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Physics
Letters
B
www.elsevier.com/locate/physletb
Linear
and
non-linear
flow
mode
in
Pb–Pb
collisions
at
√
s
NN
=
2
.
76 TeV
.
ALICE
Collaboration
a
r
t
i
c
l
e
i
n
f
o
a
b
s
t
r
a
c
t
Articlehistory: Received22May2017Receivedinrevisedform10July2017 Accepted27July2017
Availableonline4August2017 Editor:L.Rolandi
The second and the third order anisotropic flow, V2and V3, are mostly determined by the corresponding
initial spatial anisotropy coefficients,
ε
2andε
3, in the initial density distribution. In addition to theirdependence on the same order initial anisotropy coefficient, higher order anisotropic flow, Vn (n >3),
can also have a significant contribution from lower order initial anisotropy coefficients, which leads to mode-coupling effects. In this Letter we investigate the linear and non-linear modes in higher order anisotropic flow Vn for n=4, 5, 6 with the ALICE detector at the Large Hadron Collider. The
measurements are done for particles in the pseudorapidity range |
η
|<0.8 and the transverse momentum range 0.2 <pT<5.0 GeV/c asa function of collision centrality. The results are compared with theoretical
calculations and provide important constraints on the initial conditions, including initial spatial geometry and its fluctuations, as well as the ratio of the shear viscosity to entropy density of the produced system.
©2017 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/). Funded by SCOAP3.
1. Introduction
The primary goal of the ultra-relativistic heavy-ion collision programme at the Large Hadron Collider (LHC) is to study the properties of the Quark–Gluon Plasma (QGP), a novel state of stronglyinteractingmatter thatis proposedto existathigh tem-peratures and energy densities [1,2]. Studies ofazimuthal corre-lationsofproduced particleshavecontributedsignificantly tothe characterisation of the matter created in heavy-ion collisions [3, 4]. Anisotropic flow, which quantifies the anisotropy of the mo-mentum distribution of final state particles, is sensitive to the event-by-event fluctuatinginitial geometry ofthe overlapregion, togetherwiththetransportpropertiesandequationofstateofthe system[4–7].Thesuccessfuldescriptionofanisotropicflowresults by hydrodynamic calculations suggests that the created medium behaves asa nearly perfect fluid [4,5] with a shear viscosity to entropy density ratio,
η
/
s, close to a conjectured lower bound 1/4π [8].AnisotropicflowischaracterisedusingaFourier decom-positionofthe particleazimuthal distributioninthe plane trans-versetothebeamdirection[9,10]:dN d
ϕ
∝
1+
2 ∞ n=1 vncos[
n(
ϕ
−
n)
],
(1)whereN isthenumberofproducedparticles,
ϕ
istheazimuthal angleoftheparticleandnisthenth orderflowsymmetryplane.
E-mailaddress:alice-publications@cern.ch.
The nth order (complex)anisotropic flow Vn isdefined as: Vn
≡
vneinn,wherevn
= |
Vn|istheflowcoefficient,andnrepresents theazimuthofVn inmomentumspace.Fornon-centralheavy-ion collisions,thedominantflowcoefficientisv2,referredtoaselliptic
flow.Non-vanishingvaluesofhigherflowcoefficientsv3–v6atthe
LHC are ascribed primarily to theresponse of theproduced QGP tofluctuationsoftheinitialenergydensityprofileofthecolliding nucleons[11–15].
The standard (moment-defined) initial anisotropy coefficients
ε
ntogetherwiththeircorrespondinginitialsymmetryplanes(also calledparticipantplanes)n canbecalculatedfromthetransverse positions
(
r,
φ)
oftheparticipatingnucleonsε
neinn≡ −
rneinφ
rn(
for n>
1),
(2)where
denotes the averageover the transverse position of all participating nucleons,
φ
is azimuthal angle, and n is the order of the coefficient [11,16]. It has been shown in [17,18] that V2and V3 are mostly determined with the same order initial
spa-tialanisotropycoefficients
ε
2andε
3,respectively.Consideringthatη/
s reducesthe hydrodynamic response of vn toε
n,it was pro-posedin[18–21]that vn/ε
n (forn=
2,3) couldbeadirectprobe to quantitatively constrain theη
/
s of the QGP in hydrodynamic calculations.However,ε
n cannotbedeterminedexperimentally. In-stead,theyareobtainedfromvarioustheoreticalmodels,resulting inlargeuncertaintiesintheestimatedη
/
s derivedindirectlyfromv2 andv3measurements[17,19].Ontheotherhand,higherorder
anisotropic flow Vn with n
>
3 probe smaller spatial scales and http://dx.doi.org/10.1016/j.physletb.2017.07.0600370-2693/©2017TheAuthor(s).PublishedbyElsevierB.V.ThisisanopenaccessarticleundertheCCBYlicense(http://creativecommons.org/licenses/by/4.0/).Fundedby SCOAP3.
thusaremoresensitiveto
η
/
s than V2 and V3 dueto morepro-nouncedviscouscorrections[16,22].Thus,thestudyofthefullset offlow coefficientsis expected to constrain both
ε
n andη
/
s si-multaneously.However,itwasrealisedlaterthat Vn withn>
3 is notlinearlycorrelatedwiththecorrespondingε
n [16,22,23],which makes the extractionofη
/
s from measurements of higherorder flow coefficientsless straightforward.In addition to the studyof flowcoefficients, the resultsof correlationsbetweendifferent or-der anisotropic flow angles and amplitudes shed light on both theearlystage dynamicsandthetransport propertiesofthe cre-atedQGP[24–32]. Inparticular,the characteristicpatternofflow symmetry plane correlations(also knownas angularcorrelations offlow-vectors) observedin experiments isreproduced quantita-tivelybytheoreticalcalculations[29–33].However,thecorrelations betweenflow coefficients (also known as amplitude correlations offlow-vectors),investigatedusingsymmetriccumulants,provide stricterconstraintsoninitialconditionsandη
/
s thanthe individ-ual vn measurements [24–28,31,32]. It is a challenge for current theoreticalmodelstoprovidequantitativedescriptions ofthe cor-relationsbetweendifferentorderflowcoefficients.Asdiscussedabove,itisknownthatthelowerorderanisotropic flowVn(n
=
2,3)islargelydeterminedbyalinearresponseofthe systemto the correspondingε
n (except in peripheral collisions). Higher order anisotropic flow Vn with n>
3 have contributions notonlyfromthelinearresponseofthesystemtoε
n,butalso con-tributionsproportionaltotheproductofε
2 and/orε
3.Thesecon-tributionsareusually callednon-linearresponse[25,34] inhigher orderanisotropic flow. Fora single event, Vn withn
=
4, 5 and 6can bedecomposedintotheso-calledlinearandthenon-linear contributions,accordingtoV4
=
V4NL+
V4L=
χ
4,22(
V2)
2+
V4L,
(3)V5
=
V5NL+
V5L=
χ
5,32V2V3+
V5L,
(4)V6
=
V6NL+
V6L=
χ
6,222(
V2)
3+
χ
6,33(
V3)
2+
χ
6,42V2V4L+
V6L.
(5)Here
χ
n,mk is a new observable called the non-linear mode co-efficient[34] andVnNL representsthenon-linearmode whichhas contributionsfrommodeswithlowerorderanisotropycoefficients. The VnL termrepresents the linear mode, which was naïvely ex-pected from the linear response of the system to the same or-derε
n. However, a recenthydrodynamic calculation showed thatVnLisnotdrivenbythelinearresponsetothestandardly moment-defined
ε
n introducedinEq.(2),butthecorresponding cumulant-definedanisotropy coefficientε
n [30,35]. For example, V4L isex-pectedtobedrivenbythe4th-ordercumulant-definedanisotropy coefficientanditscorrespondinginitialsymmetryplanewhichcan becalculatedas
ε
4ei44≡ −
z4−
3z22 r4=
ε
4e i44+
3 r22 r4ε
2 2ei42,
(6)where z
=
reiφ. The calculations forother order anisotropycoef-ficients and their corresponding initial symmetry planes can be found in [30,35]. If the non-linear and linear modes of higher order anisotropic flow, VnNL and VnL, are uncorrelated(e.g. VnL is perpendicularto VnNL), theycan beisolated. Oneofthe proposed approachestovalidatetheassumptionthat VNL
n andVnLare uncor-relatedistestingthefollowingrelations[25]:
V4(
V2∗)
2v22 V4(
V2∗)
2v22
=
v26 v24v22
,
(7) V5V3∗V2∗v22 V5V3∗V2∗v22
=
v24v32 v22v32v22
.
(8)Iftheaboverelationsarevalid,onecouldcombinetheanalyses ofhigherorderanisotropic flowwithrespecttotheir correspond-ingsymmetryplanesandtotheplanesoflower orderanisotropic flow V2 or V3 to eliminate theuncertainty frominitial state
as-sumptionsandextract
η
/
s withbetterprecision[34].In this Letter, the linear and non-linear modes in higher or-der anisotropicflow generationare studiedin Pb–Pbcollisions at
√
sNN
=
2.76 TeV with the ALICEdetector. The main observablesare introduced in Section 2 and the experimental setup is de-scribedinSection3.Section4presentsthestudyofthesystematic uncertaintiesoftheabovementionedobservables.Theresultsand their discussionare provided inSection 5.Section6 contains the summaryandconclusions.
2. Observablesandanalysismethods
Ideally, the flow coefficient vn can be measured via the az-imuthalcorrelationsofemitted particleswithrespecttothe sym-metryplane
n asvn
=
cos n(ϕ− n
)
.Sincen isunknown ex-perimentally,thesimplestapproachtoobtainvnisusing2-particle correlations: vn
{
2} =
cos n(
ϕ
1−
ϕ
2)
1/2=
vn2 1/2.
(9)Here
denotes theaverage overall particles ina single event andthenanaverageofoverallevents,indicatestheevent aver-ageofoverallevents,andϕ
irepresentstheazimuthalangleofthei-thparticle.Theanalysedeventsaredividedintotwosub-events AandB,separatedbyapseudorapiditygap, tosuppressnon-flow effects.Thelatteraretheazimuthal correlationsnot associatedto thecommonsymmetry plane
n,such asjetsandresonance de-cays.Thus,wemodifyEq.(9)to
vn
{
2} =
cos(
nϕ
1A−
nϕ
2B)
1/2=
v2n 1/2.
(10) Hereϕ
A 1 andϕ
B2 areselectedfromsubeventAandB,respectively.
Before introducing observables related to the linear and non-linearmodesinhigherorderanisotropicflow,itiscrucialtoverify whetherEqs.(7)–(8)areapplicable.The leftandrighthandsides ofEq.(7)areobtainedbyconstructingsuitablemulti-particle cor-relations[34]:
V4(
V2∗)
2v22 A V4(
V2∗)
2 A v22=
cos(
4ϕ
1A+
2ϕ
2A−
2ϕ
3B−
2ϕ
4B−
2ϕ
5B)
cos(
4ϕ
A 1−
2ϕ
2B−
2ϕ
3B)
cos
(
2ϕ
1A−
2ϕ
2B)
,
(11) v26 v24v22
=
cos(
2ϕ
1A+
2ϕ
2A+
2ϕ
3A−
2ϕ
4B−
2ϕ
5B−
2ϕ
6B)
cos(
2ϕ
A 1+
2ϕ
2A−
2ϕ
3B−
2ϕ
4B)
cos
(
2ϕ
1A−
2ϕ
2B)
.
(12)Similarly, we can validate Eq. (8) by calculating both sides with[34]:
V5V3∗V2∗v22 A V5V3∗V2∗ A v22=
cos(
5ϕ
1A+
2ϕ
2A−
3ϕ
3B−
2ϕ
4B−
2ϕ
5B)
cos(
5ϕ
A 1−
3ϕ
2B−
2ϕ
3B)
cos
(
2ϕ
1A−
2ϕ
2B)
,
(13)v22
=
cos(
3ϕ
A 1+
2ϕ
2A+
2ϕ
3A−
3ϕ
4B−
2ϕ
5B−
2ϕ
6B)
cos(
3ϕ
A 1+
2ϕ
2A−
3ϕ
3B−
2ϕ
4B)
cos
(
2ϕ
1A−
2ϕ
2B)
.
(14)ThemagnitudeofVnNL wasdenotedasvn{m}(here
misthe lower orderflow symmetry plane andm
=
2,3) in [34]. The no-tation vn,mk, wheren specifies the order ofthe flow termwhilem andk etc. denotethe contributinglower order flowsymmetry planes,isusedinthisLetter.Ifthelinearandnon-linearmodesare independent,thenthenon-linearmodeinhigherorderanisotropic flow can be analysed by correlating Vn with
2 or/and
3 [34].
Forsub-eventAwecandefine:
v4A,22
=
cos(
4ϕ
A 1−
2ϕ
2B−
2ϕ
3B)
cos(
2ϕ
A 1+
2ϕ
2A−
2ϕ
3B−
2ϕ
4B)
,
(15) v5A,32=
cos(
5ϕ
A 1−
3ϕ
2B−
2ϕ
3B)
cos(
3ϕ
A 1+
2ϕ
2A−
3ϕ
3B−
2ϕ
4B)
,
(16) v6A,222=
cos(
6ϕ
A 1−
2ϕ
2B−
2ϕ
3B−
2ϕ
4B)
cos(
2ϕ
A 1+
2ϕ
2A+
2ϕ
3A−
2ϕ
4B−
2ϕ
5B−
2ϕ
6B)
,
(17) v6A,33=
cos(
6ϕ
A 1−
3ϕ
2B−
3ϕ
3B)
cos(
3ϕ
A 1+
3ϕ
2A−
3ϕ
3B−
3ϕ
4B)
.
(18)Similarly, one can obtain vnB,mk for sub-event B. The average of
vA
n,mk andvnB,mk,definedasvn,mk,quantifies themagnitudeofthe non-linear mode in higher order anisotropic flow, which can be writtenas[36]: v4,22
=
v4v22cos(
44
−
42
)
v42≈
v4cos(
44
−
42
)
,
(19) v5,32=
v5v3v2cos(
55
−
33
−
22
)
v23v22≈
v5cos(
55
−
33
−
22
)
,
(20) v6,222=
v6v32cos(
66
−
62
)
v6 2≈
v6cos(
66
−
62
)
,
(21) v6,33=
v6v23cos(
66
−
63
)
v43≈
v6cos(
66
−
63
)
.
(22)The approximationis validifthe correlationbetweenlower (n
=
2,3)andhigher(n>
3)flowcoefficientsisweak.As canbe seen inEqs. (3)–(5),the calculation for V6 is more
complicatedthan V4 and V5,and theexact expression for vL6 is
currentlynotavailable. Therefore,weonlyfocuson thetwo non-linearmodesofV6 withoutdiscussingvL6.AccordingtoEqs.(3)to (4),themagnitudesofthelinearmodeinhigherorderanisotropic flowcanbecalculatedas:
vL4
=
v42{
2} −
v42,22,
(23) vL5=
v52{
2} −
v52,32.
(24)Theratioofvn,mk to vn{2
}
,denotedasρ
n,mk,canbecalculated as:ρ
4,22=
v4,22 v4{
2}
=
cos(
44
−
42
)
,
(25)ρ
5,32=
v5,32 v5{
2}
=
cos(
55
−
33
−
22
)
,
(26)ρ
6,222=
v6,222 v6{
2}
=
cos(
66
−
62
)
,
(27)ρ
6,33=
v6,33 v6{
2}
=
cos(
66
−
63
)
.
(28)These observablesmeasurethe correlationsbetweendifferent or-der flow symmetry planes if the correlations between different orderflow coefficientsareweak. Theyarevery similarto the so-called weighted event-plane correlationsmeasured by theATLAS Collaboration[33].Thedifferencesareasfollows:
v22v23isusedin Eq.(20)and(26),whilev22
v23wasusedin[33],whichdidnotconsidertheanti-correlationsbetweenv2 andv3foundin[27].In
addition,multi-particlecorrelationsareusedfor v2 andv3 inthe
denominatoroftheobservables,whiletwo-particlecorrelationsare used intheevent-planecorrelationswhichmight bebiasedfrom fluctuationsofv2 andv3.
The non-linear mode coefficients
χ
n,mk in Eqs. (3) to (5) are definedas:χ
4,22=
v4,22 v4 2 (29)χ
5,32=
v5,32 v22v23 (30)χ
6,222=
v6,222 v62 (31)χ
6,33=
v6,33 v43.
(32)These quantifythe contributions ofthe non-linearmode andare expectedtobeindependentofv2 orv3.
Alloftheobservablesabovearebasedon2- andmulti-particle correlations, which can beobtained usingthegeneric framework foranisotropicflowanalysesintroducedinRef.[24].
3. Experimentalsetupanddataanalysis
The data samples analysed in this Letter were recorded by ALICE during thePb–Pb runs ofthe LHCat a centre-of-mass en-ergy of
√
sNN=
2.76 TeVin 2010. Minimumbias Pb–Pb collisioneventswere triggeredby thecoincidenceofsignalsintheV0 de-tector [37,38], with an efficiency of 98.4% of the hadronic cross section [39].The V0 detectoris composed oftwo arrays of scin-tillator counters, V0-AandV0-C, whichcover the pseudorapidity ranges 2.8
<
η
<
5.1 and−
3.7<
η
<
−
1.7, respectively. Beam background events were rejected using the timing information fromtheV0andtheZeroDegreeCalorimeter(ZDC)[37]detectors andbycorrelatingreconstructedclustersandtrackletswiththe Sil-icon Pixel Detectors (SPD). The fraction of pile-up events in the datasampleisfoundtobenegligibleafterapplyingdedicated pile-upremovalcriteria[40].Onlyeventswithareconstructedprimary vertex within±
10 cm fromthe nominal interaction point along the beam direction were used in this analysis. The primary ver-texwasestimatedusingtracksreconstructedbytheInnerTracking System (ITS) [37,41] and TimeProjection Chamber (TPC) [37,42]. The collision centrality was determined from the measured V0 amplitudeandcentralityintervalsweredefinedfollowingthe pro-ceduredescribedin[39].About13millionPb–Pbeventspassedall oftheeventselectioncriteria.Tracksreconstructedusingthecombinedinformationfromthe TPCand ITS are used in this analysis. This combination ensures a high detection efficiency, optimum momentum resolution, and aminimum contributionfromphoton conversions andsecondary charged particles produced either in the detector material or fromweakdecays. Toreduce the contributionsfrom secondaries, charged tracks were required to have a distance of closest ap-proachtotheprimary vertexinthelongitudinal(z)directionand transverse (xy) plane smaller than 3.2 cm and 2.4 cm, respec-tively.Additionally, tracks were required to haveat least 70TPC spacepointsoutofthemaximum159.Theaverage
χ
2 perdegreeoffreedom ofthe trackfit to theTPC spacepoints was required to be below 2. In this study, tracks were selected in the pseu-dorapidity range
|
η
|
<
0.8 and the transverse momentum range 0.2<
pT<
5.0 GeV/c.4. Systematicuncertainties
Numeroussources ofsystematicuncertaintywere investigated byvaryingtheeventandtrackselectionaswellastheuncertainty associated with the possible remaining non-flow effects in the analysis. The variation of theresults withthe collision centrality iscalculatedbyalternativelyusingtheTPCorSPDtoestimatethe eventmultiplicityandis foundto be lessthan3% forall observ-ables.Resultswithoppositepolaritiesofthemagneticfieldwithin theALICEdetectorandwithnarrowingthenominal
±
10cmrange ofthereconstructedvertexalongthebeamdirectionfromthe cen-treoftheALICEdetectorto9,8and7cmdonotshowadifference ofmorethan2%comparedtothedefaultselectioncriteriafor var-iousmeasurements. Thecontributions frompile-upevents tothe finalsystematicuncertaintyarefoundto benegligible.The sensi-tivityto the trackselection criteria was explored by varying the numberofTPCspacepoints andby usingtracksreconstructedin theTPC alone.Varying the numberof TPCspace points from70 to80,90and100out ofa possible158,results ina1–3% varia-tionof theresultsfor vn,within 1.5%forρ
n,mk andχ
n,mk.Using TPC-onlytracksleadstoadifferenceoflessthan14%,17%and8% forvn,ρ
n,mk andχ
n,mk,respectively.Botheffectswereincludedin theevaluationofthesystematicuncertainty.Severaldifferent ap-proaches have been applied to estimate the effects of non-flow. Theseincludethe investigationofmulti-particlecorrelationswith various|
η
|
gaps,theapplicationofthelike-signtechniquewhich correlatestwoparticleswitheitherallpositiveornegativecharges andsuppresssuchnon-flowasduetoresonancedecays,aswellas thecalculationsusingHIJINGMonteCarlosimulations[43],which donotincludeanisotropicflow.Itwasfoundthatthepossible re-mainingnon-flow effects arelessthan 10.5%,11% and7%for vn,ρ
n,mkandχ
n,mk,respectively.Theyaretakenintoaccountinthe fi-nalsystematicuncertainty.The systematicuncertainties evaluated foreachsourcementionedabovewereaddedinquadratureto ob-tainthetotalsystematicuncertaintyofthemeasurements.5. Resultsanddiscussion
As discussed in Sec. 2, one can validate the assumption that linearandnon-linear modesinhigher orderanisotropic flow are uncorrelated via Eqs. (7) and (8). These have been tested in A Multi-Phase Transport (AMPT) model [25] as well as in the hy-drodynamiccalculations [44]. Good agreementbetween left- and right-hand sides of Eqs. (7) and (8) is found for all centrality classes,independentoftheinitialconditionsandtheidealor vis-cous fluid dynamics used in the calculations. Thus, it is crucial tocheck theseequalities indata,to further confirmthe assump-tion that the two components are uncorrelated and can be iso-latedindependently.Fig. 1 confirms thatthe agreementobserved
Fig. 1. Studyofrelationshipbetweenlinear and non-linearmodesinhigher or-deranisotropicflowinPb–Pbcollisionsat√sNN=2.76 TeV,accordingtoEqs.(7) and(8).
intheoreticalcalculationsisalsopresentinthedatadespitesmall deviationsfound incentral collisions whentestingEqs. (8).Their centralitydependencyare similarastheprevious theoretical pre-dictions [25,44]. The measurements support the assumption that higher order anisotropic flow Vn (n
>
3) can be modeled as the sumofindependentlinearandnon-linearmodes.Themagnitudesoflinearandnon-linearmodesinhigherorder anisotropic flow are reported as a function of collision central-ity in Fig. 2. In this Letter, sub-events A and B are built in the pseudorapidity ranges
−
0.8<
η
<
−
0.4 and 0.4<
η
<
0.8, re-spectively,whichresultsinapseudorapiditygapof|
η
|
>
0.8 for all presentedmeasurements. It canbe seen thatthe linearmodevL
4 dependsweaklyoncentralityandisthelarger contributionto
v4
{
2}
forthecentralityrange0–30%. Thenon-linearmode, v4,22,increases monotonicallyas thecentrality decreases andsaturates around centrality percentile 50%, becoming the dominantsource forcentralityintervalsabove 40%.Similar trendsofcentrality de-pendencehavebeenobservedforV5,althoughv5,32becomes the
dominantcontributionincentralitypercentileabove30%.Onlytwo non-linearcomponentsv6,222and v6,33arediscussedforV6.Itis
showninFig. 2 (right)that v6,222 increasesmonotonically asthe
centrality decreases to centrality 50%, while v6,33 has a weaker
centralitydependencecomparedtov6,222.
The linear and non-linear modes in higher order anisotropic flow were investigated by the ATLAS Collaboration [26] using a differentapproachbasedon“EventShapeEngineering”[45].With thismethodonecanutiliselargefluctuationsintheinitial geome-tryofthesystemtoselecteventscorrespondingtoaspecificinitial shape. Theconclusion is qualitativelyconsistent withwhat is re-portedhere, although a direct comparisonis not possibledueto the different kinematic cuts (especially the integrated pT range)
usedinthetwomeasurements.Thehigherorderanisotropicflow induced by lower order anisotropic flow were alsomeasured us-ing the event-plane method at the LHC [14,46]. However, the measurements of the non-linear mode presented in this Letter are based on themulti-particle correlationsmethod witha
|
η
|
gap. This method makes it easier to measure an observable likev5,32,whichislessstraightforwardtodefineusingtheeventplane
method [14,46]. In addition, as pointed out in [25,34,47], this new multi-particle correlations method should strongly suppress short-range(inpseudorapidity)non-floweffectsandprovidesa ro-bust measurement withoutany dependenceon the experimental acceptance. The measurements are compared to recent hydrody-namic calculationsfroma hybrid
IP
-Glasma
+ MUSIC + UrQMD
model[48],inwhichrealisticevent-by-eventinitialconditionsare used and the hydrodynamic evolution takes into account both shear andbulkviscosity. It isshownthat thishydrodynamic cal-culationcould describe quantitatively thetotal magnitudes of V4and V6,aswell asthe magnitudesoftheir linear andnon-linear
modes,whileitslightlyoverestimatestheresultsfor V5.
Thecentralitydependenceof
ρ
n,mk,whichquantifiesthe angu-larcorrelationsbetweendifferentorderflow symmetry planes,isFig. 2. Centralitydependenceofv4(left),v5(middle)andv6(right)inPb–Pbcollisionsat√sNN=2.76 TeV.Contributionsfromlinearandnon-linearmodesarepresented
withopenandsolidmarkers,respectively.ThehydrodynamiccalculationsfromIP-Glasma+ MUSIC + UrQMD[48]areshownforcomparison.
Fig. 3. Centralitydependenceofρn,mkinPb–Pbcollisionsat√sNN=2.76 TeV.ATLAS
measurementsbasedontheevent-planecorrelation[33]arepresentedwithopen markers.ThehydrodynamiccalculationsfromIP-Glasma+ MUSIC + UrQMD[48] areshownwithopenbands.(Forinterpretationofthereferencestocolourinthis figurelegend,thereaderisreferredtothewebversionofthisarticle.)
presentedin Fig. 3.It is observedthat
ρ
4,22 increases fromcen-tral to peripheral collisions, which suggeststhat the correlations between
2 and
4 are stronger in peripheral than in central
collisions. It implies that VNL4 tends to align with V4 in more
peripheral collisions. The results of
ρ
6,33, which measures thecorrelation of
3 and
6,do not exhibit a strong centrality
de-pendencewithinthestatisticaluncertainties.Asmentionedabove,
ρ
4,22 andρ
6,33 are similar to the previous “event-planecorrela-tion” measurements
cos(44−
42)
w
and cos(66−
63)
w
in [33]. The comparisons between measurements of these ob-servablesare also presentedin Fig. 3. Theresults are compatible with each other, despite the different kinematic ranges used by ATLAS and this analysis. It should be also noted that the mea-surements of
ρ
n,mk presented in this Letter show the symmetry plane correlations at mid-pseudorapidity|
η
|
<
0.8 while ATLAS measuredthesymmetryplanecorrelationsusing−
4.8<
η
<
−
0.5 and 0.5<
η
<
4.8 for two-plane correlations, and using−
2.7<
η
<
−
0.5, 0.5<
η
<
2.7 and 3.3<
|
η
|
<
4.8 for 3-plane corre-lations [33]. Previous investigations suggest that there might beη-dependent
fluctuationsoftheflowsymmetryplaneandtheflow magnitude[49,50]. As a consequence,one might expect a differ-ence when measuring the correlations of flow symmetry planes fromdifferentpseudorapidityregions.However,Fig. 3showsgood agreement between the ALICE and ATLAS measurements. There-fore, no obvious indication that the flow symmetry plane varies withη
can be deduced fromthis comparison. It is noticeableinFig. 3that the
ρ
5,32measurement seemsslightlyhigherthanthe cos(55−
33−
22)
w
measurement. This is mainly dueto asmall difference betweenthe definitionsof the observable as in-troduced inSec. 2: the term
v22v23
1/2isused in
ρ
5,32, whereasv22
1/2v231/2 is usedin the“event-plane correlations”[33]. Con-sidering theknown anti-correlations between v2 and v3 [26,27],v2 2v23
1/2couldbeupto10%lowerthan
v2 2 1/2 v2 3 1/2 depending on thecentralityclass[27],leading toa slightlylargerρ
5,32 than cos(55−
33−
22)
w
fromATLAS.Ithasbeenobservedinhydrodynamicandtransportmodel cal-culations that the symmetry plane correlations, e.g. correlations of second and fourth order symmetry planes, change sign dur-ingthesystemevolution[29,30,32].Themeasuredflowsymmetry plane correlations could be nicely explained by the combination of contributions fromlinear and non-linear modes in higher or-der anisotropic flow [30]. This indicates that the flow symmetry plane correlation
ρ
n,mk carries important information about the dynamic evolution ofthe created system. In addition, the model calculations suggest that stronger initial symmetry plane corre-lations are reflected in stronger correlations between the flow symmetry planes in the final state [29,32]. And a larger value ofη
/
s of the QGP leads to weaker flow symmetry plane corre-lations in the final state. As pointed out in [29], the hydrody-namic calculations fromVISH2
+ 1
using Monte Carlo Glauber (MC-Glb) or Monte Carlo Kharzeev–Levin–Nardi (MC-KLN) initial conditions can only describe qualitatively the trends ofthe cen-trality dependence of the event-plane correlation measurements by ATLAS.Itisthereforeexpectedthatthesehydrodynamic calcu-lationscannotdescribethepresentedALICEmeasurements,which are compatiblewith theATLAS event-plane correlation measure-ments. Fig. 3 shows that the hydrodynamic calculations fromIP
-Glasma
+ MUSIC + UrQMD
[48] reproduce nicely the mea-surements of symmetry plane correlationsρ
n,mk. The measure-ments ofρ
n,mk presented in this Letter, together with the com-parison tohydrodynamiccalculations, shouldplaceconstraintson theinitialconditionsandη
/
s oftheQGPinhydrodynamic calcula-tions.Fig. 4presentsthemeasurementsofthenon-linearmode coef-ficientsasafunctionofcollisioncentrality.Itisobservedthat
χ
4,22and
χ
6,222 decrease modestly from central to mid-centralcolli-sions,andstayalmost constantfrommid-centraltomore periph-eralcollisions.For
χ
5,32andχ
6,33strongcentralitydependenceisnot observed either. Thus, the dramatic increase of vn,mk shown in Fig. 2 appears to be mainly dueto the increase of v2 and/or
v3 fromcentraltoperipheralcollisionsandnottheincreaseofthe
non-linearmodecoefficient.Itisalsonoteworthythatthe relation-ship of
χ
4,22∼
χ
6,33≈
χ5,322 is approximatelyvalid, aspredictedby hydrodynamic calculations[34].Thecomparisons to event-by-eventviscoushydrodynamiccalculationsfrom
VISH2
+ 1
[44]and fromIP
-Glasma
+ MUSIC + UrQMD
[48] are also presented inFig. 4.
VISH2
+ 1
showsthatχ
4,22 calculationswithMC-Glbini-tial conditions are larger than those with MC-KLN initial condi-tions,i.e.
χ
4,22dependsontheinitialconditions.Atthesametime,Fig. 4. CentralitydependenceofχinPb–Pbcollisionsat√sNN=2.76 TeV.
Hydro-dynamiccalculationsfromVISH2+ 1[44]areshowninshadedareasandtheone fromIP-Glasma+ MUSIC + UrQMD[48]areshownwithopenbands.(For inter-pretationofthereferencestocolourinthisfigurelegend,thereaderisreferredto thewebversionofthisarticle.)
thecurveswithdifferent
η
/
s valuesforVISH2
+ 1
arevery sim-ilar,indicating thatχ
4,22 isinsensitivetoη
/
s.The measurementsfavour IP-GlasmaandMC-KLN over MC-Glb initial conditions re-gardlessof
η
/
s.Thissuggeststhattheχ
4,22measurement canbeusedto constrain the initial conditions, withless concernof the settingof
η
/
s(
T)
inhydrodynamiccalculationsthanpreviousflow observables.It was predicted that
χ
6,222<
χ
6,33 based on the idealhy-drodynamiccalculationusingsmoothinitialGaussiandensity pro-files [34], whereas an opposite prediction was obtained in the ideal hydrodynamic calculation evolving genuinely bumpy initial conditionsobtainedfromaMonteCarlosamplingoftheinitial nu-cleonpositionsinthecollidingnuclei[44].ItisseeninFig. 4that
χ
6,222∼
χ
6,33 within the current uncertainties. The data are notabletodiscriminatethedifferentpredictionsin[34]and[44]. Hy-drodynamiccalculationsusingMC-KLNandIP-Glasmainitial con-ditions give better descriptions of
χ
6,222, compared to the onesusing MC-Glb initial conditions. For
χ
5,32 noneof thecombina-tionsofinitialconditionsand
η
/
s inthehydrodynamiccalculations agreequantitatively withdata. Thismight be due tothe current difficulty of describing the anti-correlations between v2 and v3in hydrodynamic calculations [27,51], which are involved in the calculation of
χ
5,32. Furthermore,VISH2
+ 1
calculations showthat
χ
5,32 andχ
6,33 are very weakly sensitiveto the initialcon-ditions,butdecreaseas
η
/
s increases. Theinvestigation withtheVISH2
+ 1
hydrodynamic framework shows that the sensitivity ofχ
5,32 andχ
6,33 toη
/
s is not dueto sensitivityto shearvis-couseffectsduring thebuildupofhydrodynamic flow.Instead,as foundin[44],itisduetothe
η
/
s atfreeze-out.Themeasurements ofχ
5,32 andχ
6,33 do not further constrain theη
/
s duringsys-temevolution,however,theyprovideuniqueinformationon
η
/
s atfreeze-outwhichwas poorlyknownandcannot beobtainedfrom otheranisotropicflowrelatedobservables.Furtherimprovementof model calculations on correlations between different order flow coefficients are necessary to better understand the comparison of
χ
5,32 obtained from data and hydrodynamic calculations. Theχ
6,33 results are consistent withhydrodynamic calculationsfromVISH2
+ 1
withMC-KLN initialconditions usingη
/
s=
0.08 andIP
-Glasma
+ MUSIC + UrQMD
with aη
/
s=
0.095. It is shown thatχ
5,32 andχ
6,33 have a weak centrality dependence if asmaller
η
/
s isusedinthehydrodynamiccalculations.Suchaweakcentrality dependence of
χ
5,32 andχ
6,33 is observed in data aswell.Themeasurementspresentedheresuggestasmall
η
/
s valueatfreeze-out,whichcanbeusefultoconstrainthetemperature de-pendenceoftheshearviscosityoverentropydensityratio,
η
/
s(T),
in the development of hydrodynamic frameworks. These results suggest that future tuning of the parameterisations ofη
/
s(T)
in hydrodynamic frameworks using the presented measurements is necessary.6. Summary
The linear and non-linear modes in higher order anisotropic flow generation were studied with 2- and multi-particle corre-lations in Pb–Pb collisions at
√
sNN=
2.76 TeV. The resultspre-sentedinthisLetter show that higherorderanisotropic flowcan be isolated into two independent contributions: the component thatarisesfromanon-linearresponseofthesystemtothelower orderinitialanisotropycoefficients
ε
2and/orε
3,andalinearmodewhichisdrivenbylinearresponseofthesystemtothesameorder cumulant-definedanisotropycoefficient. A weakcentrality depen-denceisobservedforthecontributionsfromlinearmodewhereas the contributions from non-linear mode increase dramatically as the collision centrality decreases, and it becomes the dominant source inhigher orderanisotropic flow inmid-central to periph-eralcollisions. Itisshownthat thisis mainlyduetotheincrease of lower order flow coefficients v2 and v3. The correlations
be-tween different flow symmetry planes are measured. The results are compatible withthe previous “event-plane correlation” mea-surements,andcanbequantitativelydescribedbycalculations us-ing the
IP
-Glasma
+ MUSIC + UrQMD
framework. Furthermore, non-linearmode coefficients, whichhave differentsensitivitiesto the shearviscosity over entropydensity ratioη
/
s and theinitial conditions,are presented inthisLetter. Comparisons to hydrody-namic calculations suggest that the data is described better by hydrodynamic calculationswithsmallerη
/
s.Inaddition,the MC-Glbinitialconditionisdisfavouredbythepresentedresults.Measurementsoflinearandnon-linearmodesinhigher order anisotropic flow and their comparison to hydrodynamic calcula-tionsprovidemorepreciseconstraintsontheinitialconditionsand temperaturedependenceof
η
/
s.Theseresultscouldalsooffernew insightsintothegeometryofthefluctuatinginitialstate andinto the dynamical evolution ofthe stronglyinteracting medium pro-ducedinrelativisticheavy-ioncollisionsattheLHC.Acknowledgements
The ALICE Collaboration would like to thank all its engineers andtechniciansfortheir invaluablecontributions tothe construc-tionoftheexperimentandtheCERNacceleratorteamsforthe out-standingperformanceoftheLHCcomplex.TheALICECollaboration gratefully acknowledges the resources and support provided by all Gridcentres andtheWorldwide LHC ComputingGrid (WLCG) collaboration. The ALICE Collaboration acknowledges the follow-ing funding agencies for their support in building and running the ALICE detector: A. I. Alikhanyan National Science Laboratory (YerevanPhysicsInstitute)Foundation (ANSL),State Committeeof Science andWorld Federation ofScientists (WFS), Armenia; Aus-trian Academy of Sciences and Österreichische Nationalstiftung für Forschung, Technologie undEntwicklung, Austria; Ministry of CommunicationsandHighTechnologies,NationalNuclearResearch Center, Azerbaijan;Conselho NacionaldeDesenvolvimento Cientí-ficoe Tecnológico(CNPq),UniversidadeFederal doRioGrandedo Sul (UFRGS),Financiadorade Estudose Projetos(Finep)and Fun-dação de Amparo à Pesquisa do Estado de São Paulo (FAPESP),
Brazil; Ministry of Science & Technology of China (MSTC), Na-tional Natural Science Foundation of China (NSFC) and Ministry of Education of China (MOEC), China; Ministry of Science, Edu-cationandSportsandCroatian Science Foundation, Croatia; Min-istryofEducation,YouthandSportsoftheCzech Republic,Czech Republic; The Danish Council for Independent Research — Nat-ural Sciences, the Carlsberg Foundation and Danish National Re-search Foundation (DNRF), Denmark;Helsinki Institute ofPhysics (HIP),Finland;Commissariatàl’EnergieAtomique(CEA)and Insti-tut Nationalde Physique Nucléaire etde Physique desParticules (IN2P3)and Centre Nationalde laRecherche Scientifique(CNRS), France; Bundesministerium für Bildung, Wissenschaft, Forschung und Technologie (BMBF) and GSI Helmholtzzentrum für Schwe-rionenforschungGmbH,Germany;GeneralSecretariatforResearch and Technology, Ministry of Education, Research and Religions, Greece; National Research, Development and Innovation Office, Hungary; Department of Atomic Energy, Government of India (DAE) and Council of Scientific and Industrial Research (CSIR), NewDelhi,India; IndonesianInstituteofScience, Indonesia; Cen-tro Fermi - Museo Storico della Fisica e Centro Studi e Ricerche EnricoFermiandIstitutoNazionalediFisicaNucleare(INFN),Italy; InstituteforInnovativeScience andTechnology,NagasakiInstitute ofApplied Science (IIST),Japan Society forthe Promotionof Sci-ence(JSPS)KAKENHIandJapanese MinistryofEducation,Culture, Sports, Science and Technology (MEXT), Japan; Consejo Nacional deCienciayTecnología (CONACYT),throughFondodeCooperatión Internacional en Ciencia y Tecnología (FONCICYT) and Dirección General de Asuntos del Personal Académico (DGAPA), Mexico; NederlandseOrganisatievoorWetenschappelijkOnderzoek(NWO), Netherlands; The Research Council of Norway, Norway; Commis-sion on Science and Technology for Sustainable Development in theSouth(COMSATS),Pakistan;PontificiaUniversidadCatólicadel Perú,Peru;MinistryofScienceandHigherEducationandNational Science Centre, Poland; Korea Institute of Science and Technol-ogyInformationandNationalResearchFoundationofKorea(NRF), Republicof Korea; Ministryof Education andScientific Research, InstituteofAtomicPhysicsandRomanianNationalAgencyfor Sci-ence,Technology andInnovation,Romania; JointInstitute for Nu-clearResearch(JINR),MinistryofEducationandScienceofthe Rus-sian FederationandNationalResearchCentre KurchatovInstitute, Russia;Ministry ofEducation, Science,Research andSportofthe Slovak Republic, Slovakia; NationalResearch Foundation ofSouth Africa,SouthAfrica; Centrode AplicacionesTecnológicasy Desar-rolloNuclear(CEADEN),Cubaenergía,Cuba;MinisteriodeCienciae Innovación andCentrodeInvestigacionesEnergéticas, Medioambi-entalesyTecnológicas(CIEMAT),Spain;SwedishResearchCouncil (VR)andKnut&AliceWallenbergFoundation(KAW),Sweden; Eu-ropean Organization for Nuclear Research, Switzerland; National Science andTechnology DevelopmentAgency (NSDTA), Suranaree University of Technology (SUT) and Office of the Higher Educa-tionCommissionunderNRUprojectofThailand,Thailand;Turkish Atomic Energy Agency (TAEK), Turkey; National Academy of Sci-encesofUkraine,Ukraine;ScienceandTechnologyFacilities Coun-cil (STFC), United Kingdom; National Science Foundation of the United Statesof America(NSF) and United StatesDepartment of Energy,OfficeofNuclearPhysics(DOENP),UnitedStatesof Amer-ica.
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