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arXiv:quant-ph/0208026 v1 5 Aug 2002

P ath Integrals and Their Application to Dissipative Quantum Systems Gert-Ludwig Ingold Institut f ur Physik, Universit at Augsburg, D-86135 Augsburg to b e published in \Coheren tE v olution in Noisy En vironmen ts", Lecture Notes in Ph ysics, http://link.spri nger. de/s eries /lnpp c Springer V erlag, Berlin-Heidelb erg-New Y ork

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Gert-LudwigIngold

Institutf urPhysik, UniversitatAugsburg,D-86135Augsburg,Germany

1 Introduction

Thecouplingofasystemtoitsenvironmentisarecurrentsubject inthis

collec-tionoflecturenotes.Theconsequencesofsuchacouplingarethreefold.Firstof

all,energymayirreversiblyb e transferredfromthesystemto theenvironment

therebygivingrisetothephenomenonofdissipation.Inaddition,the uctuating

forceexertedbytheenvironmentonthesystemcauses uctuationsofthesystem

degreeoffreedomwhichmanifestitselfforexampleasBrownianmotion.While

thesetwoe ectso ccurb othforclassicalaswellasquantumsystems,thereexists

athird phenomenon which issp eci c to thequantumworld.As aconsequence

of the entanglement b etween system and environmentaldegrees of freedom a

coherentsup erp ositionofquantumstatesmayb edestroyedinapro cess referred

to as decoherence. This e ect is of majorconcern ifone wantsto implementa

quantumcomputer.Therefore,decoherence isdiscussed indetailinChap.5.

Quantum computation,however, is by no means the only topic where the

couplingto anenvironmentisrelevant.Infact,virtuallynorealsystemcan b e

consideredascompletelyisolatedfromitssurroundings.Therefore,the

phenom-ena listed in the previous paragraph play arole inmany areas of physics and

chemistryandaseriesofmetho dshasb eendevelop edtoaddressthis situation.

Someapproacheslikethemasterequationsdiscussed inChap.2areparticularly

well suited if the coupling to the environmentis weak, a situation desired in

quantumcomputing.Ontheotherhand,inmanysolidstate systems,the

envi-ronmentalcouplingcan b eso strongthat weakcouplingtheories are nolonger

valid.Thisistheregimewherethepathintegralapproachhasproventob every

useful.

Itwouldb eb eyondthescop eofthischaptereventoattempttogivea

com-pleteoverviewoftheuseofpathintegralsinthedescriptionofdissipative

quan-tumsystems.Inparticularforatwo-levelsystemcoupledtoharmonicoscillator

degrees of freedom,theso-calledspin-b oson mo del,quiteanumb erof

approx-imations have b een develop ed which are useful in their resp ective parameter

regimes.Thischapterratherattemptsto give anintro ductionto pathintegrals

forreaders unfamiliarwithbutinterestedinthis metho danditsapplicationto

dissipativequantumsystems.

Inthis spirit,Sect. 2gives anintro ductionto path integrals.Some asp ects

discussed in this section are not necessarily closely related to the problem of

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weelab orateonthegeneralideaofthecouplingofasystemtoanenvironment.

Thepathintegralformalismisemployedtoeliminatetheenvironmentaldegrees

of freedom and thus to obtain ane ective description of the systemdegree of

freedom.Theresultsprovidethebasisforadiscussionofthedamp edharmonic

oscillatorinSect.4.Startingfromthepartitionfunctionwewillexamineseveral

asp ects ofthisdissipative quantumsystem.

Readers interested inamorein-depth treatmentof thesubject of quantum

dissipationarereferred to existingtextb o oks.In particular,we recommendthe

b o ok by U. Weiss [1] which provides an extensive presentation of this topic

togetherwithacomprehensivelistofreferences.Chapter4of[2]mayserve asa

moreconciseintro ductioncomplementarytothepresentchapter.Pathintegrals

are discussed in a whole variety of textb o oks with an emphasis either on the

physicalorthemathematicalasp ects.Weonlymentiontheb o okbyH.Kleinert

[3] which gives adetailed discussion ofpath integrals andtheir applicationsin

di erentareas.

2 Path Integrals

2.1 Intro duction

Themostoften usedand taughtapproach to nonrelativisticquantum

mechan-ics is based on the Schrodinger equation which p ossesses strong ties with the

the Hamiltonian formulationof classicalmechanics. Thenonvanishing Poisson

bracketsb etween p ositionandmomentuminclassicalmechanicsleadus to

in-tro ducenoncommutingop eratorsinquantummechanics.TheHamiltonfunction

turnsintotheHamiltonop erator,thecentralobjectintheSchrodingerequation.

One of the mostimp ortanttasks isto nd theeigenfunctions of theHamilton

op erator and the asso ciated eigenvalues. Decomp osition of a state into these

eigenfunctionsthenallowsusto determineitstimeevolution.

As an alternative, there exists a formulation of quantum mechanics based

on the Lagrange formalismof classical mechanics with the action as the

cen-tral concept. This approach, which was develop ed by Feynman in the 1940's

[4,5],avoidstheuseofop eratorsthoughthisdo esnotnecessarilymeanthatthe

solution of quantummechanicalproblems b ecomes simpler. Instead of nding

eigenfunctions of aHamiltonianone now has to evaluate afunctionalintegral

which directly yields the propagator required to determinethe dynamicsof a

quantumsystem.Since therelationb etween Feynman'sformulationand

classi-calmechanicsisveryclose,thepathintegralformalismoftenhastheimp ortant

advantageofprovidingamuchmoreintuitiveapproachaswe willtrytoconvey

tothereader inthefollowingsections.

2.2 Propagator

Inquantummechanics,one often needs todetermine thesolutionj (t)i ofthe

time-dep endentSchrodingerequation

i~ @j i

(5)

whereHistheHamiltoniandescribingthesystem.Formally,thesolutionof(1) mayb e writtenas j (t)i=T exp  i ~ Z t 0 dt 0 H(t 0 )  j (0)i: (2)

Here,thetimeorderingop eratorT isrequiredb ecausetheop eratorscorresp

ond-ing to the Hamiltonianat di erent times in general due not commute.In the

following,wewillrestrictourselvestotime-indep endentHamiltonianswhere(2)

simpli esto j (t)i=exp  i ~ Ht  j (0)i: (3)

Astheinsp ectionof(2)and(3)demonstrates,thesolutionofthetime-dep endent

Schrodingerequationcontainstwoparts:theinitialstate j (0)iwhich servesas

aninitialconditionandtheso-calledpropagator,anop eratorwhichcontainsall

informationrequired todeterminethetimeevolutionofthesystem.

Writing(3)inp ositionrepresentation one nds

hxj (t)i= Z dx 0 hxjexp  i ~ Ht  jx 0 ihx 0 j (0)i (4) or (x;t)= Z dx 0 K(x;t;x 0 ;0) (x 0 ;0) (5)

withthepropagator

K(x;t;x 0 ;0)=hxjexp  i ~ Ht  jx 0 i: (6)

It is preciselythis propagatorwhich isthe central object ofFeynman's

formu-lationofquantummechanics.Before discussingthepathintegralrepresentation

ofthepropagator,itisthereforeusefulto take alo okatsomeprop ertiesofthe

propagator.

Insteadofp erformingthetimeevolutionofthestatej (0)iintoj (t)iinone

step as was doneinequation(3), one couldenvisagetop erformthis pro cedure

intwosteps by rstpropagating theinitialstate j (0)i up to anintermediate

timet

1

and takingthe newstate j (t

1

)ias initialstate forapropagation over

thetimet t

1

.Thisamountstoreplacing(3) by

j (t)i=exp  i ~ H(t t 1 )  exp  i ~ Ht 1  j (0)i (7) orequivalently (x;t)= Z dx 0 Z dx 00 K(x;t;x 00 ;t 1 )K(x 00 ;t 1 ;x 0 ;0) (x 0 ;0): (8)

Comparing(5)and (8),we ndthesemigroupprop ertyofthepropagator

K(x;t;x 0 ;0)= Z dx 00 K(x;t;x 00 ;t )K(x 00 ;t ;x 0 ;0): (9)

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0 t 1 t x 0 x

Fig.1. According tothesemigroupprop erty(9)thepropagatorK(x;t;x

0

;0)may b e

decomp osedintopropagatorsarrivingatsometimet

1

atanintermediatep ointx

00 and

propagatorscontinuingfromtheretothe nalp ointx

This result is visualized in Fig. 1 where the propagators b etween space-time

p ointsare depicted bystraight lines connecting thecorresp onding two p oints.

Attheintermediatetimet

1

onehastointegrateoverallp ositionsx

00

.Thisinsight

willb eofusewhenwediscussthepathintegralrepresentationofthepropagator

lateron.

Thepropagator containsthe complete informationab outthe eigenenergies

E n

andthecorresp ondingeigenstatesjni.Makinguseofthecompletenessofthe

eigenstates,one ndsfrom(6)

K(x;t;x 0 ;0)= X n exp  i ~ E n t  n (x) n (x 0 )  : (10)

Here, thestardenotescomplexconjugation.Not onlydo esthepropagator

con-tain the eigenenergies and eigenstates, this informationmay also b e extracted

fromit.Tothisend,weintro ducetheretarded Greenfunction

G r (x;t;x 0 ;0)=K(x;t;x 0 ;0)

Θ

(t) (11)

where

Θ

(t)istheHeavisidefunctionwhichequals1forp ositiveargumenttand

is zero otherwise. Performing a Fourier transformation,one ends up with the

sp ectralrepresentation G r (x;x 0 ;E)= i ~ Z 1 0 dtexp  i ~ Et  G r (t) = X n n (x) n (x 0 )  E E n +i" ; (12)

where "is anin nitely smallp ositive quantity.According to (12),thep oles of

the energy-dep endent retarded Green functionindicate the eigenenergies while

thecorresp ondingresiduacanb e factorizedintotheeigenfunctionsatp ositions

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2.3 FreeParticle

Animp ortantsteptowardsthepathintegralformulationofquantummechanics

can b e made by considering thepropagator of a free particle of mass m. The

eigenstates ofthecorresp ondingHamiltonian

H=

p 2

2m

(13)

aremomentumeigenstates

p (x)= 1 p 2 ~ exp  i ~ px  (14)

with a momentumeigenvalue pout of a continuous sp ectrum. Inserting these

eigenstates intotherepresentation(10)ofthepropagator,one ndsbyvirtueof

Z 1 1 dxexp( iax 2 )= r  ia = r  a exp  i  4  (15)

forthepropagatorofthefree particletheresult

K(x f ;t;x i ;0)= 1 2 ~ Z dpexp  i ~ p 2 2m t  exp  i ~ p(x f x i )  = r m 2 i~t exp  i ~ m(x f x i ) 2 2t  : (16)

Itwasalready noted byDirac[6]that thequantummechanicalpropagator

and the classical prop erties of a free particle are closely related. In order to

demonstratethis, we evaluate theaction ofa particlemovingfrom x

i

to x

f in

timet.Fromtheclassicalpath

x cl (s)=x i +(x f x i ) s t (17)

ob eyingtheb oundaryconditionsx

cl (0)=x i andx cl (t)=x f

,thecorresp onding

classicalactionisfoundas

S cl = m 2 Z t 0 dsx_ 2 cl = m 2 (x f x i ) 2 t : (18)

This result enables us to express the propagator of a free particle entirely in

termsoftheclassicalactionas

K(x f ;t;x i ;0)=  1 2 i~ @ 2 S cl (x f ;t;x i ;0) @x f @x i  1=2 exp  i ~ S cl (x f ;t;x i ;0)  : (19)

This result isquiteremarkableandone mightsusp ect that it isdueto ap

ecu-liarityofthefreeparticle.However,sincethepropagationinageneralp otential

(intheabsence ofdeltafunctioncontributions)mayb edecomp osedintoaseries

ofshort-timepropagationsofafree particle, theresult (19)mayindeedb e

em-ployedtoconstructarepresentationofthepropagatorwheretheclassicalaction

app earsintheexp onent.Intheprefactor,theactionapp earsintheformshown

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2.4 PathIntegralRepresentationofQuantumMechanics

Whileavoidingtogoto o deeplyinto themathematicaldetails,we nevertheless

wanttosketch thederivationofthepathintegralrepresentationofthe

propaga-tor. Themainideaistodecomp ose thetimeevolutionover a nite timet into

N slicesofshorttimeintervalst=t=N wherewewilleventuallytakethelimit

N !1.Denotingtheop eratorofthekineticandp otentialenergybyT andV,

resp ectively, we thus nd

exp  i ~ Ht  =  exp  i ~ (T +V)t  N : (20)

For simplicity,we willassume that theHamiltonianis time-indep endent even

thoughthefollowingderivationmayb egeneralizedtothetime-dep endentcase.

Wenowwouldliketo decomp osetheshort-timepropagatorin(20)into apart

dep ending onthekineticenergy andanother part containingthep otential

en-ergy. However, since the two op erators do not commute,we have to exercise

somecaution.FromanexpansionoftheBaker-Hausdor formulaone nds

exp  i ~ (T +V)t  exp  i ~ Tt  exp  i ~ Vt  + 1 ~ 2 [T;V](t) 2 (21)

where termsoforder(t)

3

andhigherhaveb een neglected.Sincewe are

inter-ested inthe limitt!0,wemayneglect the contributionof thecommutator

andarrive attheTrotter formula

exp  i ~ (T +V)t  = lim N!1 [U(t)] N (22)

withtheshorttimeevolutionop erator

U(t)=exp  i ~ Tt  exp  i ~ Vt  : (23)

What we have presented here is, of course, at b est amotivationand certainly

do es not constitute a mathematical pro of. We refer readers interested in the

detailsofthepro ofandtheconditionsunderwhichtheTrotterformulaholdsto

theliterature[7].

Inp ositionrepresentation onenowobtainsforthepropagator

K(x f ;t;x i ;0)= lim N!1 Z 1 1 0 @ N 1 Y j=1 dx j 1 A hx f jU(t)jx N 1 i::: hx 1 jU(t)jx i i : (24)

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element hx j+1 jU(t)jx j i=  x j+1 exp  i ~ Tt  x j  exp  i ~ V(x j )t  = r m 2 i~t exp  i ~  m 2 (x j+1 x j ) 2 t V(x j )t  : (25)

Wethusarriveatour nalversionofthepropagator

K(x f ;t;x i ;0)= lim N!1 r m 2 i~t Z 1 1 0 @ N 1 Y j=1 dx j r m 2 i~t 1 A exp 2 4 i ~ N 1 X j=0 m 2  x j+1 x j t  2 V(x j ) ! t 3 5 (26) wherex 0 andx N

shouldb eidenti edwithx

i

andx

f

,resp ectively.The

discretiza-tionofthepropagatorusedinthisexpressionisaconsequence oftheform(21)

of the Baker-Hausdor relation. In lowest order in t, we could have used a

di erentdecomp ositionwhichwouldhaveledtoadi erentdiscretizationofthe

propagator.Foradiscussionofthemathematicalsubtleties werefer thereader

to[8].

Remarkingthat the exp onent in(26) containsa discretized version of the

action S[x]= Z t 0 ds  m 2 _ x 2 V(x)  ; (27)

wecan writethisresult inshortnotationas

K(x f ;t;x i ;0)= Z D xexp  i ~ S[x]  : (28)

The action (27) is a functional which takes as argument a function x(s) and

returns anumb er,theactionS[x].Theintegral in(28)thereforeisafunctional

integral where one has to integrate over all functions satisfyingthe b oundary

conditionsx(0)=x

i

andx(t)=x

f

. Sincethese functions represent paths,one

refers tothiskindoffunctionalintegralsalsoaspathintegral.

The three lines shown in Fig. 2 represent the in nity of paths satisfying

theb oundary conditions.Amongthemthe thickerline indicatesasp ecialpath

corresp ondingtoanextremumoftheaction.Accordingtotheprincipalofleast

actionsuchapathisasolutionoftheclassicalequationofmotion.Itshould b e

noted,however,thateventhoughsometimesthereexistsauniqueextremum,in

generalthere mayb emorethanone orevennone.Ademonstrationofthisfact

willb eprovidedinSect.2.7wherewewilldiscussthedrivenharmonicoscillator.

Theother paths depicted inFig. 2may b e interpreted as quantum

uctu-ations around the classicalpath. As we willsee in Sect. 2.8, theamplitude of

these uctuations is typicallyof the order of

p

(10)

t

Fig.2. Thethick line representsaclassical path satisfying the b oundary conditions.

The thinner lines are no solutions of the classical equation of motion and may b e

asso ciated withquantum uctuations

Beforeexplicitlyevaluatingapathintegral,wewanttodiscusstwoexamples

whichwillgive ussomeinsightintothedi erence of theapproacheso ered by

theSchrodinger andFeynmanformulationofquantummechanics.

2.5 Particleona Ring

We con ne aparticle of mass m to aring of radius R and denote its angular

degree offreedomby.This systemisdescrib ed bytheHamiltonian

H= ~ 2 2mR 2 @ 2 @ 2 : (29)

Requiring thewave functionto b e continuous and di erentiable,one nds the

stationarystates ` ()= 1 p 2 exp(i`) (30)

with`=0;1;2;::: andtheeigenenergies

E ` = ~ 2 ` 2 2mR 2 : (31)

These solutionsof thetime-indep endentSchrodinger equation allowus to

con-struct thepropagator

K( f ;t; i ;0)= 1 2 1 X `= 1 exp  i`( f  i ) i ~` 2 2mR 2 t  : (32)

Wenowwanttoderivethisresultwithinthepathintegralformalism.Tothis

end we willemploythepropagatorof thefree particle. However,animp ortant

di erenceb etweenafreeparticleandaparticleonaringdeservesourattention.

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 i f  i f n=0 n=1

Fig.3. Onaring,theangles

f

and

f

+2 nhavetob eidenti ed.Asaconsequence,

thereexistin nitely manyclassicalpathsconnecting twop ointsonaring,whichmay

b eidenti edby theirwinding numb er n

pathsconnecting 

i

and 

f

. Allthese pathsare top ologicallydi erent andcan

b echaracterizedbytheirwindingnumb ern.Asanexample,Fig.3showsapath

forn=0andn=1.Due totheirdi erent top ology,these twopaths(and any

twopathscorresp ondingto di erentwindingnumb ers) cannotb e continuously

transformedintoeachother.Thisimpliesthataddinga uctuationtooneofthe

classicalpathswillnever changeitswindingnumb er.

Therefore,we haveto sumoverallwindingnumb ersinorderto accountfor

allp ossible paths.Thepropagatorthusconsists ofasumover free propagators

corresp ondingtodi erentwindingnumb ers

K( f ;t; i ;0)= 1 X n= 1 R r m 2 i~t exp  i ~ mR 2 2 ( f  i 2 n) 2 t  : (33)

Here,thefactorRaccountsforthefact that,incontrasttothefreeparticle,the

co ordinate isgivenbyanangleinstead ofap osition.

Thepropagator(33)is2 -p erio dicin

f 

i

andcantherefore b eexpressed

intermsofaFourierseries

K( f ;t; i ;0)= 1 X `= 1 c ` exp[i`( f  i )] : (34)

TheFourierco eÆcientsarefoundtoread

c ` = 1 2 exp  i ~` 2 2mR 2 t  (35)

which proves the equivalence of (33) with our previous result (32). We thus

have obtained the propagatorof a free particle on a ring b oth by solvingthe

Schrodinger equation and by employing pathintegral metho ds.These two

ap-proaches make use of complementary representations. In the rst case,this is

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0 x i x f L 1 2 3 4 5

Fig.4. The re ection at the walls of a b ox leads to an in nite numb er of p ossible

trajectoriesconnectingtwop ointsin theb ox

2.6 Particleina Box

Another textb o ok exampleinstandard quantummechanicsis theparticle ina

b oxoflengthLcon nedby in nitelyhigh wallsatx=0andx=L. Fromthe

eigenvalues E j = ~ 2  2 j 2 2mL 2 (36)

withj=1;2;::: andthecorresp ondingeigenfunctions

j (x)= r 2 L sin   j x L  (37)

thepropagatorisimmediatelyobtainedas

K(x f ;t;x i ;0)= 2 L 1 X j=1 exp  i ~ 2 j 2 2mL 2 t  sin   j x f L  sin   j x i L  : (38)

It to ok some time until this problem was solved within the path integral

approach[9,10].Here,wehavetoconsiderallpathsconnectingthep ointsx

i and

x f

withinap erio doftimet.Duetothere ectingwalls,thereagainexistin nitely

manyclassicalpaths, veofwhicharedepictedinFig.4.However,incontrastto

thecaseofaparticleonaring,these pathsarenolongertop ologicallydistinct.

Asaconsequence,we maydeformaclassicalpathcontinuouslytoobtainoneof

theotherclassicalpaths.

If,forthemoment,wedisregardthedetailsofthere ectionsatthewall,the

motionoftheparticleinab oxisequivalenttothemotionofafree particle.The

fact that paths are foldedback on themselves can b e accounted for by taking

into account replicas of the b ox as shown in Fig. 5. Now, the path do es not

necessarily endat x

(0) f

=x

f

but atone ofthemirrorimagesx

(n) f

where nisan

arbitrary integer. In order to obtainthe propagator,we willhave to sum over

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1 2 3 4 5 x ( 2) f x ( 1) f x f x (1) f x (2) f x i

Fig.5. Insteadofaparticlegettingre ectedatthewallsoftheb oxonemaythink of

afreeparticlemovingfromthestarting p ointintheb oxtotheendp ointinoneofthe

replicasoftheb ox

canseethatforano ddnumb er2n 1ofre ections,theendp ointliesat2nL x

f

andthecontributiontothefullpropagatortherefore isgivenby

K (2n 1) (x f ;t;x i ;0)= r m 2 i~t exp  i ~ m(2nL x f x i ) 2 2t  : (39)

Ontheotherhand,foranevennumb er2nofre ections, theendp ointislo cated

at2nL+x f andwe nd K (2n) (x f ;t;x i ;0)= r m 2 i~t exp  i ~ m(2nL+x f x i ) 2 2t  : (40)

However,itisnotobviousthatjust summingupthepropagators (39)and(40)

forallnwilldothejob.

Inorderto clarifythis p oint,we startwiththesomewhat simplersituation

ofjust onewallandtakealo okatallpathsrunningb etween x

i

andx

f

intime

t.As canb e seen fromthespace-time diagraminFig.6there arepathswhich

do not cross the walland which therefore contribute to the pathintegral. On

the other hand,there exist also pathswhich cross the wallan even numb erof

times.Sincethese pathssp end sometimeinthe forbiddenregion, they donot

contributetothepathintegral.

Itrequiressomethinkingtoensurethatonlypathsnotcrossing thewallare

takenintoaccount.Ourstrategywillconsistin rstwritingdownapropagator

K free

whichdisregardsthewall.Then,wehave tosubtracto thecontributions

of allthepaths which cross thewall.This can b edone byconstructing apath

withthesameactionastheoriginalpath.Tothisendwe take theoriginalpath

upto thelastcrossing withthewallandthencontinue alongthemirrorimage

oftheoriginalpath.Wethusendupatthemirrorimage x

f

oftheoriginalend

p ointx

f

.Note that apathrunning fromx

i

to x

f

necessarilycrosses thewall

at leastonce.As aconsequence, subtractingthepropagatorb etween these two

p ointseliminates all originalpaths which do not remain inthe region x > 0.

Wetherefore obtainourdesired result,thepropagatorK

wall

inthe presence of

a wall,by subtracting a propagator going to the re ected end p ointfrom the

unconstrainedpropagatortotheoriginalendp oint[9,10,11]

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x x i x f 0 x f

Fig.6. Apath crossingthewalliscancelledbyapathrunning tothemirror p oint of

theendp oint

This result b ears muchresemblance withthemetho dof imagecharges in

elec-trostatics.Aftergivingitsomethought,this shouldnotb e to osurprisingsince

thefreeSchrodinger equationandthePoissonequationareformallyequivalent.

Accordingtothemetho dofimagechargesonemayaccountforametallicplate

(i.e. the wall)by putting a negative charge(i.e. the mirrored end p oint)

com-plementingthep ositive charge(i.e.theoriginalend p oint).For thepropagator

thisresults inthedi erence app earingin(41).

Letusnowcomebacktoourin nitelydeepp otentialwellwithtwowalls.This

problemcorresp ondstotheelectrostaticsofachargeb etweentwoparallelmetal

plates. In this case, the metho d of image charges leads to an in nitenumb er

of charges of alternating signs. The original p ositive charge gives rise to two

negativechargeswhichareeachanimagecorresp ondingtooneofthetwometal

plates. Inaddition,however,these imageshave mirrorimagescorresp onding to

theothermetalplateandthispro cess hastob ecarriedonadin nitum.

Expressing the propagator of the particle in the b ox in terms of the free

propagator works in exactly the same way. A path intersecting b oth walls is

subtracted twice, i.e.one timeto ooften.Therefore, one contributionhasto b e

restored which is donebyaddinganother endp oint. Continuingthe pro cedure

oneendsupwithanin nitenumb erofendp oints,someofwhichwehaveshown

inFig. 5.As a consequence, we can attribute a signto each end p ointin this

gure. The general rule which follows from these considerations is that each

re ection atawallleadstofactor 1.Thepropagatortherefore canb e written

as K(x f ;t;x i ;0)= r m 2 i~t 1 X n= 1 " exp  i ~ m(2nL+x f x i ) 2 2t  exp  i m(2nL x f x i ) 2  # : (42)

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Thesymmetries K(x f +2L;t;x i ;0)=K(x f ;t;x i ;0) (43) K( x f ;t;x i ;0)= K(x f ;t;x i ;0) (44)

suggest toexpandthepropagatorintotheFourierseries

K(x f ;t;x i ;0)= 1 X j=1 a j (x i ;t)sin   j x f L  : (45)

ItsFourierco eÆcientsareobtainedfrom(42)as

a j (x i ;t)= 1 L Z L L dx f sin   j x f L  K(x f ;t;x i ;0) = 2 L sin   j x i L  exp  i ~ E j t  (46)

wheretheenergiesE

j

aretheeigenenergies oftheb oxde ned in(36).Inserting

(46)into(45)we thusrecoverourprevious result(38).

2.7 DrivenHarmonic Oscillator

Eventhoughthesituationsdealtwithintheprevioustwosectionshaveb een

con-ceptuallyquiteinteresting, we couldinb othcases avoidtheexplicitcalculation

ofapathintegral.Inthepresentsection,we willintro ducethebasictechniques

needed to evaluate path integrals.As an example, we willconsider the driven

harmonic oscillator which is simple enough to allow for an exact solution. In

addition, the propagator willb e of use inthe discussion of damp ed quantum

systems inlatersections.

Ourstartingp ointistheLagrangian

L= m 2 _ x 2 m 2 ! 2 x 2 +xf(t) (47)

of aharmonicoscillator with massm and frequency ! . Theforce f(t) mayb e

duetoanexternal eld,e.g.anelectric eldcouplingviadip oleinteractiontoa

chargedparticle.Inthecontextofdissipativequantummechanics,theharmonic

oscillator could represent a degree of freedom of the environment under the

in uenceof aforceexerted bythesystem.

Accordingto(28)weobtainthepropagatorK(x

f

;t;x

i

;0)bycalculatingthe

actionforall p ossiblepathsstartingat timezero atx

i

and endingat timet at

x f

.Itisconvenienttodecomp ose thepaths

x(s)=x

cl

(s)+(s) (48)

intotheclassicalpathx

cl

satisfyingtheb oundaryconditionsx

cl (0)=x i ,x cl (t)= x f

anda uctuatingpartvanishingattheb oundaries,i.e.(0)=(t)=0.The

classicalpathhastosatisfytheequationofmotion

mx +m!

2

(16)

obtainedfromtheLagrangian(47).

Foranexactlysolvableproblemlikethedrivenharmonicoscillator,wecould

replace x

cl

by any path satisfying x(0) = x

i

, x(t) = x

f

. We leave it as an

exercise to the reader to p erform the following calculation with x

cl

(s) of the

drivenharmonicoscillatorreplacedbyx

i +(x

f x

i

)s=t.However,itisimp ortant

to note that within the semiclassical approximation discussed in Sect. 2.8 an

expansion around the classical path is essential since this path leads to the

dominantcontributiontothepathintegral.

With(48)we obtainfortheaction

S= Z t 0 ds  m 2 _ x 2 m 2 ! 2 x 2 +xf(s)  = Z t 0 ds  m 2 _ x 2 cl m 2 ! 2 x 2 cl +x cl f(s)  + Z t 0 ds  mx_ cl _  m! 2 x cl +f(s)  + Z t 0 ds  m 2 _  2 m 2 ! 2  2  : (50)

Forourcaseofaharmonicp otential,thethirdtermisindep endentoftheb

ound-aryvaluesx

i

andx

f

aswellasoftheexternaldriving.Thesecondtermvanishes

as aconsequence of the expansion aroundthe classicalpath.This can b e seen

bypartialintegrationandbymakinguseofthefactthatx

cl

isasolutionofthe

classicalequationofmotion:

Z t 0 ds mx_ cl _  m! 2 x cl +f(s)  = Z t 0 ds mx cl +m! 2 x cl f(s)  =0: (51)

We now pro ceed in two steps by rst determining the contribution of the

classicalpathandthenaddressingthe uctuations.Thesolutionoftheclassical

equationofmotionsatisfyingtheb oundaryconditionsreads

x cl (s)=x f sin(! s) sin(! t) +x i sin(! (t s)) sin(! t) (52) + 1 m! Z s 0

dusin(! (s u))f(u)

sin(! s) sin(! t) Z t 0 dusin(! (t u))f(u)  :

A p eculiarity of the harmonic oscillator in the absence of driving is the

ap-p earance of conjugate p oints at times T

n

= ( =! )n where n is an arbitrary

integer.Sincethefrequency oftheoscillationsisindep endentoftheamplitude,

thep ositionoftheoscillatoratthesetimesisdeterminedbytheinitialp osition:

x(T 2n+1 ) = x i and x(T 2n ) = x i

. This also illustrates the fact mentioned on

(17)

t

Fig.7. Inaharmonicp otentialalltrajectoriesemergingfromthesamestartingp oint

convergeatconjugatep ointsatmultiplesofhalfanoscillation p erio d

Thetaskofevaluatingtheactionoftheclassicalpathmayb e simpli edby

apartialintegration S cl = Z t 0 ds  m 2 _ x 2 cl m 2 ! 2 x 2 cl +x cl f(s)  = m 2 x cl _ x cl t 0 Z t 0 ds  m 2 x cl  x cl + m 2 ! 2 x 2 cl x cl f(s)  = m 2 (x f _ x cl (t) x i _ x cl (0))+ 1 2 Z t 0 dsx cl (s)f(s) (53)

where wehavemadeuseoftheclassicalequationofmotiontoobtainthethird

line.Fromthesolution(52)oftheclassicalequationofmotionwe get

_ x cl (0)=! x f x i cos(! t) sin(! t) 1 msin (! t) Z t 0 dssin (! (t s))f(s) (54) _ x cl (t)=! x f cos(! t) x i sin(! t) + 1 msin (! t) Z t 0 dssin (! s)f(s): (55)

Insertinginitialand nalvelo cityinto(53)we ndfortheclassicalaction

S cl = m! 2sin(! t)  (x 2 i +x 2 f )cos (! t) 2x i x f  + x f sin(! t) Z t 0 dssin (! s)f(s)+ x i sin(! t) Z t 0 dssin(! (t s))f(s) 1 m!sin(! t) Z t 0 ds Z s 0

dusin(! u)sin (! (t s))f(s)f(u):

(56)

As asecond step, we have to evaluate the contribution of the uctuations

whichisdeterminedbythethirdtermin(50).Afterpartialintegrationthisterm

b ecomes S (2) = Z t ds  m 2 _  2 m 2 ! 2  2  = Z t ds m 2   d 2 ds 2 +! 2   : (57)

(18)

Here, the sup erscript `(2)'indicates that this term corresp onds to the

contri-bution of second orderin . Inviewof theright-handside it isappropriate to

expandthe uctuation

(s)= 1 X n=1 a n  n (s) (58) intoeigenfunctionsof  d 2 ds 2 +! 2   n = n  n (59) with  n (0)= n

(t)=0.As eigenfunctionsof aselfadjointop erator, the

n are

completeandmayb echosenorthonormal.Solving(59)yieldstheeigenfunctions

 n (s)= r 2 t sin   n s t  (60)

andcorresp ondingeigenvalues

 n =   n t  2 +! 2 : (61)

Weemphasizethat (58)is nottheusualFourier seriesonanintervaloflength

t.Such anexpansioncouldb eusedintheform

(s)= r 2 t 1 X n=1 h a n  cos (2 n s t ) 1  +b n sin(2 n s t ) i (62)

which ensures that the uctuations vanish at the b oundaries. We invite the

reader toredo thefollowingcalculationwiththeexpansion(62)replacing(58).

Whileattheendthesamepropagatorshouldb efound,itwillb ecomeclearwhy

theexpansionintermsofeigenfunctionssatisfying(59)ispreferable.

Theintegrationover the uctuations now b ecomes an integration over the

expansionco eÆcientsa

n

.Insertingtheexpansion(58)intotheactionone nds

S (2) = m 2 1 X n=1  n a 2 n = m 2 1 X n=1    n t  2 ! 2  a 2 n : (63)

Asthisresult shows,theclassicalactionisonlyanextremumoftheactionbut

not necessarily a minimum although this is the case for short time intervals

t <  =! . The existence of conjugate p oints at times T

n

= n =! mentioned

ab ovemanifestsitselfhereas vanishingoftheeigenvalue

n

.Thentheactionis

indep endentofa

n

whichimpliesthat foratimeintervalT

n allpathsx cl +a n  n

witharbitraryco eÆcienta

n

aresolutionsoftheclassicalequationofmotion.

Afterexpansion of the uctuations intermsof the eigenfunctions(60),the

propagatortakestheform

K(x f ;t;x i ;0)exp  i ~ S cl Z 1 Y da n ! exp i ~ m 2 1 X  n a 2 n ! : (64)

(19)

Inprinciple,weneedtoknowtheJacobideterminantofthetransformationfrom

thepathintegraltotheintegralovertheFourierco eÆcients.However,sincethis

Jacobi determinant is indep endent of the oscillator frequency ! , we may also

compare with the free particle. Evaluating the Gaussian uctuationintegrals,

we nd for theratio b etween the prefactors of thepropagators K

!

and K

0 of

theharmonicoscillatorand thefree particle,resp ectively,

K ! exp[ (i=~)S cl ;! ] K 0 exp[ (i=~)S cl ;0 ] = r D 0 D : (65)

Here,wehaveintro ducedthe uctuationdeterminantsfortheharmonic

oscilla-tor D=det  d 2 ds 2 +! 2  = 1 Y n=1  n (66)

andthefreeparticle

D 0 =det  d 2 ds 2  = 1 Y n=1  0 n : (67)

Theeigenvaluesforthefreeparticle

 0 n =   n t  2 (68)

are obtained from the eigenvalues (61) of the harmonic oscillator simply by

setting thefrequency ! equalto zero. Withtheprefactor ofthe propagatorof

thefree particle

K 0 exp  i ~ S cl;0  = r m 2 i~t (69)

and(65),thepropagatoroftheharmonicoscillatorb ecomes

K(x f ;t;x i ;0)= r m 2 i~t r D 0 D exp  i ~ S cl  : (70)

Forreadersunfamiliarwiththeconceptofdeterminantsofdi erentialop

era-torswementionthatwemayde nematrixelementsofanop eratorbyprojection

ontoabasisasisfamiliarfromstandardquantummechanics.Theop erator

rep-resented inits eigenbasis yields adiagonal matrix withthe eigenvalues onthe

diagonal.Then,asfor nitedimensionalmatrices,thedeterminantisthepro duct

oftheseeigenvalues.

Each of the determinants(66)and (67)by itself diverges. However,we are

interestedintheratiob etween themwhichiswell-de ned[12]

D D 0 = 1 Y 1  ! t  n  2 ! = sin(! t) ! t : (71)

(20)

Inserting this result into (70)leads to the propagator of the driven harmonic

oscillatorinits nalform

K(x f ;t;x i ;0)= r m! 2 i~sin(! t) exp  i ~ S cl  = r m! 2 ~jsin(! t)j exp  i ~ S cl i   4 +n  2   (72)

withtheclassicalactionde nedin(56).TheMorseindexninthephasefactoris

givenbytheintegerpartof! t= .Thisphaseaccountsforthechangesinsignof

thesinefunction[13].Here,onemightarguethatitisnotobviouswhichsignof

thesquarero otonehastotake.However,thesemigroupprop erty(9)allowsto

constructpropagatorsacrossconjugatep ointsbyjoiningpropagatorsforshorter

timeintervals.Inthisway,thesignmayb e determinedunambiguously[14].

Itisinterestingtonotethatthephasefactorexp( in =2)in(72)impliesthat

K(x f ;2 =! ;x i ;0)= K(x f ;0;x i ;0)= Æ(x f x i

),i.e. thewavefunctionafter

one p erio dof oscillationdi ers fromtheoriginalwave functionbyafactor 1.

Theoscillatorthusreturnstoitsoriginalstateonlyaftertwop erio dsverymuch

likeaspin-1/2 particlewhichpicksupasignunder rotationby2 andreturns

to its original state only after a4 -rotation. This e ect mightb e observed in

thecaseoftheharmonicoscillatorbylettinginterferethewavefunctionsoftwo

oscillatorswithdi erentfrequency [15].

2.8 SemiclassicalApproximation

The systems considered so far have b een sp ecial in the sense that an exact

expression for the propagatorcould b e obtained. This is a consequence of the

fact thatthep otentialwasat mostquadraticintheco ordinate.Unfortunately,

inmostcasesofinterestthep otentialismorecomplicatedandapartfromafew

exceptions an exact evaluationofthe pathintegral turnsoutto b e imp ossible.

Tocop ewithsuch situations,approximationschemeshaveb een devised.Inthe

following,wewillrestrictourselvestothemostimp ortantapproximationwhich

isvalidwhenever thequantum uctuationsaresmallor,equivalently,whenthe

actionsinvolvedarelargecomparedtoPlanck'sconstantsothatthelattermay

b econsidered tob esmall.

Thedecomp ositionofageneralpathintotheclassicalpathand uctuations

around it as employedin(48) in the previous section was merely a matter of

convenience. For the exactly solvable case of a driven harmonic oscillator it

is not really relevant how we express a general path satisfying the b oundary

conditions. Within the semiclassical approximation,however, it is decisive to

expandaroundthepathleadingtothedominantcontribution,i.e. theclassical

path. From a more mathematical p oint of view, we have to evaluate a path

integraloverexp(iS=~)forsmall~.Thiscanb edoneinasystematicwaybythe

(21)

x= p

Re exp(i x )

1 1

Fig.8. Instationary phase approximation only asmall region around theextremum

contributes totheintegral. Fortheexampleshownhere,theextremumlies atx=0

At this p oint it may b e useful to give a brief reminder of the metho d of

stationaryphase.Supp ose we wanttoevaluatetheintegral

I( )= Z 1 1 dxg (x)exp i f(x)  (73)

inthelimitofverylarge .Insp ectionofFig.8,wheref(x)=x

2

,suggeststhat

thedominantcontributionto theintegralcomes fromaregion,inourexample

of size 1=

p

, around the extremal (or stationary) p oint of the function f(x).

Outside ofthisregion,theintegrandisrapidlyoscillatingandthereforegivesto

leadingorderanegligiblecontribution.Sinceforlarge ,theregiondetermining

theintegral isvery small,wemayexpandthefunctionf(x) lo callyaroundthe

extremumx 0 f(x)f(x 0 )+ 1 2 f 00 (x 0 )(x x 0 ) 2 +::: (74) and replace g (x) by g (x 0

). Neglecting higher order terms, which is allowed if

f 00

(x 0

)isoforderone,weareleftwiththeGaussianintegral

I( )g (x 0 )exp i f(x 0 )  Z 1 1 dxexp  i 2 f 00 (x 0 )(x x 0 ) 2  = s 2 jf 00 (x 0 )j g (x 0 )exp h i f(x 0 )+i  4 sgn f 00 (x 0 )  i ; (75) where sgn(f 00 (x 0

))denotes thesignof f

00 (x

0

). Iff(x) p ossesses morethanone

extremum, one has to sum over the contributions of all extrema unless one

extremumcanb eshowntob edominant.

We nowapply the stationary phase approximationto pathintegrals where

1=~playstheroleofthelargeparameter.Sincetheactionisstationary at

clas-sicalpaths,weareobligedtoexpress thegeneralpathas

x(s)=x

cl

(s)+(s); (76)

where x

cl

(22)

Withthisdecomp ositiontheactionb ecomes S= Z t 0 ds  m 2 _ x 2 V(x)  = Z t 0 ds  m 2 _ x 2 cl V(x cl )  + Z t 0 ds  mx_ cl _  V 0 (x cl )  + Z t 0 ds  m 2 _  2 1 2 V 00 (x cl ) 2  +::: (77)

It isinstructive to comparethis result with theaction(50)for thedriven

har-monicoscillator.Again,the rsttermrepresentstheclassicalaction.Thesecond

term vanishes as was shown explicitly in (51) for the driven oscillator.In the

general case,one can convinceoneselfbypartialintegrationofthekineticpart

and comparisonwith the classical equation of motion that this term vanishes

again.Thisisofcourse aconsequence ofthefactthattheclassicalpath,around

whichweexpand,corresp onds toanextremumoftheaction.Thethirdtermon

the right-hand-side of(77)is theleadingorder terminthe uctuations as was

thecasein(50).Thereishoweveranimp ortantdi erence since foranharmonic

p otentialsthesecond derivative of thep otential V

00

is notconstantand

there-fore thecontribution ofthe uctuations dep ends on theclassicalpath.Finally,

ingeneraltherewillb ehigherordertermsinthe uctuationsasindicatedbythe

dotsin(77).Thesemiclassicalapproximationconsistsinneglectingthesehigher

ordertermssothat afterapartialintegration,we getfortheaction

S sc =S cl 1 2 Z t 0 ds  m d 2 ds 2 +V 00 (x cl )   (78)

where theindex`sc'indicates thesemiclassicalapproximation.

Before deriving the propagator insemiclassical approximation,we have to

discusstheregimeofvalidityofthisapproximation.Sincethe rsttermin(78)

givesonlyrisetoaglobalphasefactor,itisthesecondtermwhichdeterminesthe

magnitudeof thequantum uctuations.For thistermto contribute,we should

have 

2

=~.1sothat themagnitudeoftypical uctuations isat mostoforder

p

~ .Thetermofthirdorderinthe uctuationsisalreadysmallerthanthesecond

order term by afactor (

p ~ )

3

=~ =

p

~ . If Planck's constant can b e considered

tob e small,we mayindeed neglectthe uctuationcontributionsofhigherthan

secondorderexceptforoneexception:Itmayhapp enthatthesecondorderterm

do es notcontribute,ashasb eenthecase attheconjugatep ointsforthedriven

harmonic oscillator in Sect. 2.7. Then, the leading nonvanishing contribution

b ecomesdominant.Forthefollowingdiscussion, we willnotconsiderthislatter

case.

InanalogytoSect.2.7weobtainforthepropagatorinsemiclassical

approx-imation K(x f ;t;x i ;0)= r m r D 0 exp  i S cl  (79)

(23)

where D=det  d 2 ds 2 +V 00 (x cl )  (80) andD 0

isthe uctuationdeterminant(67)ofthefree particle.

Eventhoughitmayseemthatdeterminingtheprefactorisaformidabletask

since the uctuationdeterminantforagivenp otentialhastob eevaluated,this

taskcanb egreatlysimpli ed.Inaddition,thefollowingconsiderationso erthe

b ene tofprovidingaphysicalinterpretationoftheprefactor.Inourevaluation

of the prefactor we followMarinov [16]. The mainidea is to make use of the

semigroupprop erty (9)ofthepropagator

C(x f ;t;x i ;0)exp  i ~ S cl (x f ;t;x i ;0)  (81) = Z dx 0 C(x f ;t;x 0 ;t 0 )C(x 0 ;t 0 ;x i ;0)exp  i ~  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0)  

where the prefactor C dep ends on the uctuationcontribution. We now have

toevaluatethex

0

-integralwithinthesemiclassicalapproximation.Accordingto

thestationaryphaserequirementdiscussed ab ove,thedominantcontributionto

theintegralcomes fromx

0 =x 0 (x f ;x i ;t;t 0 )satisfying @S cl (x f ;t;x 0 ;t 0 ) @x 0 x 0 =x 0 + @S cl (x 0 ;t 0 ;x i ;0) @x 0 x 0 =x 0 =0: (82)

Accordingtoclassicalmechanicsthesederivativesarerelatedtoinitialand nal

momentumby[17]  @S cl @x i  xf;tf;ti = p i  @S cl @x f  xi;tf;ti =p f (83)

sothat (82)can expressed as

p(t 0 ")=p(t 0 +"): (84) The p oint x 0

thus has to b e chosen such that the two partial classical paths

can b e joinedwith acontinuousmomentum.Together they therefore yield the

completeclassicalpathand inparticular

S cl (x f ;t;x i ;0)=S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0): (85)

This relationensures that thephase factors dep endingon theclassicalactions

onb othsidesof(81)areequal.

Afterhavingidenti edthestationary path,we havetoevaluatetheintegral

overx

0

in(81).WithinsemiclassicalapproximationthisGaussianintegralleads

to C(x f ;t;x i ;0) C(x f ;t;x 0 ;t 0 )C(x 0 ;t 0 ;x i ;0) (86) =  1 2 i~ @ 2 @x 2  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0)   1=2 :

(24)

Inordertomakeprogress,itisusefultotakethederivativeof(85)withresp ect

tox

f

andx

i

.Keepinginmindthatx

0

dep ends onthese twovariablesone nds

@ 2 S cl (x f ;t;x i ;0) @x f @x i = @ 2 S cl (x f ;t;x 0 ;t 0 ) @x f @x 0 @x 0 @x i + @ 2 S cl (x 0 ;t 0 ;x i ;0) @x i @x 0 @x 0 @x f + @ 2 @x 2 0  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;t)  @x 0 @x i @x 0 @x f : (87)

Similarly,one ndsbytaking derivativesofthestationaryphase condition(82)

@x 0 @x f = @ 2 @x f x 0 S cl (x f ;t;x 0 ;t 0 ) @ 2 @x 2 0  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0)  (88) and @x 0 @x i = @ 2 @x i x 0 S cl (x 0 ;t 0 ;x i ;0) @ 2 @x 2 0  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0)  : (89)

These expressions allow to eliminate thepartialderivatives of x

0

with resp ect

tox

i

andx

f

app earingin(87)andone nallyobtains

 @ 2 @x 2 0  S cl (x f ;t;x 0 ;t 0 )+S cl (x 0 ;t 0 ;x i ;0)   1 (90) = @ 2 @x i @x f S cl (x f ;t;x i ;0) @ 2 S cl (x f ;t;x 0 ;t 0 ) @x f @x 0 @ 2 S cl (x 0 ;t 0 ;x i ;0) @x i @x 0 :

Inserting this result into (86), the prefactor can b e identi ed as the so-called

VanVleck-Pauli-Morettedeterminant[18,19,20]

C(x f ;t;x i ;0)=  1 2 i~  @ 2 S cl (x f ;t;x i ;0) @x f @x i  1=2 (91)

sothat thepropagatorinsemiclassicalapproximation nallyreads

K(x f ;t;x i ;0) (92) =  1 2 ~ @ 2 S cl (x f ;t;x i ;0) @x f @x i  1=2 exp  i ~ S cl (x f ;t;x i ;0) i   4 +n  2  

where the Morse index ndenotes the numb er of signchanges of @

2 S cl =@x f @x i

(25)

Aswe have alreadymentionedab ove,derivatives oftheactionwith resp ect

top ositionarerelatedtomomenta.Thisallowstogiveaphysicalinterpretation

oftheprefactorofthepropagatorasthechange oftheendp ointofthepathas

afunctionoftheinitialmomentum

 @ 2 S cl @x i @x f  1 = @x f @p i : (93)

A zero of this expression, or equivalently a divergence of the prefactor of the

propagator,indicatesaconjugatep ointwheretheendp ointdo esnotdep endon

theinitialmomentum.

Toclosethissection, we wantto comparethesemiclassicalresult (92)with

exact resultsforthefree particleandtheharmonicoscillator.Inourdiscussion

of the free particle inSect. 2.3we already mentionedthat thepropagatorcan

b eexpressedentirelyintermsofclassicalquantities.Indeed,theexpression(19)

forthepropagatorofthefree particleagreeswith(92).

For theharmonicoscillator,we knowfromSect.2.7 thattheprefactor do es

notdep endonap ossiblypresentexternalforce.Wemaytherefore considerthe

action(56)intheabsence ofdriving f(s)=0which thenreads

S cl = m! 2sin(! t)  x 2 i +x 2 f  cos (! t) 2x i x f  : (94)

Takingthederivativewithresp ect to x

i

andx

f

one ndsfortheprefactor

C(x f ;t;x i ;0)=  m! 2 i~sin(! t)  1=2 (95)

which is identical with theprefactor inour previous result (72). As exp ected,

forp otentialsat mostquadraticintheco ordinate thesemiclassicalpropagator

agreeswiththeexactexpression.

2.9 Imaginary TimePathIntegral

In the discussion of dissipative systems we will b e dealingwith a system

cou-pled toalargenumb erofenvironmentaldegrees offreedom.Inmostcases, the

environmentwillact like a largeheat bath characterized by atemp erature T.

Thestate of theenvironmentwilltherefore b e givenbyan equilibriumdensity

matrix.Occasionally,we mayalso b einterested intheequilibriumdensity

ma-trixofthesystemitself.Such astate mayb e reachedafter equilibrationdue to

weakcouplingwithaheatbath.

In order to describ e such thermal equilibrium states and the dynamics of

the system on a unique fo oting, it is desirable to express equilibriumdensity

matricesintermsofpathintegrals.Thisisindeedp ossibleasone recognizesby

writingtheequilibriumdensityop erator inp ositionrepresentation

 (x;x 0 )= 1 hxjexp( H)jx 0 i (96)

(26)

withthepartitionfunction

Z=

Z

dxhxjexp( H)jxi: (97)

Comparingwith thepropagatorinp ositionrepresentation

K(x;t;x 0 ;0)=hxjexp  i ~ Ht  jx 0 i (98)

one concludes that apart from the partition function the equilibrium density

matrixisequivalenttoapropagatorinimaginarytimet= i~ .

Afterthesubstitution =is theactioninimaginarytime i~ reads

Z i~ 0 ds " m 2  dx ds  2 V(x) # =i Z ~ 0 d " m 2  dx d  2 +V(x) # : (99)

Here and in the following, we use greek letters to indicate imaginary times.

Motivatedbytheright-handsideof(99)wede netheso-calledEuclideanaction

S E [x]= Z ~ 0 d h m 2 _ x 2 +V(x) i : (100)

Eventhoughonemightfearalackofintuitionformotioninimaginarytime,this

resultsshowsthatitcansimplyb ethoughtofasmotionintheinvertedp otential

in real time.Withthe Euclidean action (100) we now obtainas animp ortant

result the path integral expression for the (unnormalized) equilibriumdensity

matrix hxjexp( H)jx 0 i= Z  x(~ )=x  x(0)=x 0 Dxexp  1 ~ S E [x]  : (101)

Thiskindoffunctionalintegralwasdiscussed asearlyas1923byWiener[21]in

thecontextofclassicalBrownianmotion.

Asanexamplewe consider the(undriven)harmonicoscillator.There is

ac-tuallynoneedtoevaluateapathintegralsince we knowalreadyfromSect. 2.7

thepropagator K(x f ;t;x i ;0)= r m! 2 i~sin(! t) exp  i m! 2~ (x 2 i +x 2 f )cos (! t) 2x i x f sin(! t)  : (102)

Transforming the propagatorinto imaginary timet ! i~ and renaming x

i

andx

f

intox

0

andx,resp ectively,oneobtainstheequilibriumdensitymatrix

 (x;x 0 ) (103) = 1 Z r m! 2 ~sinh (~ ! ) exp  m! 2~ (x 2 +x 02 )cosh (~ ! ) 2xx 0 sinh(~ ! )  :

Thepartitionfunctionisobtainedbyp erformingthetraceas

Z=

Z

dxhxjexp( H)jxi=

1

(27)

whichagreeswiththeexpression Z= 1 X n=0 exp  ~!  n+ 1 2  (105)

based ontheenergy levelsoftheharmonicoscillator.

Sincethepartitionfunctionoftenservesasastartingp ointforthecalculation

ofthermo dynamicprop erties,itisinstructive totakeacloserathowthis

quan-titymay b e obtainedwithinthe path integral formalism.Ap ossible approach

isthe onewe just havesketched. By meansofanimaginarytimepathintegral

one rstcalculateshxjexp( H)jxiwhichis prop ortionaltotheprobabilityto

ndthesystematp ositionx.Subsequentintegrationoverco ordinatespacethen

yieldsthepartitionfunction.

However,thepartitionfunctionmayalsob edeterminedinonestep.Tothis

end, weexpand aroundthep erio dic trajectory withextremal Euclideanaction

which in our case is given by x( ) = 0. Any deviation will increase b oth the

kinetic and p otentialenergy and thus increase the Euclidean action.All other

trajectories contributing to the partition function are generated by a Fourier

seriesontheimaginarytimeintervalfrom0to~

x( )= 1 p ~ " a 0 + p 2 1 X n=1 a n cos ( n  )+b n sin( n  )  # (106)

where wehaveintro duced theso-calledMatsubarafrequencies

 n = 2 ~ n: (107)

This ansatz should b e compared with (62) for the uctuations where a

0 was

xedb ecausethe uctuationshadtovanishattheb oundaries.Forthepartition

functionthisrequirementisdropp ed sincewehavetointegrateoverallp erio dic

trajectories. Furthermore, we note that indeed with the ansatz (106) only the

p erio dictrajectoriescontribute.Allotherpathscostanin niteamountofaction

dueto thejumpattheb oundaryas we willseeshortly.

Insertingthe Fourier expansion (106) into the Euclideanaction of the

har-monicoscillator S E = Z ~ 0 d m 2 _ x 2 +! 2 x 2  (108) we nd S E = m 2 " ! 2 a 2 0 + 1 X n=1 ( 2 n +! 2 )(a 2 n +b 2 n ) # : (109)

AsinSect.2.7wedonotwanttogointothemathematicaldetailsofintegration

measuresandJacobideterminants.Unfortunately,thefreeparticlecannotserve

as a reference here b ecause itspartition function do es not exist.We therefore

contentourselves withremarkingthatb ecauseof

1 ! 1 Y 1  2 n +! 2 = ~ P 1 n=1  2 n 1 2sinh(~ ! =2) (110)

(28)

theresult oftheGaussian integralovertheFourierco eÆcientsyieldsthe

parti-tionfunctionuptoafrequencyindep endentfactor.Thisenablesustodetermine

thepartitionfunctioninmorecomplicatedcasesbypro ceedingasab oveand

us-ingthepartitionfunctionharmonicoscillatoras areference.

Returningtothedensitymatrixoftheharmonicoscillatorwe nallyobtain

byinsertingthepartitionfunction(104)intotheexpression(103)forthedensity

matrix  (x;x 0 )= s m!  ~ cosh (~ ! ) 1 sinh(~ ! ) (111) exp  m! 2~ (x 2 +x 02 )cosh (~ ! ) 2xx 0 sinh (~ ! )  :

Without path integrals, this result would require the evaluationof sums over

Hermitep olynomials.

Theexpression forthe density matrix(111) can b e veri edinthe limitsof

highandzero temp erature.Intheclassicallimitofveryhightemp eratures,the

probabilitydistributioninrealspaceis givenby

P(x)= (x;x)= r m! 2 2 exp  m! 2 2 x 2  exp [ V(x)]: (112)

We thus have obtainedtheBoltzmanndistributionwhich dep ends only onthe

p otentialenergy.Thefactthatthekineticenergydo esnotplayarolecaneasily

b eundersto o dintermsofthepathintegralformalism.Excursionsinaveryshort

time~ costto omuchactionandaretherefore stronglysuppressed.

Intheopp osite limitof zero temp eraturethe density matrixfactorizes into

apro ductofgroundstate wavefunctions oftheharmonicoscillator

lim !1  (x;x 0 )=   m!  ~  1=4 exp  m! 2~ x 2    m!  ~  1=4 exp  m! 2~ x 02   (113)

asshould b eexp ected.

3 Dissipative Systems

3.1 Intro duction

Inclassicalmechanicsdissipationcanoftenb eadequatelydescrib ed byincluding

a velo city dep endent damping term into the equation of motion. Such a

phe-nomenologicalapproach isnolonger p ossibleinquantummechanicswhere the

Hamiltonformalismimpliesenergy conservation fortime-indep endent

Hamilto-nians. Then, a b etter understanding of the situation is necessary in order to

arriveat anappropriatephysicalmo del.

Adamp edp endulummayhelpus tounderstand themechanismof

(29)

under-molecules in the air surrounding the p endulum's mass. We may consider the

p endulum and the air molecules as one large system which,if assumed to b e

isolatedfromfurtherdegreesoffreedom,ob eysenergyconservation.Theenergy

of the p endulum alone,however, willingeneral not b e conserved. This single

degreeoffreedomisthereforesubject todissipationarisingfromthecouplingto

otherdegrees offreedom.

Thisinsightwillallowusinthefollowingsectiontointro duceamo delfor a

systemcoupledtoan environmentandto demonstrateexplicitlyits dissipative

nature. In particular,we willintro duce thequantities needed foradescription

which fo cuses on the system degree of freedom. We are then ina p osition to

return to the path integral formalismand to demonstrate how it mayb e

em-ployed to study dissipative systems. Starting from the mo del of system and

environment,the latter willb e eliminatedto obtain areduced description for

thesystemalone.Thisleaves uswith ane ective actionwhichformsthebasis

ofthepathintegraldescription ofdissipation.

3.2 EnvironmentasCollectionofHarmonic Oscillators

A suitablemo delfordissipative quantumsystems should b othincorp orate the

idea of a coupling b etween system and environment and b e amenable to an

analytic treatment ofthe environmentalcoupling. These requirementsare met

byamo delwhichnowadaysisoftenreferredtoasCaldeira-Leggettmo del[22,23]

eventhoughithasb eendiscussedintheliteratureundervariousnamesb eforefor

harmonicsystems[24,25,26,27]andanharmonicsystems [28].TheHamiltonian

H=H S +H B +H SB (114)

consistsofthreecontributions.TheHamiltonianofthesystemdegreeoffreedom

H S = p 2 2m +V(q ) (115)

mo dels a particle of mass m moving in a p otential V. Here, we denote the

co ordinate byq tofacilitatethedistinctionfromtheenvironmentalco ordinates

x n

whichwewillintro duceinamoment.Ofcourse,thesystemdegreeoffreedom

do esnothavetob easso ciatedwitharealparticlebutmayb equiteabstract.In

fact,asubstantialpartofthecalculationstob e discussed inthefollowingdo es

notdep endonthedetailedformofthesystemHamiltonian.

TheHamiltonianoftheenvironmentaldegreesoffreedom

H B = N X n=1  p 2 n 2m n + m n 2 ! 2 n x 2 n  (116)

describ es acollectionof harmonicoscillators.While theprop ertiesof the

envi-ronmentmayinsomecasesb e chosen onthebasisofamicroscopicmo del,this

(30)

linear electric element should b e welldescrib ed by aHamiltonianof the form

(116).Ontheotherhand,theunderlyingmechanismleadingtodissipation,e.g.

inaresistor, mayb emuchmorecomplicatedthanthatimpliedbythemo delof

acollectionofharmonicoscillators.

Thecouplingde nedbytheHamiltonian

H SB = q N X n=1 c n x n +q 2 N X n=1 c 2 n 2m n ! 2 n (117)

isbilinearinthep ositionop eratorsofsystemandenvironment.Therearecases

where the bilinear couplingis realistic, e.g.for an environment consisting of a

linear electric circuit like the resistor just mentionedor fora dip olar coupling

to electromagnetic eld mo des encountered in quantumoptics. Withinamore

general scop e, this Hamiltonian mayb e viewed as linearization of anonlinear

couplinginthelimitofweakcouplingtotheenvironmentaldegrees offreedom.

Aswas rstp ointedoutbyCaldeiraandLeggett,anin nitenumb erofdegrees

of freedomstill allowsforstrongdampingevenifeach environmentaloscillator

couples onlyweaklytothesystem[22,23].

Anenvironmentconsistingofharmonicoscillatorsasin(116)mightb e

criti-cized.Ifthep otentialV(q )isharmonic,onemaypasstonormalco ordinatesand

thus demonstratethat after some timea revival of theinitialstate willo ccur.

ForsuÆcientlymanyenvironmentaloscillators,however,thisso-calledPoincare

recurrence timetendstoin nity[29].Therefore,evenwithalinearenvironment

irreversibilityb ecomesp ossibleat leastforallpracticalpurp oses.

Thereader mayhavenoticedthatinthecouplingHamiltonian(117)aterm

is present which only contains anop erator actingin the systemHilb ert space

butdep ends onthecouplingconstantsc

n

.Thephysicalreason fortheinclusion

of this term liesina p otential renormalizationintro duced by the rst termin

(117).Thisb ecomesclearifweconsider theminimumoftheHamiltonianwith

resp ect tothesystemandenvironmentco ordinates.Fromtherequirement

@H @x n =m n ! 2 n x n c n q ! =0 (118) weobtain x n = c n m n ! 2 n q: (119)

Usingthisresult todeterminetheminimumoftheHamiltonianwithresp ect to

thesystemco ordinatewe nd

@H @q = @V @q N X n=1 c n x n +q N X n=1 c 2 n m n ! 2 n = @V @q : (120)

Thesecondtermin(117)thusensuresthat thisminimumis determinedbythe

barep otentialV(q ).

(31)

de-eliminationofthe environmentaldegrees of freedomleads indeed to adamp ed

equationofmotionforthesystemco ordinate.Wep erformtheeliminationwithin

theHeisenb erg picture wheretheevolutionofanop eratorA isdeterminedby

dA dt = i ~ [H ;A]: (121)

FromtheHamiltonian(114)weobtaintheequationsofmotionforthe

environ-mentaldegreesoffreedom

_ p n = m n ! 2 n x n +c n q _ x n = p n m n (122)

andthesystemdegree offreedom

_ p= @V @q + N X n=1 c n x n q N X n=1 c 2 n m n ! 2 n _ x= p m : (123)

Thetrick for solving theenvironmentalequations of motion (122) consists

intreatingthesystemco ordinateq (t)asifitwereagivenfunctionoftime.The

inhomogeneousdi erentialequationthenhasthesolution

x n (t)=x n (0)cos (! n t)+ p n (0) m n ! n sin(! n t)+ c n m n ! n Z t 0 dssin ! n (t s)  q (s): (124)

Insertingthisresult into(123) one ndsane ective equationofmotionforthe

systemco ordinate mq Z t 0 ds N X n=1 c 2 n m n ! n sin ! n (t s)  q (s)+ @V @q +q N X n=1 c 2 n m n ! 2 n (125) = N X n=1 c n  x n (0)cos(! n t)+ p n (0) m n ! n sin(! n t)  :

By apartialintegrationof thesecond termonthe left-handsidethis equation

ofmotioncanb e castintoits nalform

mq+m Z t 0 ds (t s)q (s)_ + @V @q =(t) (126)

withthedampingkernel

(t)= 1 m N X c 2 n m n ! 2 n cos (! n t) (127)

(32)

andtheop erator-valued uctuatingforce (t)= N X n=1 c n  x n (0) c n m n ! 2 n q (0)  cos (! n t)+ p n (0) m n ! n sin(! n t)  : (128)

The uctuatingforce vanishes if averagedover athermaldensity matrixof

theenvironmentincludingthecouplingtothesystem

h(t)i B+SB = Tr B  (t)exp (H B +H SB )  Tr B  exp (H B +H SB )  =0: (129)

Forweakcoupling,onemaywanttosplito thetransienttermm (t)q (0)which

isofsecond orderinthecouplingand writethe uctuatingforceas [30]

(t)=(t) m (t)q (0): (130)

Thesode ned force(t) vanishesifaveragedovertheenvironmentalone

h(t)i B = Tr B  (t)exp ( H B )  Tr B  exp( H B )  =0: (131)

An imp ortantquantity to characterize the uctuating force is the

correla-tionfunctionwhich againcan b e evaluated for  with resp ect to H

B

+H

SB or

equivalentlyfor  with resp ect to H

B

alone.With (128) and (130) we get the

correlationfunction h(t)(0)i B = X n;l c n c l  x n (0)cos (! n t)+ p n (0) m n ! i sin(! n t)  x l (0)  B : (132)

Inthermalequilibriumthesecondmomentsaregivenby

hx n (0)x l (0)i B =Æ nl ~ 2m n ! n coth  ~ ! n 2  (133) hp n (0)x l (0)i B = i~ 2 Æ nl ; (134)

sothat thenoisecorrelationfunction nallyb ecomes

h(t)(0)i B = N X n=1 ~c 2 n 2m n ! n  coth  ~ ! n 2  cos (! n t) isin(! n t)  : (135)

Theimaginarypartapp earinghereisaconsequenceofthefactthattheop erators

(t)and(0)ingeneraldonotcommute.Thecorrelationfunction(135)app ears

(33)

It is remarkable that within areduced description for the systemalone all

quantitiescharacterizingtheenvironmentmayb eexpressedintermsofthesp

ec-traldensityofbathoscillators

J(! )= N X n=1 c 2 n 2m n ! n Æ(! ! n ): (136)

As anexample,thedampingkernel mayb e expressed intermsofthis sp ectral

densityas (t)= 1 m N X n=1 c 2 n m n ! 2 n cos (! n t)= 2 m Z 1 0 d!  J(! ) ! cos(! t): (137)

For practicalcalculations, itis therefore unnecessary to sp ecify allparameters

m n ;! n and c n

app earing in (116) and (117). It rather suÆces to de ne the

sp ectraldensityJ(! ).

Themostfrequently usedsp ectraldensity

J(! )=m ! (138)

is asso ciated with the so-called Ohmicdamping. This term is sometimes

em-ployedto indicate aprop ortionalityto frequency merely at lowfrequencies

in-stead of over the whole frequency range. In fact,in any realistic situationthe

sp ectral density willnot increase like in (138) for arbitrarily high frequencies.

It is justi ed to use the term \Ohmic damping"even if (138) holds only b

e-lowacertainfrequency providedthisfrequency ismuchhigherthanthetypical

frequencies app earinginthesystemdynamics.

From(137)one ndsthedampingkernelforOhmicdamping

(t)=2 Æ(t); (139)

which renders (126) memory-free. We thus recover the velo city prop ortional

dampingtermfamiliarfromclassicaldamp ed systems.Itshould b e notedthat

thefactoroftwoin(139)disapp earsup onintegrationin(126)since(137)implies

thatthedelta functionissymmetricaroundzero.

At this p oint, we want to brie y elucidate the originof the term \Ohmic

damping".Let us consider the electric circuit shown in Fig. 9 consisting of a

resistance R, acapacitance C and aninductance L. Summingupthe voltages

around the lo op, one obtains as equation of motion for the charge Q on the

capacitor L  Q+R _ Q+ Q C =0; (140)

whichshowsthatanOhmicresistorleadsindeedtomemorylessdamping.These

considerationsdemonstratethatevenwithoutknowledgeofthemicroscopic

(34)

R

L C

Fig.9. LC oscillatorwithOhmicdamping duetoaresistorR

Thesp ectraldensity(138)forOhmicdampingunfortunatelydivergesathigh

frequencies which,as alreadymentioned,cannot b e the case in practice. Even

in theoretical considerations this feature of strictly Ohmic damping maylead

to divergencies and acuto isneeded for regularization.One p ossibilityis the

Drude cuto ,wherethesp ectraldensity

J(! )=m ! ! 2 D ! 2 +! 2 D (141)

ab ovefrequencies oftheorderof !

D

issuppressed. Thecorresp onding damping

kernelreads (t)= ! D exp( ! D jtj): (142)

Thisleadstomemorye ectsin(126)forshorttimest<!

1 D

.Forthelong-time

b ehaviour, however, only the Ohmic low frequency b ehaviour of the sp ectral

density(141)isrelevant.IfaDrudecuto isintro ducedfortechnicalreasons,the

cuto frequency !

D

shouldb emuchlarger thanallotherfrequencies app earing

intheprobleminordertoavoidspuriouse ects.

Therelation (136) b etween thesp ectral density and the \microscopic"

pa-rameters impliesthat one mayset c

n =m n ! 2 n

withoutloss of generalitysince

the frequencies !

n

and the oscillator strengths c

2 n =2m n ! n

can still b e freely

chosen. This sp ecial choice for the coupling constants has the advantage of a

translationallyinvariantcoupling[31]

H=H S + N X n=1  p 2 n 2m n + m n 2 ! 2 n (x n q ) 2  : (143)

Furthermore,we nowcandeterminethetotalmassofenvironmentaloscillators

N X n=1 m n = 2  Z 1 0 d! J(! ) ! 3 : (144)

If the sp ectral density of bath oscillators at small frequencies takes the form

J(! )!

, thetotalmassofbathoscillatorsisin nitefor 2.Inparticular,

(35)

theparticlewillb ehave forlongtimeslikeitwerefreealb eitp ossessinga

renor-malized mass due to the environmental coupling [32]. We emphasizethat the

divergence of the total mass for  2 is due to an infrared divergence and

therefore indep endent ofahigh-frequencycuto .

Itisalsousefultoexpressthep otentialrenormalizationintro ducedin(117)in

termsofthesp ectraldensityofbathoscillators.From(136)itisstraightforward

toobtain q 2 N X n=1 c 2 n 2m n ! 2 n = q 2  Z 1 0 d! J(! ) ! : (145)

Thistermisin niteforstrictlyOhmicdampingbutb ecomes nitewhena

high-frequency cuto isintro duced.

Finally,one ndsforthenoise correlationfunction(132)

K(t)=h(t)(0)i B =~ Z 1 0 d!  J(! )  coth  ~ ! 2  cos (! t) isin(! t)  : (146)

Intheclassicallimit,~!0,thiscorrelationfunctionreducestothereal-valued

expression

K(t)=mk

B

T (t); (147)

where we havemadeuseof (137).For Ohmicdampingthisimpliesdelta

corre-lated,i.e.white,noise.

Inthe quantum case, thenoise correlationfunction is complexand can b e

decomp osed intoitsrealandimaginarypart

K(t)=K

0

(t)+iK

00

(t): (148)

Employingonce more(137),one immediately ndsthat theimaginary part is

relatedtothetimederivative ofthedampingkernel by

K 00 (t)= m~ 2 d dt : (149)

ForOhmicdamping,therealpart reads

K 0 (t)=  m (~ ) 2 1 sinh 2   t ~  (150)

whichimpliesthatatzerotemp eraturethenoiseiscorrelatedevenforlongtimes.

Thenoise correlation thenonlydecaysalgebraicallylike1=t

2

muchincontrast

totheclassicalresult (147).

3.3 E ective Action

(36)

alone.Thissectionwillb edevotedtoadiscussionofthecorresp ondingpro cedure

withinthepathintegral formalism.

Westarttoillustratethebasicideabyconsideringthetimeevolutionofthe

fulldensitymatrixof systemandenvironment

W(q f ;x nf ;q 0 f ;x 0 nf ;t)= Z dq i dq 0 i dx ni dx 0 ni K(q f ;x nf ;t;q i ;x ni ;0) (151) W(q i ;x ni ;q 0 i ;x 0 ni ;0)K  (q 0 f ;x 0 nf ;t;q 0 i ;x 0 ni ;0)

which is induced by the two propagators K. Here, the co ordinates q and x

n

refer againto the systemand bath degrees of freedom,resp ectively. The

envi-ronmentisassumedtob einthermalequilibriumdescrib edbythedensitymatrix

W B

while thesystemmayb e ina nonequilibriumstate .If we neglect initial

correlationsb etween systemand environment,i.e. ifwe switch onthecoupling

after preparationof theinitialstate,theinitialdensity matrixmayb e written

infactorizedform W(q i ;x ni ;q 0 i ;x 0 ni ;0)=(q i ;q 0 i )W B (x ni ;x 0 ni ): (152)

Sinceweareonlyinterestedinthedynamicsofthesystemdegreeoffreedom,

wetrace outtheenvironment.Thenthetimeevolutionmayb eexpressed as

(q f ;q 0 f ;t)= Z dq i dq 0 i J(q f ;q 0 f ;t;q i ;q 0 i ;0)(q i ;q 0 i ) (153)

withthepropagatingfunction

J(q f ;q 0 f ;t;q i ;q 0 i ;0)= Z dx nf dx ni dx 0 ni K(q f ;x nf ;t;q i ;x ni ;0) (154) W B (x ni ;x 0 ni )K  (q 0 f ;x nf ;t;q 0 i ;x 0 ni ;0):

Here, thetrace has b een p erformedbysetting x

nf

=x

0 nf

and integrating over

theseco ordinates.Thepropagatorsmayb eexpressedasrealtimepathintegrals

while theequilibriumdensity matrixof thebathis given by apathintegralin

imaginary time. Performing the path integrals and the conventional integrals

app earing in(154) one nds a functionaldep ending on the system path. The

imp ortantp ointisthat thisfunctionalcontainsallinformationab outthe

envi-ronmentrequiredtodeterminethesystemdynamics.

Forfactorizinginitialconditions,thepropagatingfunctionJ hasb een

calcu-latedbyFeynmanand Vernon[33]onthebasisoftheHamiltonian(114).More

general initialconditionstaking into account correlations b etween system and

environmentmayb e consideredaswell[34].

Instead of deriving the propagating function we will demonstrate how to

tracetheenvironmentoutoftheequilibriumdensitymatrixofsystemplus

(37)

We start from the imaginary time path integral representation of the full

equilibriumdensitymatrix

W (q ;x n ;q 0 ;x 0 n )= 1 Z Z Dq N Y n=1 Dx n ! exp  1 ~ S E [q ;x n ]  (155)

where thepathsrunfromq (0) =q

0 and x n (0)=x 0 n toq (~ ) =qand x n (~ )= x n

. TheEuclideanactioncorresp onding to themo delHamiltonian(114) reads

inimaginarytime S E [q;x n ]=S E S [q ]+S E B [x n ]+S E SB [q;x n ] (156) with S E S [q ]= Z ~ 0 d  m 2 _  q 2 +V(q )  (157) S E B [x n ]= Z ~ 0 d N X n=1 m n 2 _  x 2 n +! 2 n  x 2 n  (158) S E SB [q ;x n ]= Z ~ 0 d q N X n=1 c n  x n +q 2 N X n=1 c 2 n 2m n ! 2 n ! : (159)

The reduced density matrix of the system is obtained by tracing over the

environmentaldegreesoffreedom

 (q ;q 0 )=Tr B W (q ;x n ;q 0 ;x 0 n )  = 1 Z Z Dq Z N Y n=1 dx n I N Y n=1 Dx n exp  1 ~ S E [q ;x n ]  (160)

wherethecircleonthesecondfunctionalintegralsignindicatesthat onehasto

integrate over closed paths x

n

(0) = x

n

(~ ) =x

n

when p erformingthe trace.

Thedep endenceontheenvironmentalcouplingmayb emadeexplicitbywriting

 (q ;q 0 )= 1 Z Z Dqexp  1 ~ S E S [q]  F[q ] (161)

where the in uence functionalF[q ] describ es the in uence of the environment

onthesystem.Here, the partitionfunctionZ should notb econfused withthe

partitionfunctionZ

ofsystemplusenvironment.Therelationb etweenthetwo

quantitieswillb ediscussed shortly.

Since the bath oscillators are not coupledamong each other, thein uence

functionalmayb edecomp osedintofactorscorresp ondingtotheindividualbath

oscillators F[q]= N Y 1 Z n F n [q] (162)

(38)

where Z n = 1 2sinh(~ ! n =2) (163)

isthepartitionfunctionofasinglebathoscillator.Thein uencefunctionalofa

bathoscillatorcanb e expressed as

F n [q]= Z dx n I Dx n exp  1 ~ S E n [q ;x n ]  (164)

withtheaction

S E n [q ;x n ]= Z ~ 0 d m n 2 " _  x 2 n +! 2 n   x n c n m n ! 2 n  q  2 # : (165)

The partitionfunctionZ of the damp edsystemis relatedto the fullpartition

function Z

by the partition function of the environmental oscillators Z

B = Q N n=1 Z n according to Z =Z =Z B

. Inthelimitofvanishingcoupling, c

n

=0,

the in uence functional b ecomes F[q] = 1 so that (161) reduces to the path

integralrepresentationofthedensitymatrixofanisolatedsystemas itshould.

Apartfromthep otentialrenormalizationtermprop ortionaltoq

2

,theaction

(165)describ es adrivenharmonicoscillator.Wemaythereforemake useofour

results fromSect.2.7.Afteranalyticcontinuationt! i~ in(56)andsetting

x i =x f =x n

one ndsfortheclassicalEuclideanaction

S E;cl n [q]=m n ! n cosh (~ ! n ) 1 sinh(~ ! n ) x 2 n c n Z ~ 0 d sinh(! n )+sinh(! n (~ )) sinh(~ ! n ) x n  q () c 2 n m n ! n Z ~ 0 d Z  0 d sinh (! n (~ ))sinh(! n  ) sinh(~ ! n )  q ()q ( ) + c 2 n 2m n ! 2 n Z ~ 0 dq 2 (): (166)

Inviewoftherequired integrationover x

n

one completesthesquare

S E;cl n [q]=m n ! n cosh (~ ! n ) 1 sinh(~ ! n ) (x n x (0) n ) 2 Z ~ 0 d Z  0 d K n (  )q ()q ( ) + c 2 n 2m n ! 2 n Z ~ 0 dq 2 () (167) where x (0) n

do es notneedtob e sp eci edsinceit dropsoutafterintegration.

Theintegral kernel app earingin(167)followsfrom(166)as

K n ()= c 2 n 2m n ! n cosh  ! n ~ 2    sinh  ~ ! n  =K n (~ ) (168)

References

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