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    058:0160 Chapter 8Professor Fred Stern Fall 2009 1

    Chapter 8: Inviscid Incompressible Flo: a !sef"l Fantas#

    8.1 Introduction

    For hi$h %e e&ternal flo abo"t streamlined bodies visco"s effects are confined tobo"ndar# la#er and a'e re$ion( For re$ions here the )(* is thin i(e( favorable press"re$radient re$ions+ ,isco"s-Inviscid interaction is ea' and traditional )(* theor# can be"sed( For re$ions here )(* is thic' and-or the flo is separated i(e( adverse press"re$radient re$ions more advanced bo"ndar# la#er theor# m"st be "sed incl"din$visco"s-Inviscid interactions(

    For internal flos at hi$h %e visco"s effects are ala#s important e&cept near the

    entrance( %ecall that vorticit# is $enerated in re$ions ith lar$e shear( .herefore+ o"tsidethe )(* and a'e and if there is no "pstream vorticit# then /0 is a $ood appro&imation(ote that for compressible flo this is not the case in re$ions of lar$e entrop# $radient(lso+ e are ne$lectin$ noninertial effects and other mechanisms of vorticit# $eneration(

    Potential flow theory

    13 4etermine from sol"tion to *aplace e"ation02 =

    )(C:

    at BS : ( 0 0V nn

    = =

    at S : V =

    Note:F: S"rface F"nction

    1

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 2

    10 ( 0 (

    DF F FV F V n

    Dt t F t

    = + = =

    for stead# flo ( 0V n=

    23 4etermine V from V = and p&3 from )erno"lli e"ation

    .herefore+ primaril# for e&ternal flo application e no consider inviscid flo theor# 0= 3 and incompressible flo const= 3

    Euler equation:

    ( 0

    ( 3

    V

    DVp g

    Dt

    VV V p z

    t

    =

    = +

    + = +

    2

    (2

    : 2

    VV V V

    Where V vorticity fluid angular velocity

    =

    = = =

    21 32

    0 0 :

    Vp V z V

    t

    If ie V then V

    + + + =

    = = =

    16 3

    2p z B t

    t

    + + + =

    Bernoullis Equation for unsteady incompressible flow notf(x)

    Contin"it# e"ation shos that 74 for is the *aplace e"ation hich is 2ndorderlinear P4 ie s"perposition principle is valid( *inear combination of sol"tion is also asol"tion3

    2

    1 2

    2

    2 2 2 2 1

    1 2 1 2 2

    2

    0

    00 3 0 0

    0

    V

    = = == +

    = = + = + =

    =.echni"es for solvin$ *aplace e"ation:

    13 s"perposition of elementar# sol"tion simple $eometries323 s"rface sin$"larit# method inte$ral e"ation33 F4 or F3 electrical or mechanical analo$s53 Conformal mappin$ for 24 flo363 nal#tical for simple $eometries separation of variable etc3

    2

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    058:0160 Chapter 8Professor Fred Stern Fall 2009

    8.! Elementary plane"flow solutions:

    %ecall that for 24 e can define a stream f"nction s"ch that:

    x

    y

    v

    u

    =

    =

    03636 2 ==

    == yxyxz

    yxuv

    i(e( 02 =lso recall that andare ortho$onal(

    yx

    xy

    v

    u

    ==

    ==

    udyvdxdydxd

    vdyudxdydxd

    yx

    yx

    +=+=

    +=+=

    i(e(const

    const

    dx

    dyv

    u

    dx

    dy

    =

    =

    ==

    1

    8.! Elementary plane flow solutions

    #niform stream

    yx

    xy

    v

    constUu

    ===

    ==== 0

    i(e(yU

    xU

    =

    =

    ote: 022 == is satisfied(;V U i = =

    Sa# a "niform stream is at an an$le tothe &

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 5

    ( 0

    1 16 3 6 3 0r

    V

    rv vr r r

    =

    + =

    i(e(:

    rv

    rrvr

    =

    ==

    ===

    r

    1velocit#.an$ential

    1velocit#%adial

    S"ch that 0V = b# definition(

    .herefore+

    rv

    rrvr

    =

    ==

    =

    ==

    r

    1

    0

    1

    r

    m

    i(e(x

    y""

    yx"r"

    1

    22

    tan

    lnln

    ==

    +==

    $oublets:

    .he do"blet is defined as:

    ==so"rce

    2sin'

    1so"rce

    2sin'

    1 3 "$ "

    2tan

    1tan1

    2tan

    1tan

    tan21

    tan%%

    %%&

    "'&%'%

    +

    ==

    1 2

    2 2

    sin sintan tancos cos

    sin sin

    2 sincos costan6 3sin sin

    1cos cos

    'r rr a r a

    r rarr a r a

    r r" r a

    r a r a

    = = +

    + = =

    + +

    For small val"e of a

    5

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 6

    1

    2 2 2 2 20

    2 sin 2lim tan 3a

    ar a"y y"

    r a r x y

    = = = + cos

    2 3a" Doulet Strengthr

    = =

    )# rearran$in$:222

    22 3

    23

    2

    =+++

    = yxyx

    y$

    It means that streamlines are circles ith radi"s

    2=( and center at 0+

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 A

    S"ppose that val"e of theand for the so"rce are reversal(0

    1

    rv

    )v

    r r r

    =

    = = = P"rel# recirc"latin$ stead# motion+ i(e( ( )v f r= ( inte$ration res"lts in:

    ln *+constant

    )%

    $ ) r

    ==

    24 vorte& is irrotational ever#here e&cept at the ori$in here V and V are infinit#(

    ,irculation

    Circ"lation is defined b#:

    c* closed contour

    + V d s

    =

    =

    For irrotational flo

    Br b# "sin$ Sto'es theorem: if no sin$"larit# ofthe flo in 3

    ( -c A A

    + V d s V d A ndA= = = =

    .herefore+ for potential flo 0= in $eneral(oever+ this is not tr"e for the point vorte& d"e to the sin$"lar point at vorte& corehere Vand V are infinit#(

    If sin$"larit# e&ists: Free vorte&r

    )=

    { {

    2 2

    0 0; ; 3 2

    2 and

    V d s

    )v e rd e rd ) )

    r

    = = = =

    ote: for point vorte&+ flo still irrotational ever#here e&cept at ori$in itself hereV+ i(e(+ for a path not incl"din$ 0+03 0 =

    A

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 8

    lso+ e can "se Sto'es theorem to sho the e&istence of :

    D

    *

    AB* AB *

    V d s V d s = = SinceD

    ( 0AB*B A

    V d s=.herefore in $eneral for irrotational motion:

    (V d x =

    =here: se "nit tan$ent vector alon$ c"rve &Since se is not Eero e have shon:V = i(e( velocit# vector is $radient of a scalar f"nction if the

    motion is irrotational( 0V d s = 3.he point vorte& sin$"larit# is important in aerod#namics+ since+

    e&tra so"rce and sin' can be "sed to represent airfoils and in$s and e shall disc"ssshortl#( .o see this+ consider as an e&ample:

    an infinite ro of vortices:

    ==

    =

    32

    cos2

    cosh2

    1ln

    2

    1ln

    1 a

    x

    a

    y)r)

    i

    i

    =here ir is radi"s from ori$in of ithvorte&(

    "all# speed and e"al stren$th Fi$ 8(11 of .e&t boo'3

    For y a? the flo approach "niform flo ith

    a

    )

    yu

    =

    =

    : belo & a&is

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 9

    orte) sheet:

    From afar i(e( y a? 3 loo's that thin sheet occ"rs hich is a velocit# discontin"it#(

    4efine ==a

    )

    2stren$th of vorte& sheet

    dxa

    )dxuudxudxud

    ulul

    23 ===

    i(e(dx

    d= Circ"lation per "nit span

    ote: .here is no flo normal to the sheet so that vorte& sheet can be "sed to sim"late abod# s"rface( .his is be$innin$ of airfoil theor# here e let 36x= to represent bod#$eometr#(

    ,orte& theorem of elmholtE: important role in the st"d# of the flo abo"t in$s3

    13 .he circ"lation aro"nd a $iven vorte& line is constant alon$ its len$th23 vorte& line cannot end in the fl"id( It m"st form a closed path+ end at a

    bo"ndar# or $o to infinit#(3 o fl"id particle can have rotation+ if it did not ori$inall# rotate

    ,ircular cylinder /without rotation0:

    In the previo"s e derived the folloin$e"ation for the do"blet:

    2 2

    sinDoulet

    y

    x y r

    == = +

    =hen this do"blet is s"perposed over a

    "niform flo parallel to the &< a&is+ e $et:

    2

    sin 1sin 1 sinU r U r

    r U r

    = =

    =here: = do"blet stren$th hich is determined from the 'inematic bod# bo"ndar#condition that the bod# s"rface m"st be a stream s"rface( %ecall that for inviscid flo it is

    9

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 10

    no lon$er possible to satisf# the no slip condition as ares"lt of the ne$lect of visco"sterms in P4s(

    .he inviscid flo bo"ndar# condition is:F: S"rface F"nction

    10 ( 0 0DF F FV F V nDt t F t

    = + = = = for stead# flo3

    .herefore at r%+ V(n0 i(e( (rrv ==0 (

    ; ;r rV v e v e = + +

    2 2

    ; ;;

    r

    r

    r

    F Fe e

    F rn eF F F

    + = = =

    +

    2

    11 cosrV n v U

    r U r

    = = =

    0

    2U ( =

    If e replace the constantU

    b# a ne constant %2+ the above e"ation becomes:

    2

    21 sin

    (U r

    r

    =

    .his radial velocit# is Eero on all points on the circle r%( .hat is+ there can be novelocit# normal to the circle r%( .h"s this circle itself is a streamline(

    =e can also comp"te the tan$ential component of velocit# for flo over the circ"lar

    c#linder( From e"ation+ 2

    21 sin

    (v U

    r r

    = = +

    Bn the s"rface of the c#linder r%+ e $et the folloin$ e&pression for the tan$ential andradial components of velocit#:

    2 sinv U =

    0=rv

    o abo"t press"re p loo' at the )erno"lliDs e"ation:

    ( )2 2 21 12 2r

    ppv v U

    + + = +

    fter some rearran$ement e $et the folloin$ non

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 11

    ( )2 2

    22

    + 11

    2

    r

    p

    v vp p* r

    UU

    += =

    For the circ"lar c#linder bein$ st"died here+ at the s"rface+ the onl# velocit# componentthat is non

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 12

    bodies( circ"lar c#linder is not a streamlined bod# li'e as airfoil3 b"t rather a bl"ffbod#( .h"s+ as e shall determine no the potential flo sol"tion is not realistic for thebac' portion of the circ"lar c#linder flos 3906 > (For $eneral:

    F(I*-I!.S)I.D(A/F!(0DDD

    *** +=

    D(A/F!(0D* : dra$ d"e to visco"s modification of press"re destr"ction

    F(I*-I!.S)I.D* : 4ra$ d"e to visco"s shear stress

    :

    :DS) DF!

    DF! DS)

    Strea"lined Body * *

    Bluff Body * *

    > >

    ,ircular cylinder with circulation:.he stream f"nction associated ith the flo over a circ"lar c#linder+ ith a point vorte&of stren$th placed at the c#linder center is:

    sin

    sin ln2U r rr

    = From ,(n0 at r%: 2U ( =

    .herefore+2 sin

    sin ln2

    U (U r r

    r

    =

    .he radial and tan$ential velocit# is $iven b#:2

    2

    11 cos

    r

    (v U

    r r

    = =

    2

    21 sin

    2(v U

    r r r

    = = + + Bn the s"rface of the c#linder r%3:

    2

    2

    11 cos 0r

    (v U

    r (

    = = =

    2 sin2

    v Ur (

    = = +

    e&t+ consider the flo pattern as a f"nction of ( .o start lets calc"late the sta$nationpoints on the c#linder i(e(:

    2 sin 02

    v U(

    = + =

    sin - 2 2

    )

    U ( U (

    = = =

    ote:2

    ))

    U (

    = =

    12

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 1

    So+ the location of sta$nation point is f"nction of (

    2

    )

    U ( U (

    = = s

    sta$nation point3

    0 0sin = 3 0+1801 5(0sin = 3 0+1502 1sin = 3 90?2 1sin > 3 Is not on the circle b"t here 0rv v= =

    For flo patterns li'e above e&cept a3+ e sho"ld e&pect to have lift force in K#direction(

    %ummary of stream and potential function of elementary !"$ flows:In Cartesian coordinates:

    yx

    xy

    v

    u

    ==

    ==

    In polar coordinates:

    rv

    rrvr

    =

    =

    =

    =

    r

    1

    1

    Flo !niform Flo xU yUSo"rce m?03Sin' m@03

    ln" r "

    1

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 1

    4o"bletr

    cos

    r

    sin

    ,orte& ) 1 ln) r90 Corner flo 362-1 22 yxA Solid

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 15

    Meep in mind that this is the potential flo sol"tion and ma# not ell represent the realflo especiall# in re$ion of adverse p&(

    he *utta 2 3ou&ows&i lift theorem:

    Since e 'no the tan$ential component of velocit# at an# point on the c#linder and theradial component of velocit# is Eero3+ e can find the press"re field over the s"rface ofthe c#linder from )erno"lliHs e"ation:

    22 2

    2 2 2

    r vv p Up

    + + = +

    .herefore:

    2 22 2 2 2

    2 2

    2

    1 12 sin 2 sin sin

    2 2 2 8

    sin sin

    Up p U U p U U

    ( ( (

    A B *

    = + = + +

    = + +

    here

    22

    2 2

    1

    2 8A p U

    (

    = +

    U

    B(

    =

    22* U =

    Calc"lation of *ift: *et "s first consider lift( *ift per "nit span+ * i(e( per "nit distancenormal to the plane of the paper3 is $iven b#:

    =Lo2er upper

    pdxpdxL

    Bn the s"rface of the c#linder+ & %cos( .h"s+ d&

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 16

    .his is an important res"lt( It sa#s that cloc'ise vortices ne$ative n"merical val"es of3 ill prod"ce positive lift that is proportional to and the free stream speed ithdirection 90 de$rees from the stream direction rotatin$ opposite to the circ"lation( M"ttaand No"'os'i $eneraliEed this res"lt to liftin$ flo over airfoils( "ation = uL is 'non as the M"tta

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 1A

    ,elocit# ratio:a

    U

    .heoretical and e&perimental lift and dra$ of a rotatin$ c#linder

    &periments have been performed that sim"late the previo"s flo b# rotatin$ a circ"larc#linder in a "niform stream( In this case (v = hich is d"e to no slip bo"ndar#condition(

    < *ift is "ite hi$h b"t not as lar$e as theor# d"e to visco"s effect ie floseparation3

    < ote dra$ force is also fair# hi$h

    Fletttern 1923 "sed rotatin$ c#linder to prod"ce forard motion(

    1A

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 18

    18

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 19

    19

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 20

    8.3 Method of Images

    .he method of ima$e is "sed to model Oslip all effects b# constr"ctin$ appropriateima$e sin$"larit# distrib"tions(

    Plane Boundaries:

    2

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 21

    %pherical and ,ur(ilinear Boundaries:

    .he res"lts for plane bo"ndaries are obtained from consideration of s#mmetr#( Forspherical and circ"lar bo"ndaries+ ima$e s#stems can be determined from the Sphere Q

    Circle .heorems+ respectivel#( For e&ample:

    Flo field Ima$e S#stemSo"rce of stren$th R at c o"tside sphere ofradi"s a+ c?a So"rces of stren$th c

    "a atc

    a 2 and line

    sin' of stren$th a" e&tendin$ from center

    of sphere toc

    a 2

    4ipole of stren$th at l o"tside sphere ofradi"s a+ l3a dipole of stren$th la

    9

    at la2

    So"rce of stren$th m at b o"tside circle ofradi"s a+ b?a e"al so"rce at

    a 2 and sin' of same

    stren$th at the center of the circle

    21

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 22

    7ultiple Boundaries:

    .he method can be e&tended for m"ltiple bo"ndaries b# "sin$ s"ccessive ima$es(

    13 For e&ample+ the sol"tion for a so"rce e"all# spaced beteen to parallel planes

    ( )[ ] ( )[ ][ ]

    ( ) ( ) ( ) ( ) ( ) ( )[ ]

    ++++++++++++=

    +++= =

    azazazazazaz"

    anzanz"z2"

    2lnln6lnln2lnln

    2lnln3+2+1+0

    22

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 2

    23 s a second e&ample of the method of s"ccessive ima$es for m"ltiple bo"ndariesconsider to spheres and ) movin$ alon$ a line thro"$h their centers atvelocities !1and !2+ respectivel#:

    Consider the 'inematic )C for :( ) ( ) 2222+ azyytxtxF ++=

    1 1;; ;0 or cos( ( (

    DFV e U 4 e U

    Dt = = =

    here 2 cos( = +

    2 cos

    2(Ua

    ( = =

    Similarl# for ) 2 cos D( U =

    .his s"$$ests the potential in the form

    1 1 2 2U U = +

    here 1and 2both satisf# the *aplace e"ation and the bo"ndar# condition:

    1 1

    D

    cos + 0D( a ( ( (

    = =

    = = 3

    2 2

    D

    0+ cos DD( a ( ( (

    = =

    = = 3

    2

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 2

    1 potential hen sphere moves ith "nit velocit# toards )+ ith ) at rest2 potential hen sphere ) moves ith "nit velocit# toards + ith at rest

    If ) ere absent(9

    01 2 2

    cos cos2

    a

    ( (

    = = +

    2

    9

    0

    a=

    b"t this does not satisf# the second condition in 3( .o satisf# this+ e introd"ce theima$e of 0 in )+ hich is a do"blet 1 directed alon$ ) at 1+ the inverse point of ith respect to )( .his ima$e re"ires an ima$e 2 at 2+ the inverse of 1ith respectto + and so on( .h"s e have an infinite series of ima$es 1+ 2+ T of stren$ths 1 +

    2 + 9 etc( here the odd s"ffi&es refer to points ithin ) and the even to points ithin(

    *et Qn nf AA AB c= =

    c

    cf

    2

    1 = +1

    2

    2f

    af = +

    2

    2

    9fc

    cf

    = +T

    =

    9

    9

    01c

    +

    =

    9

    1

    9

    12f

    a+

    ( )

    =

    9

    2

    9

    29fc

    +T

    here 1 ima$e dipole stren$th+ 0 dipole stren$th 99

    sistance

    radi"s

    0 1 1 2 21 2 2 2

    1 2

    cos cos cos

    ( ( (

    = K ith a similar development proced"re for 2(

    ltho"$h e&act+ this sol"tion is of "nield# form( *etHs investi$ate the possibilit# of anappro&imate sol"tion hich is valid for lar$e c i(e( lar$e separation distance3

    22 2 2 2

    2

    1 12 22 2

    2 2

    2D 2 cos 1 cos

    1 1 11 2 cos 1 2 cos

    D

    c c( ( c cr (

    ( (

    c c ( (

    ( ( ( ( c c c

    = + = +

    = + = +

    2

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    058:0160 Chapter 8Professor Fred Stern Fall 2009 25

    Considerin$ the former representation first definin$c

    (= and cosu =

    [ ] 21

    221

    1

    D

    1 += u

    ((

    )# the binomial theorem valid for 1