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AMS212BPerturbationMethodsLecture07
CopyrightbyHongyunWang,UCSC
Revisittheissueofboundarylayerlocation
Welookattheissuefromadifferentangle.Specifically,weanalyzetheproblemusingthecharacteristicsoffirstorderPDEs.
Considertheboundaryvalueproblem(BVP)
ε ′′y +a x( ) ′y +b x( ) y − c x( )( ) =0y 0( ) =α , y 1( ) =β
⎧⎨⎪
⎩⎪, ε→0+
Keystrategy:
WeviewthesolutionoftheBVPasthesteadstatesolutionofatimeevolutionPDE.
∂ y∂t
= ε ∂2 y∂x2
+a x( )∂ y∂x +b x( ) y − c x( )( ) Physicalmeaningoftheterms:
ε ∂
2 y∂x2
: diffusion
a x( )∂ y∂x : transportation
b x( ) y − c x( )( ) : growth/decay
Note: ε≥0isrequiredforthewell-posednessofthePDE.
Inthecaseofε→0-,weredefine
εnew = −εold
anew x( ) = −aold x( )
bnew x( ) = −bold x( )
Weconsider
∂ y∂t
= εnew∂2 y∂x2
+anew x( )∂ y∂x +bnew x( ) y − c x( )( ) , εnew →0+
AMS212BPerturbationMethods
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TheunperturbedPDE(ε=0)isafirstorderlinearPDE.
∂ y∂t
= a x( )∂ y∂x +b x( ) y − c x( )( ) Characteristics
dxdt
= −a x( ) Alongacharacteristic,wehave
dy x t( ) ,t( )
dt= ∂ y∂x
⋅dxdt
+ ∂ y∂t
= ∂ y∂x
⋅ −a x( )( )+a x( )∂ y∂x +b x( ) y − c x( )( )
= b x t( )( ) y − c x t( )( )( )
Itisclearthatthesolutionpropagatesalongcharacteristics.
Example:
∂ y∂t
= ∂ y∂x
+ y
Characteristics:
dxdt
= −1 ==> x(t)=-t+x(0)
Alongacharacteristic,thesolutionsatisfies
dydt
= y ==> y x t( ) ,t( ) = y x 0( ) ,0( )et Thefigurebelowshowsthecharacteristicsinthex-tplane.
x
t
AMS212BPerturbationMethods
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Fromthefigure,weseethatinthecaseofε=0,§ aboundaryconditionshouldbeimposedatx=1;
§ noboundaryconditionshouldbeimposedatx=0;ifaboundaryconditionisimposedatx=0,thenthereisadiscontinuityatx=0.
Inthecaseofε>0,thePDEisdiffusive
∂ y∂t
= ε ∂2 y∂x2
+ ∂ y∂x
+ y
§ Atx=0,thereisamismatch(discontinuity)betweentheboundaryconditionandthepropagationalongcharacteristics.
§ Themismatchissmoothedbythesmalldiffusionterm;butthetransportation(propagationalongcharacteristics)preventstheeffectoftheboundaryconditionfromreachingsignificantlyinside(0,1).
==> Themismatchbecomesanarrowtransitionnearx=0.==> Thereisaboundarylayeratx=0.
Summary:Aboundarylayeriscausedbyamismatch
§ eitherbetweenboundaryconditionandpropagationalongcharacteristics
§ orbetweenpropagationsalongtwodifferentgroupsofcharacteristics
NowweexamineseveralcasesofthegeneralBVP
ε ′′y +a x( ) ′y +b x( ) y − c x( )( ) =0 ThecorrespondingfirstorderPDEforϵ=0:
∂ y∂t
= a x( )∂ y∂x +b x( ) y − c x( )( ) Characteristics:
dxdt
= −a x( )
Case1: a x( ) >0forx∈ 0,1⎡⎣ ⎤⎦
Arepresentativediagramofcharacteristicsisshownbelow.
AMS212BPerturbationMethods
- 4 -
==> Thereisamismatchatx=0only.
==> Thereisaboundarylayeratx=0only.
Case2: a x( ) <0forx∈ 0,1⎡⎣ ⎤⎦
Arepresentativediagramofcharacteristicsisshownbelow.
==> Thereisamismatchatx=1only.==> Thereisaboundarylayeratx=1only.
Case3:
a x( ) = <0 , forx∈ 0, x0⎡⎣ )
>0 , forx∈ x0 ,1( ⎤⎦
⎧⎨⎪
⎩⎪
Arepresentativediagramofcharacteristicsisshownbelow.
x
t
x
t
AMS212BPerturbationMethods
- 5 -
==> Thereisamismatchatx=x0only.
==> Thereisaninternalboundarylayeratx=x0only.
Exampleofcase3:
ε ′′y +2 x − 12
⎛⎝⎜
⎞⎠⎟
′y +4 x − 12⎛⎝⎜
⎞⎠⎟
2
y =0 (wesolveditinLecture6).
Case4:
a x( ) = >0 , forx∈ 0, x0⎡⎣ )
<0 , forx∈ x0 ,1( ⎤⎦
⎧⎨⎪
⎩⎪
Arepresentativediagramofcharacteristicsisshownbelow.
==> Therearemismatchesatx=0andatx=1.
==> Thereareboundarylayersatx=0andatx=1.Exampleofcase4:
ε ′′y − x − 12
⎛⎝⎜
⎞⎠⎟
′y − y +2 x − 12⎛⎝⎜
⎞⎠⎟=0 (wesolveditinLecture6).
xx0
t
xx0
t
AMS212BPerturbationMethods
- 6 -
Remark: Thesolutioninthemiddleisdetachedfrombothboundaryconditions.Asaresult,itmaybevirtuallyundetermined.Intheexampleabove,settingx=½,theleadingtermsoftheODEgiveus
y(1/2)=0,whichservesasaanchoringcondition.WewillcomebacktotheanchoringproblemshortlyafterthediscussionofCases5A&B.
Case5A: a(x)≡0, b(x)<0
Characteristics:dx/dt=-a(x)=0,whichareverticallinesinthex-tplane.
Alongeachcharacteristic,wehave
dydt
= b x( ) y − c x( )( ) b(x)<0
==> y(x,t)convergestoc(x)ast→∞.==> y(x,∞)isdeterminedindependentoftwoboundaryconditions.
==> Therearemismatchesatx=0andatx=1.
==> Thereareboundarylayersatx=0andatx=1.Exampleofcase5A:
ε ′′y − y = −2sin x − 12
⎛⎝⎜
⎞⎠⎟, ε→0+ (wesolveditinLecture5)
Case5B: a(x)≡0, b(x)>0b(x)>0
==> y(x,t)divergesto±∞ast→∞.==> TheBVPisill-posed.
Exampleofcase5B:
ε ′′y − y = −2sin x − 12
⎛⎝⎜
⎞⎠⎟, ε→0− (wesolveditinLecture5)
Well-posednessoftheBVP(anchoringproblemincase4)
Whentherearetwoboundarylayers,anouterexpansionisdetachedfromimposedboundaryconditions.Asaresult,theouterexpansionmaybeundetermined.Thisisnotthe
AMS212BPerturbationMethods
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defectoftheasymptoticanalysis/method.Rather,thisiscausedbythefactthattheunderlyingBVPisalmostill-posed.Theexamplebelowillustratesthisill-posedness.Example:
ε ′′y −2 x − 12( ) ′y =0
y 0( ) =α , y 1( ) =β⎧⎨⎪
⎩⎪, ε→0+
Coefficientofy’:
a x( ) = −2 x − 1
2( ) = >0 , forx∈ 0, 12⎡⎣ )<0 , forx∈ 1
2 ,1( ⎤⎦
⎧⎨⎪
⎩⎪
==> Itiscase4.Outerexpansion:
Weseekanexpansionoftheform
y x( ) = a0 x( )+!
SubstitutingintotheODEyields
−2 x − 12
⎛⎝⎜
⎞⎠⎟a0′ =0
==> a0(x)=c
Question: Whyisconstantcundetermined?Answer: TheBVPisalmostsingular(ill-posed).
Anecessaryconditionforwell-posednessisthatthehomogeneousBVP
ε ′′y −2 x − 12( ) ′y =0
y 0( ) =0 , y 1( ) =0⎧⎨⎪
⎩⎪, ε→0+
hasonlythetrivialsolution,y(x)≡0.
ToshowthattheBVPisalmostsingular,weconstructafunctionu(x)suchthat§ u(x)almostsatisfiestheODE,
§ u(x)satisfiestheboundaryconditions,and§ u(0.5)≈1,
Theconstructionoffunctionu(x)isdescribedinAppendixA.
Methodofmulti-scaleexpansion
Wegobacktoinitialvalueproblems(IVP).
AMS212BPerturbationMethods
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Example:
′′y + ε ′y + y =0y 0( ) =1 , ′y 0( ) =0
⎧⎨⎪
⎩⎪, ε→0+
Physicalbackgroundoftheproblem:Oscillationofamass-springsystemwithsmallfriction.
(Drawamass-springsystem;introduceacoordinatesystemwithzpointingdownward)Newton’s2ndlaw:
m ′′z = − c ′zDragforce!"# −k z −LR( )
Elasticforce! "$ #$
+ gmGravity%
whereLRistherestlengthofthespring.Wewritetheequationas
m ′′z + c ′z +k z −LR −
gmk
⎛⎝⎜
⎞⎠⎟=0
Lety = z −LR −
gmk.Notethaty=0istherestposition.
PositionyisgovernedbytheIVP
′′y + cm
′y + kmy =0
y 0( ) = y0 , ′y 0( ) =0
⎧
⎨⎪
⎩⎪⎪
Note: Herethegravitydoesnotaffecttheequationaslongasthegravityisaconstant,independentofy.Later,wewillstudyacasewherethegravitychangeswithy.
Whenc=0,wehaveaharmonicoscillation.
′′y + k
my =0
==> ′′y +ω2 y =0
whereω = k
misthefrequencyoftheharmonicoscillation.
Ageneralsolutionis
y t( ) = c1 cos ωt( )+ c2sin ωt( ) Question: Whatdoes“smallfriction”mean?
AMS212BPerturbationMethods
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Answer: Weneedtolookatadimensionlessquantity.
Non-dimensionalization:
Wefirstidentifyatimescaleandalengthscalefornon-dimensionalization.
1time = ω⎡⎣ ⎤⎦ =
km
⎡
⎣⎢⎢
⎤
⎦⎥⎥
length = y0⎡⎣ ⎤⎦
Let
tnew = told
km, ynew =
yoldy0
Wehave
dydtold
= dydtnew
km
dydtold
2 = d2 ydtnew
2km
Substitutingintoequationyields
km
′′y tnew( )+ cmkm
′y tnew( )+ km y =0
==>′′y + c
mk′y + y =0
Weidentifythesmallparameter:
ε ≡ c
mk
“Smallfriction”meansε ≡ c
mk<<1 .
Thenon-dimensionalIVPis
′′y + ε ′y + y =0y 0( ) =1 , ′y 0( ) =0
⎧⎨⎪
⎩⎪
AMS212BPerturbationMethods
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Twotimescalesintheexactsolution:
Whenε=0,wehaveaperfectharmonicoscillation.
y(t)=cos(t)
Whenε<<1,wehaveanearlyharmonicoscillationandtheamplitudedecaysslowly.
Therearetwotimescalesintheproblem:a) theperiodofthenearlyharmonicoscillation: O(1)
b) thetimescaleoftheamplitudedecaying: O(1/ϵ)Thetwotimescalescanbeseenmathematicallyintheexactsolution.
Exactsolution:
Characteristicequation:
λ2 + ελ+1=0
==>λ1,2 =
−ε± ε2 −42 = −ε
2 ± i 1− ε2
4
Ageneralsolutionis
y t( ) = e
−ε2 t c1 cos 1− ε2
4 t + c2sin 1− ε2
4 t⎛
⎝⎜⎜
⎞
⎠⎟⎟
Applyingtheinitialconditionsy(0)=1andy’(0)=0,wehave
yext t( ) = e−ε2 t cos 1− ε2
4 t +ε21− ε2
4
sin 1− ε2
4 t
⎛
⎝
⎜⎜⎜⎜
⎞
⎠
⎟⎟⎟⎟
Theexactsolutionshowstwotimescales:
a) theperiodofthenearlyharmonicoscillation: 2π
b) thehalf-lifeoftheamplitudedecaying: 2εlog 2( )
Straightforwardexpansion:
AderivationofthestraightforwardexpansionfromthedifferentialequationisgivenintheAppendixB.Hereweobtainthestraightforwardexpansionviaashortcut,byTaylorexpandingtheexactsolution.WekeepO(1)termsandO(ϵ)termsintheTaylorexpansion.
AMS212BPerturbationMethods
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yext t( ) = e−ε2 t cos 1− ε2
4 t +ε21− ε2
4
sin 1− ε2
4 t
⎛
⎝
⎜⎜⎜⎜
⎞
⎠
⎟⎟⎟⎟
= 1− ε
2t +!⎛⎝⎜
⎞⎠⎟cost + ε
2sint +!⎛⎝⎜
⎞⎠⎟
= cost + ε 1
2sint −t2cost
⎛⎝⎜
⎞⎠⎟+!
Atwo-termstraightforwardexpansionis
yasy t( ) = cost + ε 1
2sint −t2cost
⎛⎝⎜
⎞⎠⎟
Letuslookattheperformanceoftheleadingterm,usingthesecondtermasanerrorindicator.
Error t( ) = yext t( )− cos t( )Leadingtermofyasy
!"# $#≈ ε2sint −
εt2 cost
Secondtermofyasy
! "### $###
Fort∈[0,O(1)],wehave
Error t( ) =O ε( )
Fort=O(1/ϵ),wehave
Error t( ) =O 1( ) Conclusion: Thestraightforwardexpansionisonlyvalidfort∈[0,O(1)].
NewGoal: Tofindaleadingtermexpansionthatisvaliduniformlyforlongtime.Thelargeerrorinthestraightforwardexpansionatlongtimeiscausedbytheterm(ϵtcost),whichiscalledasecularterm(aseculartermisanoscillatingtermwithagrowingamplitude).
Coefficient(ϵt)insecularterm(ϵtcost)comesfromexpandingexp(-ϵt/2).
Toaccommodatet∈[0,O(1/ϵ)],weshouldavoidexpandingexp(-ϵt/2).Letusseewhathappensifwedonotexpandexp(-ϵt/2).
AMS212BPerturbationMethods
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yext t( ) = e−ε2 t cos 1− ε2
4 t +ε21− ε2
4
sin 1− ε2
4 t
⎛
⎝
⎜⎜⎜⎜
⎞
⎠
⎟⎟⎟⎟
= e
−ε2 t cos t +O ε2t( )( )+O ε( )⎡
⎣⎤⎦
= e−ε2 t cos t( )+O ε2t( )+O ε( )⎡
⎣⎤⎦
==> yext t( ) = e−ε2 t cost +O ε( ) isvaliduniformlyfort∈[0,O(1/ϵ)].
Note: Fort≫O(1/ϵ),thesolutionisvirtuallyzerobecauseofthefactorexp(-ϵt/2).
Summary:
Toaccommodatet∈[0,O(1/ϵ)],weshouldavoidexpandingexp(-ϵt/2).
Strategyofmulti-scaleexpansion:
WetreatT0=tandT1=ϵtastwoseparatevariables.
(andthus,exp(-ϵt/2)iskeptasexp(-T1/2),insteadofbeingexpanded).
AMS212BPerturbationMethods
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AppendixAWeconstructafunctionu(x)suchthat
§ u(x)almostsatisfiestheODE: ε ′′y −2 x − 1
2( ) ′y = o εn( ) foranyn,§ u(x)satisfiestheboundaryconditions:
u(0)=0andu(1)=0, and
§ u(0.5)≈1,
Toconstructthefunction,westartbyexaminingtheexactsolutionofε ′′y −2 x − 12( ) ′y =0 .
Exactsolution:
ε ′′y −2 x − 12
⎛⎝⎜
⎞⎠⎟
′y =0
==>exp
− x − 12( )2
ε
⎛
⎝⎜
⎞
⎠⎟ ′y
⎛
⎝⎜
⎞
⎠⎟′
=0
==>exp
− x − 12( )2 + 1
4
ε
⎛
⎝⎜
⎞
⎠⎟ ′y = c0
==>′y x( ) = c0 exp
− 14 + x − 1
2( )2ε
⎛
⎝⎜
⎞
⎠⎟
==>y x( ) = c0 exp
− 14 + s − 1
2( )2ε
⎛
⎝⎜
⎞
⎠⎟ ds
0
x
∫ + c1
Weset y(0)=0andy(1)=2
(Notethaty(1)=2isnotthehomogeneousboundarycondition!)Weobtain
c1=0
c0 =2
exp − 14 + s − 1
2( )2ε
⎛
⎝⎜
⎞
⎠⎟ ds
0
1
∫= 1ε1+O ε( )( )
(Wewillstudyasymptoticexpansionsofintegralslater)
y 12
⎛⎝⎜
⎞⎠⎟=1 (symmetry)
AMS212BPerturbationMethods
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′y 12
⎛⎝⎜
⎞⎠⎟= c0 exp
− 14 + x − 1
2( )2ε
⎛
⎝⎜
⎞
⎠⎟x=12
= c0 exp−14ε
⎛⎝⎜
⎞⎠⎟ ≡ η ε( )
whereη ε( ) = 1
εexp −1
4ε⎛⎝⎜
⎞⎠⎟ 1+O ε( )( ) = o εn( ) foranyn
′′y 12
⎛⎝⎜
⎞⎠⎟= c0
2 x − 12( )
εexp
− 14 + x − 1
2( )2ε
⎛
⎝⎜
⎞
⎠⎟x=12
=0
Nextweconsider
y1 x( ) = y x( )− η ε( )x Functiony1(x)satisfies
y1(0)=0
y1′
12
⎛⎝⎜
⎞⎠⎟=0 , y1′′
12
⎛⎝⎜
⎞⎠⎟=0
ε ′′y1 −2 x − 12
⎛⎝⎜
⎞⎠⎟
′y1 = −2 x − 12⎛⎝⎜
⎞⎠⎟−η ε( )x( )′ =2η ε( ) x − 12
⎛⎝⎜
⎞⎠⎟
(Recallthaty(x)satisfiestheODEexactly.)
y1
12
⎛⎝⎜
⎞⎠⎟=1− η ε( )12 ≈1
Finally,weconsider
u x( ) = y1 x( ) , x ≤ 1
2
y1 1− x( ) , x > 12
⎧⎨⎪
⎩⎪
Functionu(x)satisfies
§ ε ′′y −2 x − 12( ) ′y = o εn( ) foranyn,
§ u(0)=0andu(1)=0, and§ u(0.5)≈1
Therefore,weconcludethattheBVP
AMS212BPerturbationMethods
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ε ′′y −2 x − 12( ) ′y =0
y 0( ) =α , y 1( ) =β⎧⎨⎪
⎩⎪, ε→0+
isveryclosetobeingsingular(althoughitisnotexactlysingular).
AppendixBWederiveastraightforwardexpansionoftheIVP
′′y + ε ′y + y =0y 0( ) =1 , ′y 0( ) =0
⎧⎨⎪
⎩⎪
Weseekanexpansionoftheform
y t( ) = a0 t( )+ εa1 t( )+!
Initialcondition:
a0(0)+ϵa1(0)+…=1 0 0( ) + 1 0( ) +! =1==> a0(0)=1, a1(0)=0
a0’(0)+ϵa1’(0)+…=0
==> a0’(0)=0, a1’(0)=0
Substitutingintotheequationyields
′′a0 + ε ′′a1( )+ ε ′a01( )+ a0 + εa1( ) =0 ==> ′′a0 +a0⎡⎣ ⎤⎦+ ε ′′a1 +a1 + ′a0⎡⎣ ⎤⎦ =0
Allcoefficientsmustbezero.
ε0:
′′a0 +a0 =0a0 0( ) =1 , ′a0 0( ) =0
⎧⎨⎪
⎩⎪
==> a0 t( ) = cos t( )
ε1:
′′a1 +a1 = − ′a0 = sinta1 0( ) =0 , ′a1 0( ) =0
⎧⎨⎪
⎩⎪
AMS212BPerturbationMethods
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LetA s( ) = L a1 t( )⎡⎣ ⎤⎦ .
TakingLaplacetransformyields
s2A s( )+ A s( ) = 1
s2 +1
==>
A s( ) = 1
s2 +1( )2
Recall
L−1 1
s2 +ω2( )⎡
⎣⎢⎢
⎤
⎦⎥⎥= sinωt
ω
Differentiatingwithrespecttoωyields
L−1 −2ω
s2 +ω2( )2⎡
⎣
⎢⎢⎢
⎤
⎦
⎥⎥⎥= −sinωt
ω2 + t cosωtω
==>
L−1 1
s2 +ω2( )2⎡
⎣
⎢⎢⎢
⎤
⎦
⎥⎥⎥= 12ω2
sinωtω
−t cosωt⎛⎝⎜
⎞⎠⎟
==>
a1 t( ) = L−1 1
s2 +1( )2⎡
⎣
⎢⎢⎢
⎤
⎦
⎥⎥⎥= 12 sint −t cost( )
==>yasy t( ) = cos t( )+ ε12 sint −t cost⎡⎣ ⎤⎦