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Internat. J. Math. & Math. Sci.

VOL. 17 NO. (1994) 155-164

FLOWS FOR CHOSEN VORTICITY FUNCTIONS-- EXACT SOLUTIONS OF THE NAVIER-STOKES

EQUATIONS

155

O.P. CHANDNAandE.O.OKU-UKPONG

Department

of Mathematicsand Statistics

and

FluidDynamics ResearchInstitute University of Windsor Windsor, Ontario, Canada N9B 3P4

(Received April 30, 1992)

ABSTRACT. Solutions areobtainedfortheequationsof the motionof thesteadyincom- pressibleviscousplanar generalizedBeltrami flowswhenthe vorticity distributionisgiven by

V2b + f(z,y)

for threechosen forms of

f(z,).

KEY

WORDS

AND

PHRASES. viscousflow,asymptoticsuctionprofile,Beltrami flow.

1991AMS

MATHEMATICS

SUBJECTCLASSIFICATION CODES. 76 Fluid

Me-

chanics,35 Partial DifferentialEquations.

1.

INTRODUCTION.

Onlyasmall number of exact solutions of the Navier-Stokes equations has been found and Chang-Yi

Wang [1]

hasgivenanexcellentreview of these solutions. Theseknownsolutionsot viscousincompressibleNewtoaianfluids may be classifiedintothreetypes:

(i)

Flows for which the non-linearinertiaterms inthe linear momentum equations vanish identically. Parallelflowsand flows with uniformsuction areexamplesof these

flows;

(ii)

flowswithsimilarityproperties such that theflowequationsreducetoaset of ordinary differential equations. Stagnationpoint flowis anexample ofsuch

flows;

(iii)

flowsforwhichthe vorticity functionis sochosen that the governing equationinterm of the stream function reduces toalinearequation. Taylor

[2], Kampe

de Feriet

[3], Kovasznay [4], Wang [5]

and Lin and Tobak

[6] employed

this

approach,

taking

V2, K,, V, f().

V, + (K 4x),, V2, A + Cy

and

V K( Ry),

respectively.

In

this paper,westudy generalizedBeltrami flows when thevorticityfunction w

-Vb

isgiven by

V, + A

2

+ Bz + Cz + D, V2 , + Ay + Cz +D, Vb , + Cz

+Dy,

where

A,B,C,D

arereal constants.

(2)

2. BASIC

EQUATIONS

AND SOLUTIONS.

Steadyplaneincompressibleviscousfluidflow,inthe absence of external forces,isgoverned bythesystem:

+

0

1 P 1

(2.1)

where

(, ), f:(, 9)

axethe velocity

components,/5(,, 9)

thepressurefunction,p theconstant density,pthe constant viscosity and,2

r

0’

+

b

isthe Laplacian operator. Thevorticity functionforthisflowisgivenby

(2.2)

Letting

U,L

to be the characteristic velocity and length respectively, we introduce the non-dimensional variables

(2.3)

=Z, Y=Z, "=y, =y, =W, v-v,

in system

(2.1)

and equation

(2.2). We

apply theintegrability condition P-u Pu- to the linearmomentum equationsto find that u, v,w must satisfy the system:

(2.4)

where

R

L isthe Reynolds number.

Introducingthe stremfunction

(z, y)

suchthat

,.=,, v=-,

insystem

(2.4),

wefindthat

(z,y)

must satisfy

V@ + R 0(, Vb)

0

0(,)

In

this paper,westudyflows for which the vorticity distributions take theforms

w

-V2 -( + Ay

m

+ Bzy + Cz + Dy)

(b)

w

-Vb -( + Ay + Cz + Dy)

., -V2 -( + Cz + Dy)

where

A, B, C, D

arereal constants.

Form (a):

Substituting

(2.7)

inthe compatibility equation

(2.6),

weget

R(2Ay + Bz + D), R(By + C). + /, + Ay + Bzy + Cz + Dy +

2A 0

(2.8) (2.9)

(2.10)

(3)

EXACT SOLUTIONS OF THE STEADY NAVIER-STOKES EQUATIONS 157

Employingthecanonical coordinates

Ay

2

+ Bzy + Cz + Dy, = (2.)

where

(By + C) # O, (2.10)

maybewrittenas

-( + c). + + +

2A 0.

Thisequationissolved to obtain

f()(By + D):" (Ay + Bzy + Cz + Dy + 2A) (2.13)

where

f

isanaxbitrary function of

.

Introducing

(2.13)

into

{2.7),

weget

{R’ [C’(C’ + D’) + 2BCD( + B’(’] /"() + 2R[C(RAC + D)- B(] /’() + [1 RB- RC ] ()} + 2RC{2R[C(AD + BC)+ AB] f’()

+

2A

[RB + 1] f() RB/(()}. + R {2R [C(2A +

3B

) + ABCD

+ 4RC { [A + ]/"(0}.’ + R { [ + ]/"(0}.’

0

Since

,

eindependent vables d

{I, , , ,

isaHnely independent t,itfollows that the ccients of the

vous

powersof zero.

Tng

the coecients of

, s, ,

d1

equM

to zero,weget

(2.14)

f() cI + c (2.15)

2A(RB

+ 1)cl RBc

RBc,( 0

(2.16)

wherecl,

c

axearbitrary constants. Since

{1, }

isalinearlyindependent set,itfollows from

(2.16)

that

2A(RB + 1)cl RBc2 O, RBcl

0 giving

c c

0. Usingc,

c

0in

(2.15),

weobtain

f(()

0.

From

(10),

the streamfunction isgivenby

@(z, y) -(Ay’ + Bzy + Cz + Dy + 2A) (2.17)

The exact integral ofthisflowis

u=-(2Ay+Bz+D), ,=By+C,

and 1

[B(z2 + y,) + 2(BD 2AC)z + 2BCy]

p= po

- (2.18)

wherep0 is anaxbitraryconstant.

Equation

(2.17)

represents an impingement of two constant-vorticity oblique flows with stagnation point

(Z,Y)--<

2AC-BD

,

,-

) (2.9)

(4)

fornon-zero values of

A, B,

Cand E. The stagnation pointshifts upward as

B

gets smaller forfixedvaluesof

A,

Cand

E.

Weremark that when

A B

-1,

C D

0,the solution

(2.17)

reducestooneof the flows in

Wang’s [1]

paper.

Form

{b):

Employing

(2.8)

in

(2.6),

weobtain

R(2Ay

+ D)b, RCI, + + Ay

2

+ Cz + Dy +

2A 0

(2.20)

Choosingthe canonical coordinates

Ay

2

+ Cz + Dy,

I Y

(2.21)

whereC

#

0,

(16)

takes theform

-RCl,, + P + +

2A O.

(2.22)

We

solve this equation toget

=g()expIcy ) (Ay2 + Cz + Dy + 2A)

whereg isanarbitraryfunctionof

. We

substitute

(2.23)

into

(2.8)

toget

[R:C’ g"(,) + 2RAC g’(,) + (1 R:Cg()] + 2RCg’()(2Ar + D)

+ R2C2g"()(2Arl + D)

0

(2.23)

(2.24)

Since

,

1areindependent variables and

{1, (2A/+ D), (2A/+ D)

2

}

isalinearly independent set,itfollows that

g"() O, g’(6)

0,

(1 R2C)g()

0

(2.25)

From (1 RCZ)g()

0, we get the three possibilities:

g() =.0, R2C #

1;

R2C

2 1,

g(O #

0;

g(O o, R’C .

Thestream function

(2.23)

isgiven by

-(Ay +Cz+Dy+2A)

;g=O,

R 2C 2#1

,/,(,) ge g0 ( + 6’ + + z);6 ’ , #

-(A +6’+D+A)

;=0,

R 6’=1

whereg

#

0impliesg

K (non-zero constant).

Whenthestreamfunction isgiven by

(2.26)

,(z,y)--(Ay

/

Cz + Dy + 2A); RC

--1 or

RC #1, (2.27)

the exactintegralforthe flowis

u

-(2Ay + D),

v

C,

and p po

+

2ACz

(2.28)

(5)

EXACT SOLUTIONS OF THE STEADY NAVIER-STOKES EQUATIONS 159

wherep0isan arbitrary constant.

Thesolution

(2.28)

maybe realizedonaplatesituated

along

y

-

with uniform suction or blowing.

C >

0 andC

<

0,respectively, for blowingandsuction attheplate.

The exactintegralfor theflow givenby the stream function

(z,y)

Kexp (---V) -(Av2 +Cz + Dy + 2A); R

C2 1

(2.29)

is

u=-exp

V

(2Av + D),

v

C,

and p po

+

2ACz

(2.30)

wherep0is anarbitrary constant.

If

K

RCD in

(2.29)

and

(2.30),

the velocityprofilein

(2.30)

canberealizedon aplate

locatedalongV 0with uniformsuction. The velocity profileattains the form

(2.31)

onlyasymptotically, andsomay beregardedasthe asymptoticsuctionprofile

[7].

C

>

0 and C

<

0 forblowing andsuctionatthe plate, respectively.

Form

(c):

Substitution of

(2.8)

into

(2.6)

yields

RD. RCCu + + Cz + Dy

0

(2.32)

Thecanonicalcoordinates

=Cz+Dy,

7=V;

C:f-0 (2.33)

areemployedin

(2.32)

toget

-RC + + o.

Thesolutionofthisequationis

b h()exp (cy) -(Dz+Ey)

wherehisanarbitraryfunctionof

.

We employ

(2.34)

in

(2.9)

toobtain

R2C2(C

2

+ D-)h"() + 2nCDh’() + (1 n2C2)h()

0

(2.34)

(2.35)

Thegeneralsolutionof

(2.35)

is

h(O

A1 exp(Al) + A2 exp(A2)

(B1

Ci Cos(m( + C)

exp

;R2(C + D )-

1

>

0

R2(C

2

+ D )-

1 0

;R:(C

:

+ D )

1

<

0

(2.36)

(6)

where

-D + Cv/R2(C

:

+ D )

1

V/1 R2(C +

D

’)

A1.2 RC(C + D,)

m

R(C2 +

02

(2.37)

and

A,A=,B,B=,C,C=

ebitryconstts.

Wesh study the three possibiHtiessepately.

(i) R(C + D )-1>

0

The strefunction,

om (2.34)

d

(2.36),

is

(z,y) A

exp

[ACz + (2D+ )yl + A,

exp

[A,

Cz

+ (A,D+ )y]-(Cz+Dy)

(=.3s)

TheexactintegrMoftsflowis

u=

(D+ )A

exp

[ACz + (D+ )y]

+ (2D+)A,

exp

,C+ (A2D+)yI-D,

v

-D {lA

exp

[Cz + (D + ) y] (2.39)

+

2Aexp

and

P=po

+

2 1-

R,(C,

+

O2

A1A2exPtR-- +

wherep0 isanarbitrary constant and

A1

,2 aregiven by

(2.37).

Ts

flow reprents impingement of obquefo stre th obfique rota- tionM,

vergent flow,

th stagnation point

(z,y)

2,(C + D’)-

1

DR’(C’ + D’)

l

m { -4AA’[R’(C’ + D’) I]

}

a=(C + D)=

R(C + D) 2.40)

whereA,A2 enon-zero

mM

constants deither

A >

0,

A <

0or

A <

0,

A2 >

0.

Fo

ed

ues

of

R,

Cd

D,

the stagnation point sftsupwdwhenthe absolute vMueof

A

islgerth that of

A.

H A

d

A

areofthesesign, the abovephenomenonds not

te

plce,dwehave aflow thouta

staation

point.

(ii) Rx(C ,

+ D =)-1=0

Using

(2.36)

in

(2.34),

the stre functionis

(z,V) [Bx + B2(Cz + DV)]e[R(OV- D)]- (C + Dr) (2.41) Ts

flow h theexitintegrM

u

{DB2 + RC[Bx + B2(Cx + Ov)]}exp[R(CV- O,)]- E,

v

{-DB2 + RD [Bx + Bx(C + Oy)]}

exp

[R(Cy- D)] + D,

d

(2.42)

1

(7)

EXACT SOLUTIONS OF THE STEADY NAVIER-STOKES EQUATIONS 161

wherep0 isan arbitrary constant.

If

B2

isapositive realconstant,thisflow representsanimpingement ofanoblique uniform streamwithanoblique rotational,divergent flow,with stagnation point

1

(CB1

(z,t/) -C +

D2

B2

D In

B2,

DB

C

)

R + In B, (2.43)

Forfixed values of

R

and

C,

the stagnation point shifts upwardif

B1

and

D

areof opposite signs and the absolute value of

B1

islargerthan

If

B2

isanegative realconstant,

(2.41)

representsanoblique uniform streamwhich abuts on anoblique rotational,convergent flow.

(iii) R 2(C2+D2)-1<0

From

(2.27)

and

(2.36),

the stream functionisgivenby

{’z,y) C,

Cos

[m(Cz +

Dy)

+ C2]

exp

Cv- Dz _(Cz +

Dy)

R(C + D 2) (2.44)

The exactintegral forthisflowis

{

CCos

[m(Cz + Dy) +

R(C

2

+ D 2)

Cy-

Dz -mRD(C + D2)Sin [m(Cz + Dy) + C2]}

exp

R(C2 +

02

D,

v

R(C2 +

02

{DCos [m(Cz + Dy) + C,] (2.45)

+mRC(C + D2)Sin[m(Cz +

Dy)

+ C2]}

exp

[R(C

2

+

D2

+ C,

2(Cv Dz) R(C + D =)

1 1

]C21Cos2[m(Oz+Dt/)+O2]ex

p

P0+

1-

R=(C = +

D2

and

whereP0 isanarbitraryconstant,andmisgivenby

(2.37).

If

Cx >

0,the stagnation points forthisflowaxe

( RC[(2n + I){ C:] [C1v/1- R2(C: + D2’i]

(=,y)

----R(b ..D-) + RDIn R(C2 + D2) RD[(2n+I);-C2]

X/1 R2(C + D’)

RCln

R(C2 +

D2

(2.46)

wheren isaninteger.

Fig. 1 shows the streamlines for

(z,y) -(Av

2

+ Bzt/+ Cz + Dy + 2A)

when

A B C D

1. Figures 2 and 3 represent the flows

tk(z,y) -(Ay

2

+

Ca:

+ Dy + 2A)

and

(z,t/) K

exp

(cY) (At/2 + Cz + Dt/+ 2A)

for

K R A C D

1. Figures4 and 5 illustrate thecase

(c) (X72 +

Cz

+ Dt/)

when

R2(C

2

+ D 2) >

1. Figure4 shows reversedflow.

C=D=I,R=2, Az

=50,

A2

=60andC=D=R=l,

A1

=1,

A2=-1,

respectively,forFigures4 and 5. The flows when

R2(C

2

+ D 2)

1 aregiveninFigures 6 and

7whenC=D=l,R= ,B1

=50,

B2=-60andC=D=l,R=,Bt

=0,

B2=l.

WhenR

(C 2+D2)<1.

wehave

Figure8forC=D=l,R=1/2, Cx

=5,

C2=0.

(8)

Figure 1

-0. l0

55

-.00

-o.o -I.$ -s.@ .s

Figure 2

Fibre

3

-;0

-0

-40

o

o 4o

F]x

4

(9)

EXACT SOLUTIONS OF THE STEADY NAVIER-STOKES EQUATIONS 163

oo BO

Fibre

5

-’O.O

-tS.O -?.$ 15.0 Io

(10)

REFERENCES

[1]

C.-Y. WANG Exact solutions of the steady-state Navier-Stokes equations,

Annu. Rev__._:

Fluid Mech. 23.

(1991)

159-177.

[2]

G.I. TAYLOR On thedecay ofvortices ina viscousfluid,Phil.

Mag:, Serie....__.s

6,46

(1923)

671-674.

[3]

J.

KAMPE DE FERIET

Sur quelques casd’integration des equations du mouvementplan d’unfluide visqueux incompressible,

Proc_._._: Int._._:..Congr.

Appl.

Mech.._...:, 3rd_._.:.

Stockholm 1_

(1930)

334-338.

[4] L.I.G. KOVASZNAY

Laminarflow behindatwo-dimensional grid,

Proc_.

CambridgePhil.

Soc_. 44,

(1948)

58-62.

[5]

C.-Y. WANG

On

a class ofexact solutions of the Navier-Stokes equations,

J__.

of

Mech. 33

(1966)

696-698.

[6]

S.P. LIN and M. TOBAK Reversed flow abovea plate withsuction,

.AIAA_,

24,

No.

2.

(1986)

334-335.

[7]

H. SCHLICHTING

.Boundary-Laye ,

McGraw-Hill, 1968.

(11)

Journal of Applied Mathematics and Decision Sciences

Special Issue on

Decision Support for Intermodal Transport

Call for Papers

Intermodal transport refers to the movement of goods in a single loading unit which uses successive various modes of transport (road, rail, water) without handling the goods during mode transfers. Intermodal transport has become an important policy issue, mainly because it is considered to be one of the means to lower the congestion caused by single-mode road transport and to be more environmentally friendly than the single-mode road transport. Both consider- ations have been followed by an increase in attention toward intermodal freight transportation research.

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