubled. 3

Problem 3: (Sangwook Park) (continued on the next page) 4

5