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Convection in Boundary Layers

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Convection in Boundary Layers. P M V Subbarao Associate Professor Mechanical Engineering Department IIT Delhi. A tiny layer but very significant………. Momentum Vs Thermal Effects. n Potential for diffusion of momentum change (Deficit or excess) created by a solid boundary. - PowerPoint PPT Presentation
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Convection in Boundary Layers P M V Subbarao Associate Professor Mechanical Engineering Department IIT Delhi tiny layer but very significant………..
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Page 1: Convection in Boundary Layers

Convection in Boundary Layers

P M V Subbarao

Associate Professor

Mechanical Engineering Department

IIT Delhi

A tiny layer but very significant………..

Page 2: Convection in Boundary Layers

Pr,,Re,

*

**

dx

dpxf L

Prandtl Number: The ratio of momentum diffusion to heat diffusion.

T

m

Pr

Other scales of reference:

Length of plate: L & Free stream velocity : uoo

Potential for diffusion of momentum change (Deficit or excess) created by a solid boundary. Potential for Diffusion of thermal changes created by a solid boundary.

Momentum Vs Thermal Effects

Page 3: Convection in Boundary Layers

0

''

y

s y

TkTThq

0*

0 *scaleLength

scale eTemperatur

yyyy

T

0

**

y

sfluids yL

TTkTTh

Pr,,Re,*

**

0*

* dx

dpxf

k

hL

y Lfluidy

Page 4: Convection in Boundary Layers

This dimensionless temperature gradient at the wall is named asNusselt Number:

resistance Convection

resistance Conduction1

h

kL

k

hLNu fluid

fluid

Pr,,Re,*

**

0*

* dx

dpxf

k

hx

yNu x

fluidy

Local Nusselt Number

Page 5: Convection in Boundary Layers

Average Nusselt Number

avgfluid

avgavg k

LhNu

,

Page 6: Convection in Boundary Layers

Computation of Dimensionless Temperature Profile

First Law of Thermodynamics for A CV

Energy Equation for a CV

How to select A CV for External Flows ?

Relative sizes of Momentum & Thermal Boundary Layers …

T

m

Pr

Page 7: Convection in Boundary Layers

Liquid Metals: Pr <<< 1

y*

1.0u*(y*) y*)

Page 8: Convection in Boundary Layers

Gases: Pr ~ 1.0

y

1.0

u*(y*)

y*)

Page 9: Convection in Boundary Layers

Water :2.0 < Pr < 7.0

y

1.0

u*(y*)

y*)

Page 10: Convection in Boundary Layers

Oils:Pr >> 1

y

1.0

u*(y*)

y*)

Page 11: Convection in Boundary Layers

The Boundary Layer : A Control Volume

For pr < 1

xx uT &dxxdxx uT &

Page 12: Convection in Boundary Layers

CV

CM VdVbt

b

dt

dB

.

Reynolds Transport Theorem

The relation between A CM and CV for conservation of any extensive property B.

• Total rate of change of any extensive property B of a system(C.M.) occupying a control volume C.V. at time t is equal to the sum of

• a) the temporal rate of change of B within the C.V.

• b) the net flux of B through the control surface C.S. that surrounds the C.V.

Page 13: Convection in Boundary Layers

Conservation of Mass

• Let b=1, the B = mass of the system, m.

The rate of change of mass in a control mass should be zero.

CV

CM VdVtdt

dm

.

0.

CV

VdVt

Above integral is true for any shape and size of the control volume, which implies that the integrand is zero.

0.

Vt

Page 14: Convection in Boundary Layers

Conservation of Momentum

• Let b=V, the B = momentum of the system, mV.

The rate of change of momentum for a control mass should be equalto resultant external force.

CV

CM VdVVt

V

dt

Vmd

.

FVdVVt

V

CV

.

bodysurface ffVVt

V

.

Momentum equation of per unit volume:

Page 15: Convection in Boundary Layers

For a boundary layer :

gVVt

Vij ˆ..

For an incompressible flow

gVVt

Vij ˆ..

g

Dt

DVij ˆ.

Page 16: Convection in Boundary Layers

Conservation of Energy

• Let b=e, the B = Energy of the system, me.

The rate of change of energy of a control mass should be equalto difference of work and heat transfers.

CV

CM VdVet

e

dt

dE

.

WQVdVet

e

CV

.

Energy equation per unit volume:

wqVet

e

.

Page 17: Convection in Boundary Layers

Tkq .

Using the law of conduction heat transfer:

The net Rate of work done on the element is:

ijVw ..

From Momentum equation: N S Equations

g

Dt

DVij ˆ.

Page 18: Convection in Boundary Layers

Then

Vg

Dt

DVVV ij .ˆ..

gzV

he 2

2

wqVet

e

.

Page 19: Convection in Boundary Layers

j

iijij x

uVTkVg

Dt

DVV

Dt

Dh ....

j

iij x

uVg

Dt

DVVTkVg

Dt

DVV

Dt

Dh .ˆ..

Substitute the work done by shear stress:

j

iij x

uTk

Dt

Dh .

This is called the first law of thermodynamics for fluid motion.

For an Incompressible fluid:

Page 20: Convection in Boundary Layers

Vpx

u

x

u

j

i

j

iij ij

.'

Dt

DpVp .

Invoking conservation of mass:

j

iij x

uTk

Dt

Dh .

First law for a fluid motion:

0. VDt

D

Page 21: Convection in Boundary Layers

Dt

Dp

x

uTk

Dt

Dh

j

iij

'.

Dt

DpTk

Dt

Dh

.

is called as viscous dissipation.

Dt

DpTk

Dt

DTC p

.

Page 22: Convection in Boundary Layers

Boundary Layer Equations

Consider the flow over a parallel flat plate.

Assume two-dimensional, incompressible, steady flow with constant properties.

Neglect body forces and viscous dissipation.

The flow is nonreacting and there is no energy generation.

Page 23: Convection in Boundary Layers

The governing equations for steady two dimensional incompressible fluid flow with negligible viscous dissipation:

Page 24: Convection in Boundary Layers

Boundary Conditions

Page 25: Convection in Boundary Layers

Scale Analysis

Define characteristic parameters:

L : length

u ∞ : free stream velocity

T ∞ : free stream temperature

Page 26: Convection in Boundary Layers

General parameters:

x, y : positions (independent variables)

u, v : velocities (dependent variables)

T : temperature (dependent variable)

also, recall that momentum requires a pressure gradient for the movement of a fluid:

p : pressure (dependent variable)

Page 27: Convection in Boundary Layers

Define dimensionless variables:

L

xx *

L

yy *

u

uu*

u

vv*

s

s

TT

TT

2*

u

pp

Page 28: Convection in Boundary Layers

Similarity parameters can be derived that relate one set of flow conditions to geometrically similar surfaces for a different set of flow conditions:

Page 29: Convection in Boundary Layers

0*

*

*

*

y

v

x

u

2*

*2

*

*

*

**

*

**

Re

1

y

u

x

p

y

vv

x

uu

L

2*

2

**

**

PrRe

1

yyv

xu

L

Page 30: Convection in Boundary Layers

Boundary Layer Parameters

• Three main parameters (described below) that are used to characterize the size and shape of a boundary layer are:

• The boundary layer thickness,

• The displacement thickness, and

• The momentum thickness.

• Ratios of these thicknesses describe the shape of the boundary layer.

Page 31: Convection in Boundary Layers

Boundary Layer Thickness

• The boundary layer thickness, signified by , is simply the thickness of the viscous boundary layer region.

• Because the main effect of viscosity is to slow the fluid near a wall, the edge of the viscous region is found at the point where the fluid velocity is essentially equal to the free-stream velocity.

• In a boundary layer, the fluid asymptotically approaches the free-stream velocity as one moves away from the wall, so it never actually equals the free-stream velocity.

• Conventionally (and arbitrarily), we define the edge of the boundary layer to be the point at which the fluid velocity equals 99% of the free-stream velocity:

Page 32: Convection in Boundary Layers

• Because the boundary layer thickness is defined in terms of the velocity distribution, it is sometimes called the velocity thickness or the velocity boundary layer thickness.

• Figure  illustrates the boundary layer thickness. There are no general equations for boundary layer thickness.

• Specific equations exist for certain types of boundary layer.

• For a general boundary layer satisfying minimum boundary conditions:

0 ;)( ;0)0(

y

y

uuuu

The velocity profile that satisfies above conditions:

2

22

yy

uu

Page 33: Convection in Boundary Layers

Further analysis shows that:

xx Re

5.5

Where:

xu

xRe

Page 34: Convection in Boundary Layers

Variation of Reynolds numbers

All Engineering Applications

Page 35: Convection in Boundary Layers

Laminar Velocity Boundary Layer

The velocity boundary layer thickness for laminar flow over a flat plate:

as u∞ increases, δ decreases (thinner boundary layer)

The local friction coefficient:

and the average friction coefficient over some distance x:

x

xRe

5.5

Page 36: Convection in Boundary Layers

Laminar Thermal Boundary Layer

022

2

d

df

pr

d

d

Boundary conditions:

1 00

Page 37: Convection in Boundary Layers

This differential equation can be solved by numerical integration.

One important consequence of this solution is that, for pr >0.6:

3/1

0

332.0 prd

d

Local convection heat transfer coefficient:

0

**

y

fluidx yL

kh

0

**

y

sfluids yL

TTkTTh

Page 38: Convection in Boundary Layers

Local Nusselt number:

0

x

ukh fluidx

000

Re

xfluid

xx

xu

x

ux

k

xhNu

3/1Re332.0 prk

xhNu x

fluid

xx

Page 39: Convection in Boundary Layers

Average heat transfer coefficient:

L

xfluid

L

xavg dxprx

k

Ldxh

Lh

0

3/1

0

Re332.011

L

fluidavg

x

dxpr

u

x

k

Lh

0

3/1332.01

xavg hh 2

6.0 Re664.0 3/1 prprk

LhNu L

fluid

avgavg

Page 40: Convection in Boundary Layers

A single correlation, which applies for all Prandtl numbers,Has been developed by Churchill and Ozoe..

100

0468.01

Re338.0

41

32

3/1

xx

x Pe

pr

prNu

xavg NuNu 2

Page 41: Convection in Boundary Layers

Turbulent Flow

• For a flat place boundary layer becomes turbulent at Rex ~ 5 X 105.

• The local friction coefficient is well correlated by an expression of the form

7x

51

, 10Re Re059.0

xxfC

Local Nusselt number: 60 0.6 Re029.0 3/154

prprNu xx

Local Sherwood number: 60 0.6 Re029.0 3/154

ScScSh xx


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