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    Introduction to Turbulent Flows

    Dr. Murat Koksal

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     I am an old man now, and when I die and go to heaven there

    are two matters on which I hope for enlightenment. One isquantum electrodynamics and the other is turbulent motion

    in fluids. And about the former, I am rather optimistic.

    Sir Horace Lamb (1932)

    Turbulence was probably invented by the Devil on the

     seventh day of Creation when the Good Lord wasn’t looking.

    Peter Bradshaw (1994)

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    Outline

    • General characteristics of turbulent flows

    • Movies on turbulent flows

    • Scales of turbulence – Energy Cascade• Turbulence closure problem

    • Turbulence modeling

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    What is turbulent fluid motion?

    “Turbulent fluid motion is an irregular condition of

    flow in which various quantities show a random

    variation with time and space coordinates, so that

    statistically distinct average values can be

    discerned” (Hinze, 1975).

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    Why do we study turbulent flows?

    • Virtually all flows of practical interest are

    turbulent:

     – Flows past airplanes, rockets, ships, automobiles,

     – Flows in chemical reactors, mixers, combustion

    chambers and engines,

     – Flows in oil and gas pipelines, – Boundary layer in earth’s atmosphere, currents in

    oceans, motion of clouds.

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    Historical Background

    • In 1500, Leonardo da Vinci recognized that there weretwo states of fluid motion: regular/ordered vsirregular/disordered. He called the latter as “LaTurbolenza”.

    • In 1839, Hagen rediscovered the two states of fluidmotion in his experiments carried out in a brass pipe.

    • In 1883, Reynolds carried out his famous dye

    experiments and defined the transition to turbulence.

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    Hagen’s Experiments 

    Flow, V

    Horizontal Pipe

    P = ?

    P

    V

    P~V

    P~V1.75

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    Reynolds’s Experiments and Transition to

    Turbulence

    The transition to turbulent flow depends on the

    Reynolds number, Re.

    Re = inertial force/viscous force

    Inertial force ~ u2/l

    Viscous force ~ u/l2

    Re = ul/  = [Velocity Scale][Length Scale] / [Viscosity]

    For a pipe flow: 

    v

     DV 

    ityviskinematic

     Diameter Velocity Average av

    cos

     Re

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    Transitional Re

    For pipe flows, transitional Reynolds number is ~ 2300.

    This value depends on roughness of the pipe, pipe

    entrance conditions and external perturbations such as

    noise and vibration. The transition to turbulence can be

    delayed up to Re = 50, 000.

    We usually consider a pipe flow to be fully turbulent

    when Re > 50, 000.

    For a flow over a flat plate, the transition Reynoldsnumber is ~ 500,000.

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    Why does transition occur?

    • For small enough length scales and low enough velocities, when Re is not too large, viscous forcesoutweigh the inertial forces. Any perturbation is quicklydampened by the viscosity.

    • However, as Re increases, viscous stresses areovercome by fluids inertia and the laminar motionbecomes UNSTABLE. Any perturbation grows quickly,the motion becomes 3-D marked by rapid velocity and

    pressure fluctuations.

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    What is turbulent fluid motion?

    “Turbulent fluid motion is an irregular condition of

    flow in which various quantities show a random

    variation with time and space coordinates, so that

    statistically distinct average values can be

    discerned” (Hinze, 1975).

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    General Characteristics of Turbulent Flows

    • IRREGULARITY: Turbulent flows are described as irregularand random. This is attributed to eddying motion defined aslocal swirling motion where the vorticity can be quite severe.Turbulent eddies appear at a wide RANGE OF SIZES andgive rise to vigorous mixing.

    FLOW

    D      

    Eddies in a typical turbulent pipe flow

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    • LARGE REYNOLDS NUMBER:  Turbulent flows occur atlarge Reynolds numbers as the inertial forces outweigh theviscous forces. 

    • INSTABILITY AND NONLINEARITY: Turbulencedevelops as an instability of laminar flow.

    • DIFFUSIVITY: In turbulent flows, mass, momentum and heattransfer take place at a much larger rate than laminar flows.Reynolds’s dye experiment is a good example of increasedmass transfer as the flow becomes turbulent. Due to enhancedmomentum transfer, turbulent flows experience larger resistancein pipes, on aircraft’s wings and ships’ hulls. On the other hand,

    the delay of separation causes reduction in drag in the case ofbluff bodies.

    General Characteristics of Turbulent Flows

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    Question – Which velocity profile belongs

    to turbulent flow? Why?

    Flow

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    Which one of the below is a turbulent flow?

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    • CONTINUUM: Turbulence is a continuum phenomena. Even,the smallest eddies in a turbulent flow are far larger than

    molecular length scale. 

    • TURBULENT FLOW VS TURBULENT FLUID: Turbulence is the property of flow not the property of the fluid.

     Any fluid flow with a Re > Retr  can become turbulent.

    • DISSIPATION: Turbulent flows consist of a continuousspectrum of scales of eddies from largest to the smallest.Energy is taken from the mean flow by deforming it, istransferred to smaller eddies by means of vortex stretching until

    viscous forces dissipate it. This is known as energy cascade. Without an energy supply, turbulence decays rapidly. 

    General Characteristics of Turbulent Flows

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    Energy Spectrum of Turbulence/

    Scales in Turbulent Flows

    “Big whirls have little whirls that feed on

    their velocity. Little whirls have lesser

    whirls, and so on to viscosity”  Richardson

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    Pipe Flow 

    If D = 10 cm, U = 2 m/s, Re = 80,000

    lt ~ 1.22 mm

    f ~ 80 Hz

    ~ 0.25 m

    f = 1/  ~ 22 600 Hz

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    In summary…. 

    • Turbulence is dominated by large energy bearingeddies. They produce the energy for turbulence by

    shearing the mean flow and they are responsible for

    enhanced mixing.

    • Small eddies dissipate the energy transferred to them

    due to viscous forces. However, the rate of energy

    dissipation is controlled by the rate of energy they

    receive from larger eddies.