in order to
[观察]
1. He got up very early in order to / so as to catch the first bus.
2. In order to catch the first bus, he got up very early.
3. He works very hard in order to / so as to support his family.
4. Turn the volume down in order not to / so as not to wake the child.
[归纳] in order to 意为 “为了……”,表示目的;在用法和意义上相当于so as to结构,但是in order to结构可以用于句首、句中,而so as to多用于句中。其否定式分别为:in order not to 和so as not to。
[拓展] in order to和so as to在句中表示目的时,常可以转化成in order that或so that引导的目的状语从句。如:
We should work hard in order to / so as to pass the exam.
→ We should work hard in order that / so that we can pass the exam.
为了能通过考试,我们应该努力学习。
[小试] 翻译下面的句子。
1. He went there early so as to / in order to get a good seat.
He went there early so that / in order that he could get a good seat.
2. In order not to wake the baby we went in quietly.
Key:
1. 他去得早,以便找到个好座位。
2. 为了不惊醒小孩,我们轻轻地走了进去。
第二篇:Threshold resummation to any order in (1-x)
PreprinttypesetinJHEPstyle-PAPERVERSION
arXiv:0710.5693v3 [hep-ph] 13 Nov 2007GeorgesGrunberg?CentredePhysiqueTh?eorique,EcolePolytechnique,CNRS,91128PalaiseauCedex,FranceE-mail:georges.grunberg@pascal.cpht.polytechnique.frAbstract:Asimpleansatzissuggestedforthestructureofthresholdresummationofthemomentumspacephysicalevolutionkernels(‘physicalanomalousdimensions’)atallordersin(1?x),takingasexamplesDeepInelasticScatteringandtheDrell-Yanprocess.Eachtermintheexpansionisassociatedtoadistinctrenormalizationgroupandschemeinvariantperturbativeobject(‘physicalSudakovanomalousdimension’)dependingonasinglemomentumscalevariable.Bothlogarithmicallyenhancedtermsandconstanttermsarecapturedbytheansatzatanyorderintheexpansion.Theansatzismotivatedbyalarge–β0dispersivecalculation.Adispersiverepresentationat?niteβ0ofthephysicalSudakovanomalousdimensionsisalsoobtained,associatedtoasetof‘Sudakove?ectivecharges’whichencapsulatethenon-Abeliannatureoftheinteraction.Itisfoundthatthedispersiverepresentationrequiresanon-trivial,andprocess-dependent,choiceofvariablesinthe(x,Q2)plane.SomeinterestingpropertiesofthephysicalSudakovanomalousdimen-sionsarepointedout.Theensuing1/Nexpansioninmomentspaceisstraightforwardly
derivedfromthemomentumspaceexpansion.Keywords:resummation,renormalons.
1.Introduction
Thresholdresummation,namelytheresummationtoallordersofperturbationtheoryofthelargelogarithmiccorrectionswhicharisefromtheincompletecancellationofsoftandcollineargluonsattheedgeofphasespace,isbynowawelldevelopedtopic[1,2]inperturbativeQCD.Abouttenyearsago,thesubjectwasextended[3–5]tocoveralsotheresummationoflogarithmicallyenhancedtermswhicharesuppressedbysomepowerof(1?x)forx→1inmomentumspace(orbysomepowerof1/N,N→∞inmomentspace),concentratingonthecaseofthelongitudinalstructurefunctionFL(x,Q2)inDeepInelasticScattering(DIS)wherethesecorrectionsareactuallytheleadingterms.AsfarasIamaware,littleworkhasbeenperformedonthissubjectsincethen.Inthispaper,buildingupontherecentwork[6],Iprovideaverysimpleansatzforthestructureofthresholdresummationatallordersin(1?x),workingatthelevelofthemomentumspacephysicalevolutionkernels(or‘physicalanomalousdimensions’,seee.g.[7–10]),whichareinfraredandcollinearsafequantitiesdescribingthephysicalscalingviolation,where
–1–
thestructureoftheansatzappearstobeparticularlytransparent.Ishalldealexplicitlywiththeexamplesofthe(non-singlet)DeepInelasticScattering(DIS)structurefunctionF2(x,Q2),aswellaswiththeDrell-Yanprocess.Theansatzismotivatedbyalarge–β0dispersivecalculation,and,following[6,11–15],easilygeneralizesitselftoageneral?nite–β0dispersiverepresentationofthephysicalevolutionkernelatanyorderinthex→1expansion.
Thepaperisorganizedasfollows:section2isdevotedtoDIS.Insection2.1,themomentumspaceansatzforthresholdresummationforthenon-singletstructurefunctionF2(x,Q2)isdisplayed,whichintroducesateachorderofthex→1expansionanew‘jetphysicalanomalousdimension’.Theansatzisjusti?edinsection2.2byalarge–β0calculation,whichalsoprovidesadispersiverepresentationforeachofthepreviousphysicalanomalousdimensions.Thesedispersiverepresentationsarethenextendedto?nite–β0insection2.3,whereasetof‘jetSudakove?ectivecharges’whichencapsulatethenon-Abeliannatureoftheinteractionisintroduced.TheDrell-Yancaseisaddressedinsection3inquiteasimilarway.Theansatzfortheanalogousτ→1expansionisgiveninsection3.1,andjusti?edinsection3.2byalarge–β0calculation,whichyieldsthedispersiverepresentationofthecorresponding‘softphysicalanomalousdimensions’speci?ctotheDrell-Yanprocess.Theserepresentationsarethenextendedto?nite–β0insection3.3,whereasetof‘softSudakove?ectivecharges’isintroduced.BothintheDISandintheDrell-Yancase,anon-trivial(process-dependent)choiceofexpansionparameterinthe(x,Q2)(resp.(τ,Q2))planehastobemadeinordertoderivethedispersiverepresentations.TheconclusionsaregiveninSection4.The1/NexpansioninmomentspaceisderivedinastraighforwardwayfromthecorrespondingmomentumspaceexpansionansatzinAppendixA(DIS)andB(Drell-Yan).Thesetwolastappendicesalsoclarifytheconnectionbetweenthede?nitionsofthe‘jet’(DIS)(orthe‘soft’(DY))scalesinmomentumandmomentspacesrespectively.
2.DeepInelasticScatteringcase
2.1Asystematicexpansionforx→1
Thescale–dependenceofthe(?avournon-singlet)deepinelasticstructurefunctionF2canbeexpressedintermsofF2itself,yieldingthefollowingevolutionequation(seee.g.Refs.[7,9,10]):
dF2(x,Q2)K(x/z,Q2)F2(z,Q2).(2.1)z
K(x,Q2)isthemomentumspacephysicalevolutionkernel,orphysicalanomalousdimen-sion;itisrenormalization–groupinvariant.In[6],usingknownresultsofSudakovresum-mationinmomentspace,theresultfortheleadingcontributiontothisquantityinthex→1limitwasderived.Forcompletness,Ireproducethisshortderivationhere.
De?ningmomentsby
?2(N,Q)=F2?1
0dxxN?1F2(x,Q2),(2.2)
–2–
Eq.(2.1)impliesthatthemoment–spacephysicalevolutionkernelis:
?1?2(N,Q2)dlnFN?122?dxxK(x,Q)=K(N,Q)≡
dlnQ2=?1
dx
0xN?1?1
dln?2(2.5)
whereA(αs)isthe‘cusp’anomalousdimension,andB(αs)thestandard‘jet’Sudakovanomalousdimension1.Moreover,theconstanttermcanbewritten[14]intermsofthequarkelectromagneticformfactorF(Q2)[18–21]:
??2)2dlnF(Q2J(?)H(αs(Q2))=(2.6)?2????=G1,αs(Q2),ε=0+Bαs(Q2),
whereeachofthetwotermsinthe?rstlineisseparatelyinfrareddivergent,butthedivergencecancels[14]inthesum;inthesecondlinetheresultisexpressedintermsof?22???222B(αs)andGQ/?,αs(?),ε,whichisthe?nitepartofdlnF(Q)/dlnQ2asde?nedinRef.[21]usingdimensionalregularization.
Comparing(2.3)and(2.4)onetherefore?ndsthefollowingrelation[6]inmomentumspace:
??2??J(1?x)Q0δ(1?x)+O(1?x)K(x,Q2)=dlnQ2
=???2J(1?x)Q
dlnQ2+
???Q2d?20
1?x
1?=+?10??dxF(x)?F(1)???J(1?x)Q2AandBareseparatelyschemedependentquantities.
–3–
whereF(x)isasmoothtestfunction.Thisprescriptionaccountsforthedivergentvir-tualcorrections,whichcancelagainstthesingularitygeneratedwhenintegratingthereal–??emissioncontributionsnearx=1.Onethus?ndsthatJ(1?x)Q2/(1?x)istheleadingtermintheexpansionofthephysicalmomentumspaceevolutionkernelK(x,Q2)inthex→1limitwith(1?x)Q2?xed.Thetermproportionaltoδ(1?x)iscomprisedofpurelyvirtualcorrectionsassociatedwiththequarkformfactor.Thistermisinfrareddivergent,butasindicatedinthesecondlinein(2.7),thesingularitycancelsexactlyuponintegrating??overxwiththedivergenceoftheintegralofJ(1?x)Q2/(1?x)nearx→1.
NextIobservethateq.(2.7)stronglysuggeststhefollowinggeneralizationtoasys-tematicexpansionforx→1inpowersof1?x,or,moreconveniently(forreasonstobeclari?edinsection2.2),inpowersof
r≡1?x
rJW??2+??2dlnF(Q2)
IalsonotethatnointegrationovertheLandaupoleexplicitlyappearsinthismomen-tumspaceversionofSudakovresummation.Weshallseehoweverthattheperturbative??expansionsofthesubleadingphysicalSudakovanomalousdimensionsJiW2docontain??infraredrenormalons(atthedi?erenceofJW2!).
Onecanalsogivethegeneralizationofeq.(2.7),witharegularizedvirtualcontribution:K(x,Q)=21
dlnQ2
?1δ(1?x)+J0W?Q2
0?2??2??2?+rJ1W+Or=dlnQ2+
??d?2x,W2=1?x
r
whereF(x)isasmoothtestfunction.Theproofthat(2.12)isindeedequivalentto(2.7)forthetwoleadingtermsisgiveninAppendixA,byconsideringthemomentsofthetwoexpressions.
2.2DispersiverepresentationofthephysicalSudakovanomalousdimensions
(largeβ0)
ThecorrectnessoftheansatzEq.(2.11)canbecheckedatlarge–β0,upontakingthex→1expansionofthelarge–β0dispersiverepresentationofthephysicalevolutionkernel.Thisprocedurewillactuallyyieldamorepowerfulresult,namelythe(large–β0)dispersiverep-resentationsofthephysicalSudakovanomalousdimensionsJandJi.
Letusconsiderthelarge–β0butarbitraryx(0<x<1)dispersiverepresentation[8]ofthephysicalevolutionkernel.Atthelevelofthepartoniccalculation,theconvolutiononther.h.sof(2.1)becomestrivialinthelarge–β0limitsincetheO(αs)correctionstoF2(z,Q2)generatetermsthataresubleadingbypowersof1/β0.Therefore,inthislimitK(x,Q2)isdirectlyproportionaltothepartonicdF2(x,Q2)/dlnQ2,so
?∞2?d?K(x,Q2)?largeβ0=CF0??JW2?=+?10?1dxF(x)1?x???2,(2.13)J(1?x)Q
),andaMink(?2)istheV
integratedtime-likediscontinuityoftheone-loopV-schemecoupling(whichcorrespondstothesingledressedgluonpropagator,using‘naivenon-abelization’):d?2
ρV(?)=2daMink(?2)V
m2ρV(m2),(2.15)
–5–
where
ρV(?2)≡
1
π
=
1
lnwith
?
k2/Λ2V
?.Λ2V=Λ2e
5/3
,whereΛ2isde?nedinthe
12CA
?
1
(r)r
F(r)(ξ)+F0(ξ)+rF(r)
1(ξ)+O(r2),
where
ξ≡
?
W2,
with
F(r)(ξ)=?lnξ?
3
1
2
ξ+
2ξlnξ?4ξ+
1
2+2
lnξ?6?9ξlnξ+
1
2
ξ2.
Thus(.≡??2
d
r
F˙(r)(ξ)+F˙(r)0(ξ)+rF˙(r)1
(ξ)+O(r2),with
F˙(r)(ξ)=1?12
ξ2
F˙(r)0
(ξ)=?1?2ξlnξ+2ξ?ξ2
F˙(r)1
(ξ)=32
ξ+2ξ2lnξ?10ξ2,(2.17)(2.18)
(2.20)
(2.21)
(2.22)
(2.23)
(2.24)
and,takingasecondderivative:
¨(r)(?,x)=1xF
¨(r)(ξ)F02=2ξlnξ+2ξ2
¨(r)(ξ)=?9ξlnξ?35F1ξ+ξ2
r
with?FJ(ξ)+FJ0(ξ)+rFJ1(ξ)+O(r)+Vs(?)δ(1?x),2(2.28)
FJ(ξ)=F(r)(ξ)θ(ξ<1)
FJi(ξ)=
?1˙xF(?,x)=(r)Fi(ξ)θ(ξ<1),(2.29)
r
with?¨J(ξ)+F¨J(ξ)+rF¨J(ξ)+O(r)+V¨s(?)δ(1?x),F012(2.32)
¨J(ξ)=F¨(r)(ξ)θ(ξ<1),Fii¨J(ξ)=F¨(r)(ξ)θ(ξ<1)F(2.33)
(r)˙(r)(ξ),F˙(r)(ξ)in(2.20)andwhereIusedthefactthatallthetermsF(r)(ξ),Fi(ξ)andFi
(2.23)vanishatξ=1(whichallowstotreattheθfunctione?ectivelyasamultiplicativeconstantwhentakingthederivatives).Thesefeaturesactuallyfollowfromthestronger
–7–
˙(r)(?,x),bothpropertythattheexactfunctionF(r)(?,x),aswellasits?rstderivativeFvanishatξ=1,i.e.for?=1?x
4r??(1+r)(3+r)(1?ξ)2+O(1?ξ)3.(2.34)
Ifurthernotethatthetermswhichvanishforξ→0inFJi(butnotinFJ!)arelog-arithmicallyenhanced,hencenon-analytic,whichimplies(seebelow)thatthesubleadingphysicalSudakovanomalousdimensionsJidohaverenormalons(atthedi?erenceoftheleadingphysicalanomalousdimensionJ!).
ReportingtheresultEq.(2.32)into(2.14),onethusobtainsthesmallrexpansion(r=(1?x)/x)ofthephysicalevolutionkernel:
?1?2?K(x,Q)largeβ0=CF?∞
?Mink2¨2a(?)FJ1(ξ)+O(r)?2V
?∞2d?+δ(1?x)CF0Mink2¨a(?)FJ(ξ)?2V+d?20
?Ji(W)?largeβ0=CF2??2∞¨J(ξ)aMink(?2)FVd?2
dlnQ2?????=CF
largeβ0?∞0d?2
dlnQ2+?Q2
0d?2aMink(?2)V2???2222¨˙Vs(?/Q)+FJ(?/Q),
(2.38)
wheretheintegralonther.h.s.isindeedbothinfraredandultravioletconvergent.
–8–
2.3DispersiverepresentationofthephysicalSudakovanomalousdimensions
(?niteβ0)
Following[6,13],itisstraightforwardtogivethegeneralizationofEqs.(2.36)and(2.37)at?niteβ0:
2J(W)=CF?∞0d?2(2.39)
?2¨J(ξ),aMink(?2)FJii
where,infullanalogywith(2.15),
ρJ,Ji(?)=22daMinkJ,Ji(?)m2ρJ,Ji(m2),(2.40)
and,similarlyto(2.16),ρJ,Ji(?2)correspondtothetimelikediscontinuitiesofsome“Eu-
clidean”e?ectivecharges,originallyde?nedforspacelikemomenta:
?∞2?∞d?d?2Eucl2aJ,Ji(k)==?(1+?2/k2)200
?∞
0dlnQ2
?=CFd?2
Q2
dlnQ2+d?2
wheretermshavebeenarrangedproperlytohavebothinfraredandultravioletconver-gence:InotethattheintegralsoveraMink(?2)andaMink(?2)in(2.43),althoughinfraredFJconvergent,areseparatelyultravioletdivergent.
Fromthesedispersiverepresentations,theperturbativeexpansionsofthe‘jet’Sudakove?ectivechargesaMink(?2)andaMink(?2)canbederivedinastraightforwardway[6]JJi
orderbyorderinthefullnon-Abeliantheory,giventheexpansionsofJ(W2)andJi(W2)(andsimilarlyforaMink(?2)using(2.43)and(2.6)).F??22¨Vs(?/Q)+1?2???Mink222˙+aJ(?)FJ(?/Q)?1,aMink(?2)F?(2.43)
3.Drell-Yancase
3.1Theτ→1expansion
ThecrosssectionoftheDrell–Yanprocess,ha+hb→e+e?+X,is:
??1dxidσfi/ha(xi,?F)fj/hb(xj,?F)gij(τ,Q2,?2F)29Qsxj0i,j(3.1)
–9–
wheresisthehadroniccenter–of–massenergy,s?=xixjsisthepartonicone,Q2isthesquaredmassoftheleptonpairandτ=Q2/s?.Thepartonicthresholdτ→1ischaracter-izedbySudakovlogarithms.
Letusde?netheMellintransformofthequark–antiquarkpartoniccrosssectionin
222(3.1),e.g.inelectromagneticannihilationgqq?(τ,Q,?F)=eq[δ(1?τ)+O(αs)],by
?12222(3.2)dττN?1gqqGqq?(τ,Q,?F).?(N,Q,?F)≡
IntheN→∞limitonecanderive(seee.g.[14])theanalogueofEq.(2.4):
22dlnGqq?(N,Q,?F)
1?τ
whereKDY(τ,Q2)isthemomentumspacephysicalDrell–Yanevolutionkernelde?nedforarbitraryτ,andtheN-dependenttermsarecontrolledbythe‘soft’SudakovphysicalanomalousdimensionS:
S(?2)=A(αs(?2))+1
dln?2,(3.4)?2SQ2(1?τ)2+HDY(αs(Q2))+O(1/N),?(3.3)
whereDisthestandard(scheme-dependent)‘soft’SudakovanomalousdimensionrelevanttotheDrell-Yanprocess.Moreover,theconstanttermcanbeexpressedintermsoftheanalytically–continuedelectromagneticquarkformfactor[14]:
????22?dlnF(?Q)?2HDY(αs(Q))=S(?2),(3.5)2?
wheretheinfraredsingularitiescancel[14]inthesum,asin(2.6):
????22?dlnF(?Q)?2S(?2)HDY(αs(Q))=2????dR=G1,αs(Q2),ε=0+β(αs)
withR(αs(Q2))?2?=ln?F(?Q)
????2dln?F(?Q2)?
?(3.7)2?Dαs(Q2),?(3.6)1?τ1?τ
?????dln?F(?Q2)?2
+????+?+infrared?nite???02?δ(1?τ)+O(1?τ)S(?)DY??2?
–10–
WeseethatthephysicalSudakovanomalousdimensionScontrolstheleadingtermintheexpansionofthemomentumspacephysicalDrell–Yankernel(3.3)nearthreshold.Theτ→1limitistakensuchthatEDY=Q(1?τ),correspondingtothetotalenergycarriedbysoftgluonstothe?nalstate,iskept?xed.Thevirtualcontribution,proportionaltoδ(1?τ),isdeterminedbythequarkformfactor,analytically–continuedtothetime–likeaxis.Thistermisinfraredsingular,butuponperforminganintegraloverτthissingularitycancels
?2?2withtheonegeneratedbyintegratingthereal-emissionterm2SQ(1?τ)/(1?τ)near
τ→1.
SimilarlytotheDIScase,Eq.(3.7)suggestsageneralizationtoanexpansionforτ→1inpowersof1?τat?xedEDY.AsintheDIScase,however,itturnsout(seesection3.2)thatinordertoderiveadispersiverepresentationsuchanexpansionisnottheappropriateone.Instead,oneshouldconsideranexpansioninpowersofthealternativevariable:
rDY≡2
1?τ
τ
(3.8)
2,with:(properlynormalizedsothatrDY?1?τforτ→1)at?xedWDY
22
WDY≡rDYQ2,
(3.9)
namely:KDY(τ,Q2)=
2
dlnQ2
?2??2??2?
δ(1?τ)+S0WDY+rDYS1WDY+OrDY,
(3.10)
wherethecoe?cientsSandSiarethephysical‘soft’anomalousdimensionsappropriatetotheDrell-Yanprocess.Afterregularizingthevirtualcontribution,Eq.(3.10)canbewrittenas:KDY(τ,Q)=
?
2
2
dlnQ2
2
dlnQ2
δ(1?τ)+S0WDY+rDYS1WDY
+??
?
Q2
?
2
??
2
??2?+OrDY
=
d?2
τ+
√
rDY
2
SWDY
?
??
=
+
?
1
?
1
dτF(τ)
1?τ
S(1?τ)2Q
?
(3.12)
??2
,
whereF(τ)isasmoothtestfunction.
–11–
3.2DispersiverepresentationofthephysicalSudakovanomalousdimensions
(largeβ0)
InquiteasimilarwaytotheDIScase,westartfromthelarge–β0butarbitraryτ(0<τ<1)dispersiverepresentationofthephysicalDrell–Yanmomentumspaceevolutionkernel,
?2?KDY(τ,Q)largeβ0=CF?∞d?20
where?=?2/Q2,andexpandingtherealcontributionusingtheexplicitexpression3for(r)FDY(?,τ)in[8](Eq.(4.87)there),oneobtains:
FDY(?,τ)=(r)??)2+Vt(?)δ(1?τ),(3.14)41?4?22EDY???11?4?21?4?2
τ+√
2rDY=?2
rDY2FDY(ξDY)+F0,DY(ξDY)+rDYF1,DY(ξDY)+O(rDY),(r)(r)(r)(3.17)
with
FDY(ξDY)=2tanh(r)?1
1?4ξDY?(1?4ξDY)tanh?2??19+84ξDY?32ξDY2?1+(18+16ξDY+32ξDY)tanh(81?4ξDY?(?1?(
rDY
Takingonederivative(.=??2
rDY
with
(r)˙DYF(ξDY)=?d1+11+11?4ξDY+....(3.19)(r)˙(r)(ξDY)+rDYF˙DY˙(r)(ξDY)+O(r2),(ξDY)+FFDY0,DY1,DY(3.20)
˙(r)(ξDY)=F0,DY11?4ξDY12ξDY?1?4ξDY
8√1?4ξDY?4ξDYtanh?1?((3.21)1?4ξDY),(r)˙DY˙(r)(ξDY)arenowsingular,butintegrable,atthephase-whereallthetermsF(ξDY)andFi,DY
spaceboundary4ξDY=1.Thisresultfollowsimmediatelyfrom(3.19)whichyields:
2(r)˙DY(?,τ)=F42rDY
Usingtheseresultsin(3.14),andnotingthat:
?√θ(1?τ(1+
?FS(ξDY)+FS0(ξDY)+rDYFS1(ξDY)+O(rDY)+Vt(?)δ(1?τ),(3.24)2??2rDY1+....1?4ξDY(3.22)
rDY
with
FS(ξDY)=FDY(ξDY)θ(4ξDY<1)
FSi(ξDY)=(r)Fi,DY(ξDY)θ(4ξDY(r)<1),(3.25)
–13–
and
˙DY(?,τ)=F?2
1?4ξDY)??1
τ+√
rDY
??2
∞
0+rDYd?2??˙˙ρV(?)FS0(ξDY)?FS0(0)2?∞d?20(3.29)
?2¨t(?),aMink(?2)VV
whereIperformedintegrationbypartsinthevirtualcontribution,inordertoobtainat
˙t(0)beingin?nite(theintegralitselfisinfrareddivergentsinceleasta?niteintegrand,V2):¨t(0)=?1).Comparingwith(3.10)Ideduce(ξDY=?2/WDYV
?2?S(WDY)largeβ0=CF
andalso(?=?2/Q2):
????22?dlnF(?Q)?¨t(?),aMink(?2)VV(3.31)?∞0d?2??2˙S(ξDY)?F˙S(0),ρV(?)Fii(3.30)?2?2
–14–
whichchecksEq.(3.10)inthelarge–β0limit,andinadditiongivesthe(large–β0)dispersiverepresentationsofthephysicalSudakovanomalousdimensionsSandSi,aswellasthe(large–β0)dispersiverepresentationofthetime-likequarkformfactor[14].Finally,thedispersiverepresentationoftheregularizedvirtualcontributionin(3.11)isgivenby:
????2dln?F(?Q2)?S(?)=CF2
?2?∞d?20
Si(WDY)=CF2?∞
0?2d?2??˙˙ρS(?)FS(ξDY)?FS(0)2
dln?2;aMinkS,Si(?)≡?2?∞?2dm2
?2aMinkS,Si(?)2?2/k2?2+k2ρS,Si(?2).(3.35)
Fromthesedispersiverepresentations,theperturbativeexpansionsofthe‘soft’Sudakove?ectivechargesaMink(?2)andaMink(?2)canbederivedinastraightforwardway[6]orderSSi2)andS(W2).byorderinthefullnon-Abeliantheory,giventheexpansionsofS(WDYiDY
Furthermore,thegeneralizationof(3.31)is
????2dln?F(?Q2)?
whereasthatof(3.32)is:
????2dln?F(?Q2)?S(?)=CF2?2¨t(?),aMink(?2)VF(3.36)
?2?∞0d?2
4.Conclusions
IpresentedasimplemomentumspaceansatzforthestructureofasystematicexpansionofthephysicalevolutionskernelsaroundtheSudakovlimit,focussingonDISandtheDrell-Yanprocess.Eachorderintheexpansionisgivenbyapeculiar‘jet’or‘soft’(dependingontheprocess)physicalSudakovanomalousdimension.
Theansatzhasbeenderivedfromalarge–β0dispersiverepresentation,whichcanbereadilyextendedtothefullnon-Abeliantheoryat?niteβ0.Clearlymorejusti?cationsandchecksarestillneeded.Inthisrespect,thegeneralOPEmethodintroducedin[3,4]maygivetheappropriatetoolforasystematicderivation.Anotherpossibility(whichshallbethesubjectofafutureinvestigation)istoperformacheckoftheansatzbymatchingitwithexisting[24,25]?xedordercalculations;asaby-productonewouldget(iftheansatzturnsouttobecorrect)theperturbativeexpansionoftherelevant‘jet’and‘soft’physicalanomalousdimensionswhichoccurascoe?cientsintheseexpansions.
Ihaveshownthattheconnectionoftheansatzwiththedispersiverepresentationrequiresanon-trivial,andprocess-dependent,choiceofexpansionparameterintheSudakovlimit.WhiletheadequateparameterrintheDIScaseisstandard,andreferstothe?nalstatejetmassscale,themeaningofthecorrespondingparameterrDYintheDrell-Yancaseremainstobeunderstood:itdoesnotcorrespond(ascouldbenaivelyexpected)tothetotalenergyEDYradiatedinthe?nalstate.
2))momentumspaceItwasfoundthat,althoughtheleadingjet(J(W2))andsoft(S(WDY
physicalanomalousdimensionsdonot[6]haverenormalons(atleastatlarge–β0),renor-
2))physicalmalonsdostarttoappearinthesubleadingjet(J0(W2))andsoft(S0(WDY
anomalousdimensions.
GiventhemultiplicityofemergingphysicalSudakovanomalousdimensions,itwouldbeinterestingto?ndoutwhetherthereexistsanyrelationshipbetweenthem.Inparticular,onemightwonderwhetheranyexact,orapproximate,universalitypropertyholdsamong
Minkthevarious‘Sudakove?ectivecharges’aMinkJ,JiandaS,Si.Actually,fromtheobservationthat
thesumJ(W2)+J0(W2)isatotalderivativeatlarge–β0(whichfollowsfromthe?nitnessofFJ(ξ)+FJ0(ξ)atξ=0,see(2.22)),andmakingtheassumptionthatthisproperty
2stillholdsat?niteβ0,onecanalreadyreadilydeduceintheDIScasethataMinkJ(?)and
2aMinkJ0(?)haveidenticalexpansionsuptoNLO,andtherefore[6]coincidewiththecusp
anomalousdimensionuptothisorder.
Thetransitiontoan1/Nexpansioninmomentspacehasbeenshowntobestraightforward,andtheconnectionbetweenthemomentumandmomentspacejet(orsoft)scaleshasbeenclari?ed.Fromtheexpansionsinmomentspace,onecaneasilyobtainthemomentspacedispersiverepresentations,followingthemethodin[6],bysubstitutingthedispersiverepresentationsofthephysicaljetandsoftphysicalanomalousdimensionsinthemomentspaceexpansion.
ThelongitudinalstructurefunctionFL(x,Q2),whichhasnotbeenaddressedinthispaper,needsaspecialtreatment(tobereportedelsewhere).Indeed,itappearsthedispersiveap-proachdoesnotworkinastraightforwardwayinthiscase,essentiallybecauseatlarge–β0thelongitudinalphysicalevolutionkernelKL(x,Q2)doesnotcoincideanymorewiththe
–16–
derivativedFL(x,Q2)/dQ2.Thisisduetothefactthatthelongitudinalcoe?cientfunctionisO(αs),ratherthenO(α0s)asinthecaseofF2(whichcouldbereplacedatlarge–β0byitsleadingtermδ(1?z)ontherighthandsideofEq.(2.1)).Inparticular,KL(x,Q2)isnotsuppressedforx→1,contrarytoFL(x,Q2)itself.Preliminaryinvestigationnever-thelessseemstoindicatethatanansatzoftheformofEq.(2.11)mightstillbevalidforKL(x,Q2)(withadi?erentcoe?cientoftheδ(1?x)term),althoughtheconnectionwiththedispersiveapproachislost(excepteventuallyatlarge–β0,wheretheleadingSudakov??physicalanomalousdimensionJLW2couldbeatotalderivative).
Finally,althoughIhavestudiedherethesimplestexampleswhereonlyonescale(‘jet’or‘soft’)ispresent,theansatzcanbereadilyextendedtoothercases[6]wherebothofthesescalesdooccursimultaneously.
Acknowledgements
IwishtothankEinanGardiforanumberofpastdiscussionsonthedispersiveapproach.
A.N→∞expansioninmomentspace(DeepInelasticScattering)
TheN→∞expansionofthemomentspacephysicalevolutionkernelEq.(2.3)canbestraightforwardlyobtainedbytakingthemomentsofthemomentumspaceexpansionEq.(2.11)(r=1?x
??2?2?dlnF(Q2)JW+r
N1+i?∞0dt?1N?N+1tJiti?Q2
1+tNe?tt
N1+i?∞0dte?ti
Oneshouldnotethattheintegralonther.h.s.of(A.4)containsconstantterms,aswellaslogarithmsofN.Moreover,theintegralbeingconvergent,theconstanttermsdetermine??2?tJitW+O(1/N2+i).(A.4)
–17–
thelogarithmicallydivergentterms,giventhebetafunctioncoe?cients:seetheargumentfollowingEq.4in[13]–whichimpliesthattheknowledgeofthelogarithmictermsatagivensubleadingorderofthe1/Nexpansionalso?xestheconstanttermsatthesameorder.Inparticular,theN→∞expansionofthenexttoleadingrealemissionterminEq.(A.1)is:
?1
?2?1N?1
dxxJ0W=
r
JW
and,takingtheN→∞limitwithQ2/N?xedinsidetheintegralonther.h.s.,theanalogue
ofEq.(A.4):
?1??
2N?11?+O(1/N).(A.7)JtWdxx
t0inEq.(A.1)(wheretheIRdivergences
?2
?Q2d?2
Q
cancell,aswehaveseeninsection(2.1)).Since0tJt
dlnQ2
??2
=
?
∞
dt
?
1
N
?N+1
1
N
?
,(A.6)
TheinfrareddivergenceinEq.(A.7)canberegularizedasinEq.(2.12)bysubtractingfrom
?Q22
ther.h.s.of(A.7)theIRdivergentpiece0d?
r
JW
??2
?
=
+
??+
∞
dte?t
1
t
?
1
2
Combining(A.5)with(A.8)onethusgetsthelargeNexpansionofthe?rsttwoleadingrealemissiontermsinEq.(A.1):
???1??N1?1?2?dtJtWdxxN?1
t00
???∞?1?t2?dte+J0tW
N0
?
?2+O(1/N2).(t?2)JtW
?2JtW
?
??
(A.8)
The?rsttermonther.h.sof(A.9)canalsobewritten,uptoexponentiallysmallcorrectionsatlarge
RN
N,as0dt(e?t?1)1
?Q2
5
dlnQ2
d?2
+
Ialsonotethattakingthemomentsoftheleadingterminthe?rstlineofEq.(2.7)onegets(settingt=N(1?x)):
?
1
dxxN?1
1
=?
N
∞0
dte?t
1
?N?1
1
N
?
τ+
√
rDY
????
?2?dln?F(?Q2)?2SWDY+
N1+i
?
∞0
du
?
1
2N
?2N+1
uSiu
i
?
2Q
2
N1+i
?
∞0
due
?u
ThustheN→∞expansionofthenexttoleadingrealemissionterminEq.(B.1)is:
?
1
??
2?2
uSiuWDY+O(1/N2+i).
i
(B.3)
dττ
N?1
S0WDY=
?
2
?
1
rDY
?2?SWDY=2
?
∞0
du
?
1
2N
?2N+1
1
N2
?
,(B.5)
–19–
and,takingtheN→∞limitwithQ2/N2?xedinsidetheintegralonther.h.s.of(B.5),theanalogueofEq.(B.3):
?
1
dττ
N?1
2
u
TheinfrareddivergenceinEq.(B.6)canberegularizedasinEq.(3.11)bysubtractingfrom
?Q22
ther.h.s.of(B.6)theIRdivergentpiece0d?
dlnQ2
?2?SuWDY+O(1/N).?
2
(B.6)
cancell,aswehaveseeninsection(3.1)).Since
?Q2
inEq.(B.1)(wheretheIRdivergences
?
d?22Q2
Suu
???
2?DYSu2W
(B.7)
rDY
?2?
SWDY
?
+
??=2+
∞0
due?u
1
?
u
2
1
2
?2?(u?2)SuWDY+O(1/N2).
Combining(B.4)with(B.7)onethusgetsthelargeNexpansionofthe?rsttwoleading
realemissiontermsinEq.(B.1):?
1
dττ
N?1
??
2
?
∞0
N
due
?u
u?
??12?2
S0uWDY+
???
2?DY?2Su2W
N
du
1
?Q2
dlnQ2
d?2
+
1?τ
??22
S(1?τ)Q=2
?
N0
?udu1?
u
which,comparedto(B.6),checkstheequivalenceoftheleadingtermsin(3.7)and(3.11).
“
2fDYu2W
u
??
2?2
SuWDY+O(1/N),
?2
2QSu
(B.9)
u
S
”
.
–20–
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–21–