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Monroe L. Weber- Shirk School of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 March 16, 2022
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Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

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Page 1: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Monroe L. Weber-Shirk School of Civil and

Environmental Engineering

Basic Governing Differential Equations

Basic Governing Differential Equations

CEE 331

April 19, 2023

CEE 331

April 19, 2023

Page 2: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

OverviewOverview

Continuity Equation Navier-Stokes Equation

(a bit of vector notation...) Examples (all laminar flow)

Flow between stationary parallel horizontal plates

Flow between inclined parallel plates Pipe flow (Hagen Poiseuille)

Continuity Equation Navier-Stokes Equation

(a bit of vector notation...) Examples (all laminar flow)

Flow between stationary parallel horizontal plates

Flow between inclined parallel plates Pipe flow (Hagen Poiseuille)

Page 3: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Why Differential Equations? Why Differential Equations?

A droplet of water Clouds Wall jet Hurricane

A droplet of water Clouds Wall jet Hurricane

Page 4: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Conservation of Mass in Differential Equation Form

Conservation of Mass in Differential Equation Form

v x z

xx

yy

z z

FHG

IKJy

y

FHG

IKJy

y

t

y x z t

y x z

Mass flux into differential volume

Mass flux out of differential volume

Rate of change of mass in differential volume

vvy

y

FHG

IKJv

vy

y

FHG

IKJ x z x z

Page 5: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Continuity EquationContinuity Equation

vy

vy t

vy

vy t

Mass flux out of differential volume

vvy

y vy

yvy y

y x z

FHG

IKJ

2 vvy

y vy

yvy y

y x z

FHG

IKJ

2 Higher order termHigher order term

outout inin Rate of mass decreaseRate of mass decrease

vy t

0

vy t

0 1-d continuity equation1-d continuity equation

vvy

y vy

y x z v x zt

y x z

FHG

IKJ

vvy

y vy

y x z v x zt

y x z

FHG

IKJ

Page 6: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

u, v, w are velocities in x, y, and z directions

u, v, w are velocities in x, y, and z directions

Continuity EquationContinuity Equation

0tr

+Ñ× =¶

V

t

u

x

v

y

w

z

af af a f0 3-d continuity equation3-d continuity equation

If density is constant...

ux

vy

wz

0

Vector notationVector notation

0Ñ× =Vor in vector notation

True everywhere! (contrast with CV equations!)True everywhere! (contrast with CV equations!)

divergencedivergence

Page 7: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Continuity IllustratedContinuity Illustrated

ux

vy

wz

0

x

y

What must be happening?

0vy¶¶

0ux¶¶

\< >

Page 8: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

ShearShear

GravityGravityPressurePressure

Navier-Stokes EquationsNavier-Stokes Equations

momentummomentum

Derived by Claude-Louis-Marie Navier in 1827

General Equation of Fluid Motion Based on conservation of ___________ with forces…

____________ ___________________ ___________________

U.S. National Academy of Sciences has made the full solution of the Navier-Stokes Equations a top priority

Derived by Claude-Louis-Marie Navier in 1827

General Equation of Fluid Motion Based on conservation of ___________ with forces…

____________ ___________________ ___________________

U.S. National Academy of Sciences has made the full solution of the Navier-Stokes Equations a top priority

Page 9: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

If _________ then _____

Navier-Stokes Equation

Inertial forces [N/m3], a is Lagrangian acceleration

Pressure gradient (not due to change in elevation)

Shear stress gradient

Navier-Stokes EquationsNavier-Stokes Equations

V r =åa FV r =åa F2pa g Vr r m+ =-Ñ + Ñ2pa g Vr r m+ =-Ñ + Ñ

a a

( )p gr- Ñ + =( )p gr- Ñ + =

2mÑ =V2mÑ =Vdudx

t m=dudx

t m=

Is acceleration zero when dV/dt = 0?

t m= ÑVt m= ÑV

( ) 2pa g Vr r m=- Ñ + + Ñ( ) 2pa g Vr r m=- Ñ + + Ñg is constanta is a function of t, x, y, z

NO!

0p rÑ + ¹g 0p rÑ + ¹g 0V ¹ 0V ¹

Page 10: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Lagrangian accelerationLagrangian acceleration

Notation: Total DerivativeEulerian Perspective

Notation: Total DerivativeEulerian Perspective

u v wt x y z

¶ ¶ ¶ ¶= + + +¶ ¶ ¶ ¶V V V V

a u v wt x y z

¶ ¶ ¶ ¶= + + +¶ ¶ ¶ ¶V V V V

a

( , , , )D

t x y z u v wDt t x y za a a a a¶ ¶ ¶ ¶

= + + +¶ ¶ ¶ ¶

( , , , )D

t x y z u v wDt t x y za a a a a¶ ¶ ¶ ¶

= + + +¶ ¶ ¶ ¶

( , , , )D

t x y z u v wDt t x y z

¶ ¶ ¶ ¶= + + +¶ ¶ ¶ ¶

V V V V V( , , , )

Dt x y z u v w

Dt t x y z¶ ¶ ¶ ¶

= + + +¶ ¶ ¶ ¶

V V V V V

tV

a V V¶

= + ×ѶtV

a V V¶

= + ×Ѷ

kjizyx

()()()

() kjizyx

()()()

()

( ) () () ()() u v w

x y z¶ ¶ ¶

×Ñ = + +¶ ¶ ¶

V( ) () () ()() u v w

x y z¶ ¶ ¶

×Ñ = + +¶ ¶ ¶

V

( , , , )D dt dx dy dz

t x y zDt t dt x dt y dt z dta a a a a¶ ¶ ¶ ¶

= + + +¶ ¶ ¶ ¶

( , , , )D dt dx dy dz

t x y zDt t dt x dt y dt z dta a a a a¶ ¶ ¶ ¶

= + + +¶ ¶ ¶ ¶

Total derivative (chain rule)

Material or substantial derivative

Page 11: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

x2 1VVV =D - =2 1VVV =D - =

tV

a V V¶

= + ×ѶtV

a V V¶

= + ×Ѷ

Over what time did this change of velocity occur (for a particle of fluid)? x

tVD

D =x

tVD

D =

space tV

a =DD

=space tV

a =DD

=V

Vx

DDV

Vx

DD

1V1V 2V2V

VDVD

111111 VVM QAV 111111 VVM QAV

222222 VVM QAV 222222 VVM QAV

( )1 2 AVM M Vr+ = D( )1 2 AVM M Vr+ = D

Why no term?tV¶¶tV¶¶

N-S

Page 12: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Application of Navier-Stokes Equations

Application of Navier-Stokes Equations

The equations are nonlinear partial differential equations

No full analytical solution exists The equations can be solved for several

simple flow conditions Numerical solutions to Navier-Stokes

equations are increasingly being used to describe complex flows.

The equations are nonlinear partial differential equations

No full analytical solution exists The equations can be solved for several

simple flow conditions Numerical solutions to Navier-Stokes

equations are increasingly being used to describe complex flows.

Page 13: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

( )0 p gr=- Ñ +( )0 p gr=- Ñ +

Navier-Stokes Equations: A Simple Case

Navier-Stokes Equations: A Simple Case

No acceleration and no velocity gradients No acceleration and no velocity gradients

p gy Cr=- +p gy Cr=- +

p grÑ =-p grÑ =-

x y z

p p pg g g

x y zr r r

¶ ¶ ¶=- =- =-

¶ ¶ ¶x y z

p p pg g g

x y zr r r

¶ ¶ ¶=- =- =-

¶ ¶ ¶

0 0p p p

gx y z

r¶ ¶ ¶

= =- =¶ ¶ ¶

0 0p p p

gx y z

r¶ ¶ ¶

= =- =¶ ¶ ¶

xyz could have any orientation

Let y be vertical upward

g

For constant

( ) 2pa g Vr r m=- Ñ + + Ñ( ) 2pa g Vr r m=- Ñ + + Ñ

Page 14: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Infinite Horizontal Plates: Laminar Flow

Infinite Horizontal Plates: Laminar Flow

( ) 2pa g Vr r m=- Ñ + + Ñ

( ) 20 p g Vr m=- Ñ + + Ñ

Derive the equation for the laminar, steady, uniform flow between infinite horizontal parallel plates.

2

20p ux y

mæ ö¶ ¶

=- + ç ÷è ø¶ ¶

0p

gy

=- -¶

0 0

2 2 2

2 2 20 y

p v v vg

y x y zr m

æ ö¶ ¶ ¶ ¶=- - + + +ç ÷è ø¶ ¶ ¶ ¶

2 2 2

2 2 20 z

p w w wg

z x y zr m

æ ö¶ ¶ ¶ ¶=- - + + +ç ÷è ø¶ ¶ ¶ ¶

2 2 2

2 2 20 x

p u u ug

x x y zr m

æ ö¶ ¶ ¶ ¶=- - + + +ç ÷è ø¶ ¶ ¶ ¶

y

x

Hydrostatic in yHydrostatic in y0v =

0w =

x

y

z

Page 15: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Infinite Horizontal Plates: Laminar Flow

Infinite Horizontal Plates: Laminar Flow

2

20p ux y

mæ ö¶ ¶

=- + ç ÷è ø¶ ¶

2

20p ux y

mæ ö¶ ¶

=- + ç ÷è ø¶ ¶

2

2

dp d udx dy

mæ ö

= ç ÷è ø

2

2

dp d udx dy

mæ ö

= ç ÷è ø

2

2

dp d udy dy

dx dym

óóôôô ôõ õ

æ ö= ç ÷è ø

2

2

dp d udy dy

dx dym

óóôôô ôõ õ

æ ö= ç ÷è ø

dp duy A

dx dymæ ö

+ = ç ÷è ødp du

y Adx dy

mæ ö

+ = ç ÷è ø

dp duy A dy dy

dx dym

óóôô

ô ôõ õ

æ öé ù+ = ç ÷ê ú è øë û

dp duy A dy dy

dx dym

óóôô

ô ôõ õ

æ öé ù+ = ç ÷ê ú è øë û

2

2y dp

Ay B udx

m+ + =2

2y dp

Ay B udx

m+ + =

Pressure gradient in x balanced by shear gradient in yPressure gradient in x balanced by shear gradient in y

dudy

t m=dudy

t m=

ddyt

=ddyt

=

No a so forces must balance!

Now we must find A and B… Boundary Conditions

Page 16: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

negativenegative

Infinite Horizontal Plates: Boundary Conditions

Infinite Horizontal Plates: Boundary Conditions

No slip condition

u = 0 at y = 0 and y = au = 0 at y = 0 and y = a a

B 0

a dpdx

Aa2

20 A

a dpdx

2

( )2

y y a dpu

dxm-

=2a dp

ydx

t æ ö= -è ø2

a dpy

dxt æ ö= -

è ø

y

du dpy A

dy dxmæ ö

= +ç ÷è ødu dp

y Ady dx

mæ ö

= +ç ÷è ø

dpdx

dpdx

let be___________

uu

2

2y dp

Ay B udx

m+ + =

What can we learn about ?

x

Page 17: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Laminar Flow Between Parallel Plates

Laminar Flow Between Parallel Plates

2pa g Vr r m=- - Ñ + Ñ

20 pg Vr m=- - Ñ + Ñ

2

20 x

p ug

x yr m

æ ö¶ ¶=- - + ç ÷è ø¶ ¶

2 2 2

2 2 20 x

p u u ug

x x y zr m

æ ö¶ ¶ ¶ ¶=- - + + +ç ÷è ø¶ ¶ ¶ ¶

U

a

u

y

x

No fluid particles No fluid particles are acceleratingare accelerating

Write the x-componentWrite the x-component

Page 18: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Flow between Parallel Plates Flow between Parallel Plates

2

20 x

p ug

x yr m

æ ö¶ ¶=- - + ç ÷è ø¶ ¶

2

20 x

dp d ug

dx dyr m

æ ö=- - + ç ÷è ø

General equation describing laminar General equation describing laminar flow between parallel plates with the flow between parallel plates with the only velocity in the x directiononly velocity in the x direction

u is only a function of y

ˆxg g i= ×

2

2 x

d u dpg

dy dxm ræ ö

= +ç ÷è ø

Page 19: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Flow Between Parallel Plates: Integration

Flow Between Parallel Plates: Integration

2

2 x

d u dpg

dy dxm r= +

2

2 x

d u dpg

dy dxm r= +

x

du dpy g A

dy dxm ræ ö= + + =

è øx

du dpy g A

dy dxm ræ ö= + + =

è ø

2

2 x

d u dpdy g dy

dy dxm ræ ö= +

è øó ó

ôôõõ

2

2 x

d u dpdy g dy

dy dxm ræ ö= +

è øó ó

ôôõõ

x

du dpdy y g A dy

dy dxm ræ öæ ö= + +ç ÷è øè ø

óóô ôõ õ

x

du dpdy y g A dy

dy dxm ræ öæ ö= + +ç ÷è øè ø

óóô ôõ õ

2

2 x

y dpu g Ay B

dxm ræ ö= + + +

è ø

2

2 x

y dpu g Ay B

dxm ræ ö= + + +

è ø

U

a

u

y

x

tt

Page 20: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

u = U at y = a

Boundary ConditionsBoundary Conditions

2

2 x

y dpu g Ay B

dxm ræ ö= + + +

è ø

2

2 x

y dpu g Ay B

dxm ræ ö= + + +

è ø

Boundary condition

B 000 B 000

Boundary condition

2

2 x

a dpU g Aa

dxm ræ ö= + +

è ø

2

2 x

a dpU g Aa

dxm ræ ö= + +

è ø 2 x

U a dpA g

a dxm

ræ ö= - +è ø2 x

U a dpA g

a dxm

ræ ö= - +è ø

2

2 x

Uy y ay dpu g

a dxr

m- æ ö= + +

è ø

2

2 x

Uy y ay dpu g

a dxr

m- æ ö= + +

è ø

u = 0 at y = 0

Page 21: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Discharge per unit width!

DischargeDischarge

2

00

2

aa

x

y y ay dpq udy U g dy

a dxr

mæ ö- æ ö= = + +ç ÷è øè ø

óôõ

ò2

00

2

aa

x

y y ay dpq udy U g dy

a dxr

mæ ö- æ ö= = + +ç ÷è øè ø

óôõ

ò

3

2 12 x

Ua a dpq g

dxr

mæ ö= - +è ø

3

2 12 x

Ua a dpq g

dxr

mæ ö= - +è ø

2

2 x

y y ay dpu U g

a dxr

m- æ ö= + +

è ø

2

2 x

y y ay dpu U g

a dxr

m- æ ö= + +

è ø

Page 22: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: Oil SkimmerExample: Oil Skimmer

An oil skimmer uses a 5 m wide x 6 m long moving belt above a fixed platform (=60º) to skim oil off of rivers (T=10 ºC). The belt travels at 3 m/s. The distance between the belt and the fixed platform is 2 mm. The belt discharges into an open container on the ship. The fluid is actually a mixture of oil and water. To simplify the analysis, assume crude oil dominates. Find the discharge and the power required to move the belt.

An oil skimmer uses a 5 m wide x 6 m long moving belt above a fixed platform (=60º) to skim oil off of rivers (T=10 ºC). The belt travels at 3 m/s. The distance between the belt and the fixed platform is 2 mm. The belt discharges into an open container on the ship. The fluid is actually a mixture of oil and water. To simplify the analysis, assume crude oil dominates. Find the discharge and the power required to move the belt.

hl

= 1x10-2 Ns/m2

= 860 kg/m3 60ºxg

Page 23: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: Oil SkimmerExample: Oil Skimmer

dpdx

=dpdx

= ˆ cos(60) 0.5xg g g= ×= =g i cos(60) 0.5xg g g= ×= =g i

m 0.002a m 0.002a m/s 3U m/s 3U

( ) ( ) ( ) ( )3

2 3-2 2

(3 m/s)(0.002 m) (0.002 m)0.5 9.806 m/s 860 kg/m )

2 12 1x10 N s/mq = -

×( ) ( ) ( ) ( )3

2 3-2 2

(3 m/s)(0.002 m) (0.002 m)0.5 9.806 m/s 860 kg/m )

2 12 1x10 N s/mq = -

×

In direction of beltq = 0.0027 m2/s (per unit width)

Q = 0.0027 m2/s (5 m) = 0.0136 m3/s

3

2 12 x

Ua a dpq g

dxr

mæ ö= - +è ø 00

dominatesdominates

60ºxg

Page 24: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

How do we get the power requirement? ___________________________

What is the force acting on the belt? ___________________________

Remember the equation for shear? _____________ Evaluate at y = a.

How do we get the power requirement? ___________________________

What is the force acting on the belt? ___________________________

Remember the equation for shear? _____________ Evaluate at y = a.

Example: Oil Skimmer Power Requirements

Example: Oil Skimmer Power Requirements

x

du dpy g A

dy dxm ræ ö= + +

è øx

du dpy g A

dy dxm ræ ö= + +

è ø 2 x

U a dpA g

a dxm

ræ ö= - +è ø2 x

U a dpA g

a dxm

ræ ö= - +è ø

2 x

a dp Uy g

dx am

t ræ öæ ö= - + +è øè ø2 x

a dp Uy g

dx am

t ræ öæ ö= - + +è øè ø

Power = Force x Velocity [N·m/s]

Shear force (·L · W)

=(du/dy)

Page 25: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: Oil Skimmer Power Requirements

Example: Oil Skimmer Power Requirements

2 x

a dp Uy g

dx am

t ræ öæ ö= - + +è øè ø2 x

a dp Uy g

dx am

t ræ öæ ö= - + +è øè ø

cos 602a U

gam

t r= +cos 602a U

gam

t r= +

cos 60x

dpg g

dxr ræ ö+ =è ø

cos 60x

dpg g

dxr ræ ö+ =è ø

( ) ( ) ( )( )

22

23 2

3 m N s1x10

0.002 m 860 kg Ns m9.8 m/s 0.5 19.2 2 m 0.002 m m

t

- ×æ öæ öè øè øæ ö= + =

è ø( ) ( ) ( )

( )

22

23 2

3 m N s1x10

0.002 m 860 kg Ns m9.8 m/s 0.5 19.2 2 m 0.002 m m

t

- ×æ öæ öè øè øæ ö= + =

è ø

Power LWUt=Power LWUt=

sm 3

m 5m 6mN

19.2Power 2

sm 3

m 5m 6mN

19.2Power 2

(shear by belt on fluid)

= 3.46 kW

FVFV

How could you reduce the power requirement? __________Decrease

Page 26: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Potential and kinetic energy

Heating the oil (thermal energy)

Example: Oil Skimmer Where did the Power Go?

Example: Oil Skimmer Where did the Power Go?

Where did the energy input from the belt go?

Where did the energy input from the belt go?

h = 3 m

P Qhg=P Qhg=

m 3s

m0.0136

mN

84303

3

P m 3

sm

0.0136mN

84303

3

P

W443P W443P

Page 27: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Velocity ProfilesVelocity Profiles

-2

-1

0

1

2

3

0 0.0005 0.001 0.0015 0.002

y (m)

u (m

/s)

oil

water

2

2 x

y y ay dpu U g

a dxm m r

- æ ö= + +è ø

2

2 x

y y ay dpu U g

a dxm m r

- æ ö= + +è ø

Pressure gradients and gravity have the same effect.

In the absence of pressure gradients and gravity the velocity profile is ________linear

Page 28: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: No flowExample: No flow

Find the velocity of a vertical belt that is 5 mm from a stationary surface that will result in no flow of glycerin at 20°C (= 0.62 Ns/m2 and =12300 N/m3)

Find the velocity of a vertical belt that is 5 mm from a stationary surface that will result in no flow of glycerin at 20°C (= 0.62 Ns/m2 and =12300 N/m3)

Page 29: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Laminar Flow through Circular Tubes

Laminar Flow through Circular Tubes

Different geometry, same equation development (see Young, et al. p 253)

Apply equation of motion to cylindrical sleeve (use cylindrical coordinates)

Different geometry, same equation development (see Young, et al. p 253)

Apply equation of motion to cylindrical sleeve (use cylindrical coordinates)

Page 30: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Max velocity when r = 0

Laminar Flow through Circular Tubes: Equations

Laminar Flow through Circular Tubes: Equations

2 2

4l x

r R dpv g

dxr

m- æ ö= +

è ø

2 2

4l x

r R dpv g

dxr

m- æ ö= +

è ø

2

max 4 x

R dpv g

dxr

mæ ö=- +è ø

2

max 4 x

R dpv g

dxr

mæ ö=- +è ø

2

8 x

R dpV g

dxr

mæ ö=- +è ø

2

8 x

R dpV g

dxr

mæ ö=- +è ø

4

8 x

R dpQ g

dxp

rmæ ö=- +è ø

4

8 x

R dpQ g

dxp

rmæ ö=- +è ø

Velocity distribution is paraboloid of revolution therefore _____________ _____________

Q = VA =

average velocity (V) is 1/2 vmax

VR2

R is radius of the tubeR is radius of the tube

Page 31: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Laminar Flow through Circular Tubes: Diagram

Laminar Flow through Circular Tubes: Diagram

Velocity

Shear (wall on fluid)2

lx

dv r dpg

dr dxr

mæ ö= +è ø2

lx

dv r dpg

dr dxr

mæ ö= +è ø

2l

x

dv r dpg

dr dxt m ræ ö= = +

è ø2l

x

dv r dpg

dr dxt m ræ ö= = +

è ø

2lghr

lr

t æ ö=-è ø2

lghrl

rt æ ö=-

è ø l

dhl

40

l

dhl

40

True for Laminar or Turbulent flow

Shear at the wallShear at the wall

Laminar flow

2 2

4l x

r R dpv g

dxr

m- æ ö= +

è ø

2 2

4l x

r R dpv g

dxr

m- æ ö= +

è ø

Next slide!

Page 32: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

cv energy equation

Relationship between head loss and pressure gradient for pipesRelationship between head loss and pressure gradient for pipes

1 21 2

1 2l

p pz z h

g gr r+ = + +1 2

1 21 2

l

p pz z h

g gr r+ = + + Constant cross section

2 21 1 2 2

1 1 2 21 22 2p t l

p V p Vz H z H h

g g g ga a

r r+ + + = + + + +

( ) ( )2 1 2 1lgh p p gz gzr r r=- - - -( ) ( )2 1 2 1lgh p p gz gzr r r=- - - -

lh p zg g

x x xr r

D D=- -

D D Dlh p z

g gx x x

r rD D

=- -D D D

lx

h pg g

x xr r

Dæ ö=- +è øD D

lx

h pg g

x xr r

Dæ ö=- +è øD D

lx

h dpg g

l dxr ræ ö=- +

è øl

x

h dpg g

l dxr ræ ö=- +

è ø

l is distance between control surfaces (length of the pipe)

In the energy equation the z axis is tangent to g

x is in tangent to V

x

zg g

xD

=D

xz

Page 33: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

The Hagen-Poiseuille EquationThe Hagen-Poiseuille Equation

4

128lhD

Ql

gpm

=4

128lhD

Ql

gpm

=2

32lhD

Vl

gm

=2

32lhD

Vl

gm

=

Hagen-Poiseuille Laminar pipe flow equations4

8 x

R dpQ g

dxp

rmæ ö=- +è ø

4

8 x

R dpQ g

dxp

rmæ ö=- +è ø

From Navier-Stokes

4

8lhR

Q gl

pr

mæ ö=- -è ø

4

8lhR

Q gl

pr

mæ ö=- -è ø

lx

h dpg g

l dxr ræ ö=- +

è øl

x

h dpg g

l dxr ræ ö=- +

è øRelationship between head loss and pressure gradient

What happens if you double the pressure gradient in a horizontal tube? ____________flow doubles

V is average velocity

Page 34: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: Laminar Flow (Team work)

Example: Laminar Flow (Team work)

Calculate the discharge of 20ºCwater through a long vertical section of 0.5 mm ID hypodermic tube. The inlet and outlet pressures are both atmospheric. You may neglect minor losses. What is the total shear force?

What assumption did you make? (Check your assumption!)

Calculate the discharge of 20ºCwater through a long vertical section of 0.5 mm ID hypodermic tube. The inlet and outlet pressures are both atmospheric. You may neglect minor losses. What is the total shear force?

What assumption did you make? (Check your assumption!)

Page 35: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

SummarySummary

Navier-Stokes Equations and the Continuity Equation describe complex flow including turbulence

The Navier-Stokes Equations can be solved analytically for several simple flows

Numerical solutions are required to describe turbulent flows

Page 36: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

GlycerinGlycerin

3

2 12 y

Ua a dpQ g

dyr

mæ ö

= - +ç ÷è ø3

02 12

Ua a grm

= -

y

dpg g

dyr r+ =

2

6a g

Urm

=

Um N m

Ns mm s

0 005 12300

6 0 620 083

2 3

2

. /

. /. /

a fc hc h

RVl kg m m s m

Ns m

1254 0 083 0 005

0 620 8

3

2

/ . / .

. /.

c ha fa f

y

Page 37: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Example: Hypodermic Tubing Flow

Example: Hypodermic Tubing Flow

QD h

Ll

4

128

QN m m

x Ns m

9806 0 0005

128 1 10

3 4

3 2

/ .

/

c hafa fc h

Q x m s 158 10 8 3. /

VQd

4

2V m s 0 0764. /

RVd

Rm s m kg m

x Ns m

0 0764 0 0005 1000

1 10

3

3 2

. / . /

/

a fa fc hc h

R 38

Q L s 158. /

ldhl

40

ldhl

40

ldhrl

F lshear 4

2 l

dhrlF l

shear 42

2shear lF r hp g=- 2shear lF r hp g=-

= weight!

pz

Vg

Hp

zV

gH hp t l

1

11 1

12

2

22 2

22

2 2

Page 38: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Euler’s Equation Along a Streamline

Euler’s Equation Along a Streamline

va 2 phg va 2 phg

xp

xh

gxu

utu

xp

xh

gxu

utu

phg a phg a

Inviscid flow (frictionless)

x along a streamline

v = u = velocity in x direction

Velocity normal to streamline is zero

u v w g h pt x y z

r r¶ ¶ ¶ ¶é ù

+ + + =- Ñ - Ñê ú¶ ¶ ¶ ¶ë û

V V V Vu v w g h p

t x y zr r¶ ¶ ¶ ¶é ù

+ + + =- Ñ - Ñê ú¶ ¶ ¶ ¶ë û

V V V V

Page 39: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Euler’s EquationEuler’s Equation

xp

xh

gxu

u

1

xp

xh

gxu

u

1

01

dxdp

dxdh

gdxdu

u

01

dxdp

dxdh

gdxdu

u

0 udugdhdp

0 udugdhdp

(Multiplying by dx converts from a force balance equation to an energy equation)

xp

xh

gxu

utu

xp

xh

gxu

utu

We’ve assumed: frictionless and along a streamline

SteadySteady

Euler’s equation along a streamline

x is the only independent variable

Page 40: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Bernoulli EquationBernoulli Equation

0 udugdhdp

0 udugdhdp

Euler’s equation

01 udugdhdp

01 udugdhdp

constant2

2

vgh

p

constant2

2

vgh

p

constant2

2

g

vh

p

constant2

2

g

vh

p

The Bernoulli Equation is a statement of the conservation of ____________________

constant2

2

vgh

p

constant2

2

vgh

p

Integrate for constant density

Bernoulli Equation

Mechanical Energy p.e. k.e.

Page 41: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Hydrostatic Normal to Streamlines?

Hydrostatic Normal to Streamlines?

phgz

wy

vx

ut

vvvvphg

zw

yv

xu

t

vvvv

xp

xh

gxu

utu

xp

xh

gxu

utu

y

p

y

hg

0y

p

y

hg

0 dhdp dhdp

y

p

y

hg

z

vw

y

vv

x

vu

t

v

y

p

y

hg

z

vw

y

vv

x

vu

t

v

y, v perpendicular to streamline (v = 0)

x, u along streamline

Page 42: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Laminar Flow between Parallel Plates

Laminar Flow between Parallel Plates

U

l

a

uy

lyy

lyy

yllp

p

yl

lp

p

ypyp

ll

yl yl

sinyl sinyl

y

h

l

Page 43: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Equation of Motion: Force Balance

Equation of Motion: Force Balance

lyy

lyy

yllp

p

yl

lp

p

ypyp

ll

yl yl

sinyl sinyl

ypyp

yllp

p

yl

lp

p

ll

lyy

lyy

maF maF

sinyl sinyl

00

pressure

shear

gravity

acceleration

+

-

-

+

+

= l

Page 44: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

Equation of MotionEquation of Motion

0sin

ylp

0sin

ylp

lh

sinlh

sin

lh

lp

y

lh

lp

y

hp

ly

hp

ly

hp

dld

dyd hp

dld

dyd

dydu dydu 2

2

dyud

dyd 2

2

dyud

dyd

But

h

l

Laminar flow assumption!Laminar flow assumption!

0sin

ylly

ylyl

lp

pyp 0sin

ylly

ylyl

lp

pyp

Page 45: Monroe L. Weber-Shirk S chool of Civil and Environmental Engineering Basic Governing Differential Equations CEE 331 July 14, 2015 CEE 331 July 14, 2015.

U

a

u

Limiting casesLimiting cases

( )2

2y y ay d

u U p ha dx

gm-

= + +( )2

2y y ay d

u U p ha dx

gm-

= + +

Both plates stationary

Hydrostatic pressure ( ) 0d

p hdx

g+ =( ) 0d

p hdx

g+ =

aUy

u a

Uyu

0U 0U

( )2

2y ay d

u p hdx

gm-

= +( )2

2y ay d

u p hdx

gm-

= +

Linear velocity distribution

Parabolic velocity distribution

Motion of plate

Pressure gradient

y

x