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Physics
Letters
B
www.elsevier.com/locate/physletb
Longitudinal
asymmetry
and
its
effect
on
pseudorapidity
distributions
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
Article history:Received30October2017
Receivedinrevisedform9March2018 Accepted15March2018
Availableonline22March2018 Editor:L.Rolandi
FirstresultsonthelongitudinalasymmetryanditseffectonthepseudorapiditydistributionsinPb–Pb collisions at√sNN =2.76 TeVattheLargeHadronColliderareobtainedwiththe ALICEdetector.The longitudinal asymmetry arises becauseofanunequal number ofparticipatingnucleons fromthe two collidingnuclei,andisestimatedforeacheventbymeasuringtheenergyintheforward neutron-Zero-Degree-Calorimeters(ZNs).Theeffectofthelongitudinalasymmetryismeasuredonthepseudorapidity distributionsofchargedparticlesintheregions|
η
|<0.9,2.8<η
<5.1 and−3.7<η
<−1.7 bytaking theratioofthepseudorapiditydistributionsfromeventscorrespondingtodifferentregionsofasymmetry. Thecoefficientsofapolynomialfittotheratiocharacterisetheeffectoftheasymmetry.AMonteCarlo simulationusingaGlaubermodelforthecollidingnucleiistunedtoreproducethespectrumintheZNs andprovidesarelationbetweenthemeasurablelongitudinalasymmetryandtheshiftintherapidity( y0) oftheparticipantzoneformedbytheunequalnumberofparticipatingnucleons.Thedependenceofthe coefficientofthelinearterminthepolynomialexpansion,c1,onthemeanvalueofy0isinvestigated.©2018TheAuthor(s).PublishedbyElsevierB.V.ThisisanopenaccessarticleundertheCCBYlicense (http://creativecommons.org/licenses/by/4.0/).FundedbySCOAP3.
1. Introduction
Ina heavy-ion collision,the numberof nucleons participating fromeach ofthe two collidingnuclei isfinite, andwillfluctuate event-by-event. The kinematic centre of mass of the participant zone,definedastheoverlapregionofthecollidingnuclei,in gen-eralhasafinitemomentuminthenucleon–nucleoncentreofmass frame because of the unequal number of nucleons participating fromthetwonuclei.Thismomentumcausesalongitudinal asym-metry in the collision and corresponds to a shift of rapidity of the participantzone withrespect to the nucleon–nucleon centre ofmass (CM) rapidity,termed therapidity-shift y0. The value of
y0isindicativeofthemagnitudeofthelongitudinalasymmetryof
thecollision [1,2].Assumingthenumberofnucleonsparticipating fromeachofthetwonucleiis A and B,thelongitudinal asymme-tryinparticipantsisdefinedas
α
part=
AA−+BB andtherapidity-shiftcanbeapproximatedasy0
∼
=
12lnA
B atLHCenergies [2].
The shift in the CM frame of the participant zone, which evolvesintoastateofdensenuclearmatter,needstobeexplored in heavy-ion collision models. Comparison of model predictions with the observed
-polarisation, possibly due to vorticity from the initial state angular momentum surviving the evolution, re-quiresaprecisedetermination ofinitial conditionsandhencethe
E-mail address:alice-publications@cern.ch.
shiftintheCMframe [3–5].Such ashiftmayalsoaffect observa-tions on correlationsamongst particles,which eventually provide informationaboutthestate ofthematterthroughmodel compar-isons.Further,theresultantdecreaseintheCMenergymayaffect various observables includingthe particle multiplicity.The trans-verse spectraareknowntobe affectedby theinitialgeometryof the events, as estimated through techniques of event shape en-gineering, indicating an interplay between radial and transverse flow [6].Themeasurementoflongitudinalasymmetrywillprovide anewparametertowardseventshapeengineering,affectingmany otherobservables.
The simplest of all possible investigations into the effect of longitudinal asymmetry is a search for modification ofthe kine-maticdistributionoftheparticles.Thepseudorapiditydistribution (dN
/
dη
)ofsoftparticles,averagedoveralargenumberofevents, is symmetric in collisions of identical nuclei. These distributions were observed to be asymmetric in collisions of unequal nuclei such as d–Au [7] and p–Pb [8–10] and have been explained in termsoftherapidity-shiftoftheparticipantzone [11].Ina heavy-ioncollision,theeffectoftherapidity-shiftoftheparticipantzone shouldbediscernibleinthedistributionofproducedparticles.This smalleffectcan beestimatedby takingtheratioof pseudorapid-ity distributions inevents corresponding todifferent longitudinal asymmetries [2].It was suggested that the rapidity distribution of an event, scaled by the average rapidity distribution, can be expanded in termsofChebyshevpolynomials, wherethecoefficientsof
expan-https://doi.org/10.1016/j.physletb.2018.03.051
0370-2693/©2018TheAuthor(s).PublishedbyElsevierB.V.ThisisanopenaccessarticleundertheCCBYlicense(http://creativecommons.org/licenses/by/4.0/).Fundedby SCOAP3.
sionaremeasuresofthestrengthoflongitudinalfluctuationsand canbedeterminedbymeasuringthetwoparticlecorrelation func-tion [12]. Usingthe samemethodology,the event-by-event pseu-dorapidity distributions are also expanded in terms of Legendre polynomials [13].TheATLASCollaborationexpandedthe pseudora-piditydistributionsintermsofLegendrepolynomialsandobtained thecoefficientsbystudyingpseudorapiditycorrelations [14].
Inthepresentwork,theeventsare classifiedaccordingtothe asymmetrydeterminedfromthemeasurementofenergiesof neu-tron spectators on both sides of the collision [2]. The effect of asymmetryisinvestigatedbytakingtheratioofthemeasuredraw dN
/
dη
distributionsforeventsfromdifferentregionsofthe distri-butionofmeasuredasymmetry.Amajoradvantageofstudyingthis ratioisthecancellationof(i)systematicuncertainties and(ii)the effectsofshortrange correlations. Thefirst measurements ofthe effectofasymmetry ontherawdN/
dη
distributionsarereported here.Thepaperisorganisedasfollows:Sect.2providesan introduc-tion to the experimental setup andthe details of the data sam-ple.Section3discusses thecharacterisation ofthechangeinraw dN
/
dη
distributions for events classified in different asymmetry regions.Section 4 describesthe simulationsemployed to provide arelationbetweenthemeasuredasymmetryandtherapidity-shifty0 of the participant zone. The relation between the parameter
characterisingthechangeinrawdN
/
dη
distributionsisshownfor differentcentralities inSect.5,along withits relationto the esti-matedvaluesof y0.2. Experimentaldetailsanddatasample
TheanalysisusesdatafromPb–Pb collisioneventsat
√
sNN=
2.76TeV, recordedintheALICEexperimentin2010,witha min-imumbias trigger [15,16]. The data used inthe presentanalysis isrecordedintheneutronZeroDegreeCalorimeters (ZNs),theV0 detectors,theTimeProjectionChamber(TPC)andtheInner Track-ingSystem(ITS).Both ZNsandV0detectorsare oneithersideof theinteractionvertex,thoseinthedirectionofpositive pseudora-pidityaxisarereferredasV0AandZNAandthoseintheopposite directionarereferredasV0CandZNC.Adetaileddescriptionofthe ALICEdetectorsandtheirperformancecanbefoundelsewhere [17,
18].
Theeventasymmetryis estimatedusing theenergymeasured inthetwoZNssituated114metresawayfromthenominal inter-actionpoint(IP)oneitherside.TheZNsdetectonlyspectator neu-tronsthatarenotboundinnuclearfragments,sincethelatterare bentawaybythemagneticfieldoftheLHCseparationdipole.The ZNdetectionprobability forneutrons is 97.0%
±
0.2%(stat)±
3% (syst) [19]. The relative energyresolution of the1n peak at 1.38 TeVis21%fortheZNAand20% fortheZNC [19].Theproduction ofnuclearfragmentsincreaseswithcollisionimpactparameter de-grading the resolution on the number of participating nucleons. TheenergyintheZNsisagoodmeasureofthenumberof specta-torneutronsonlyforthemorecentralcollisions [18].Theanalysis islimited tothe top 35% mostcentral sample andemploys data from∼
2.
7 millionevents.The raw dN
/
dη
distributions in the region|
η
|
<
0.
9 are ob-tainedbyreconstructingthechargedparticletracksusingtheTPC and ITS. The requirements on the reconstructed tracks obtained using the measurements in these detectors are the same as in other earlieranalyses [15]. The measured amplitudes inthe V0A(
+
2.
8<
η
<
+
5.
1)
andV0C (−
3.
7<
η
<
−
1.
7) are used to es-timate the raw dN/
dη
distributions of charged particles in the forwardregions. Both V0AandV0Care scintillatorcounters,each withfour segments in pseudorapidity andeight segments in az-imuth.Therawdistributions measuredare termedasdN/
dη
dis-tributionsthroughoutthemanuscript.Inordertoensureauniform detectorperformance,thepresentanalysisuseseventswithz
po-sition (along the beam direction) of the interaction vertex, Vz,
within
±
5 cm of the IP in ALICE. The centrality of Pb–Pb col-lisionswas estimatedby twoindependentmethods.Oneestimate wasbasedonthechargedparticlemultiplicityreconstructedinthe TPCandtheother wasbasedon theamplitudesintheV0 detec-tors[20].3. Analysisandsystematicuncertainties
Inthepresentanalysis,changesintherawpseudorapidity dis-tribution ofchargedparticles areinvestigated fordifferentvalues ofmeasuredasymmetryoftheevent.Themethodofmeasurement oftheasymmetryandtheparameterscharacterisingthechangein dN
/
dη
distributionsarediscussedinthissection.3.1. Analysis
Anyeventasymmetryduetounequalnumberofnucleonsfrom the two participatingnucleimaymanifest itself inthe longitudi-naldistributions,i.e.dN
/
d y (or dN/
dη
)oftheproducedparticles because of a shift in the effectiveCM. Assuming that the rapid-itydistributions can bedescribed by a symmetricfunction about a mean y0 ( y0=
0.
0 for symmetricevents), the ratioofthedis-tributions forasymmetric and symmetric eventsmay be written as
(
dN/
d y)
asym(
dN/
d y)
sym=
f(
y−
y0)
f(
y)
∝
∞ n=0 cn(
y0)
yn (1)Foranyfunctionalformoftherapiditydistribution,thisratiomay beexpandedinaTaylorseries.Thecoefficientscn ofthedifferent
termsin theexpansiondepend onthe shapeandtheparameters oftherapiditydistribution [2].IntheALICEexperiment,the pseu-dorapiditiesoftheemittedparticleswere measured.Theeffectof arapidity-shift y0 onthepseudorapiditydistributionis discussed
inSect.4.2.
Theunequalnumberofparticipatingnucleonswillyielda non-zero y0 ofthe participant zone andwill causean asymmetry in
thenumberofspectators.Thisasymmetrycanprovideinformation aboutthemeanvaluesof y0 usingtheresponsematrixdiscussed
inSect.4.Theasymmetryofeacheventisestimatedbymeasuring theenergyintheZNsonbothsidesoftheinteractionvertex:EZNA
onthesidereferredtoastheA-side(
η
>
0)andEZNC onthesidereferred to astheC-side (
η
<
0).A smalldifference inthe mean andtherelativeenergyresolutionofthe1n peakat1.38TeVwas observed in theperformance ofthe two ZNs [19]. Foreach cen-tralityinterval,theenergydistributionineachZNisdividedbyits mean,andthe widthofthe EZNC/
EZNC distributionis scaledtothewidthofthecorrespondingdistributionusingEZNA.The
asym-metryinZNisdefinedas
α
ZN=
ε
ZNA−
ε
ZNCε
ZNA+
ε
ZNC(2) where
ε
ZNC(A)isadimensionlessquantityforeachevent,obtainedafterscalingthedistributionsofEZNC(A)asdescribedabove.
For the 15–20% centrality interval, Fig. 1 showsthe distribu-tionofthe asymmetry
α
ZN.Toinvestigatethesignificanceofthisdistribution,the contributionof theresolutionof ZNsto the res-olution of the asymmetry parameter
α
ZN is evaluated. For eachcentralityinterval,valuesofEZNC andEZNAaresimulatedforeach
Fig. 1. ThedistributionoftheasymmetryparameterαZNforthe15–20%centrality
interval.Thedistributionisdemarcatedintothreeregionsusing|αcut
ZN|.AGaussian
fittothedistributionyieldsawidthof0.13.
corresponding tothe average numberofneutrons andthe corre-sponding energy resolution. The average number of neutrons is estimatedby dividing the experimental distribution of energyin ZNby1.38TeV.Thesevaluesareusedtoobtain
α
ZNforeacheventandits distribution.The widthofthe distributioncorresponds to theintrinsicresolutionofthemeasuredparameter
α
ZN andvariesfrom0.023 to0.050 fromthemostperipheral (30–35%)selection to themostcentral (0–5%) selection.The observed widthof 0.13 ofthedistributionof
α
ZN reportedinFig.1isconsiderablylargerthan the resolution of
α
ZN (0.027 for the centralityintervalcor-responding to the data in the figure) and the increase in width maybeattributedtotheevent-by-eventfluctuationsinthe num-ber of neutrons detected in each ZN. To investigatethe effectof
α
ZN on the dN/
dη
distributions, the events are demarcated intothree regions of asymmetry by choosing a cut value
α
cut ZN. Theseregions correspond to (i)
α
ZN<
−
α
ZNcut (Region 1), (ii)α
ZN≥
α
ZNcut(Region 2)and(iii)
−
α
cutZN
≤
α
ZN<
α
ZNcut (Region3). Regions1and2 are referred to as the asymmetric regions and Region3 is re-ferredtoasthesymmetricregion.
Theeffectofthemeasuredasymmetry
α
ZNonthepseudorapid-itydistributionsisinvestigatedbystudyingtheratioofdN
/
dη
dis-tributionineventsfromtheasymmetricregion tothosefromthe symmetricregion.There aresmalldifferencesinthedistributions ofcentrality andvertexposition inevents ofdifferentregions of asymmetry.Itisnecessarytoensurethatanycorrelationbetween theratioofdN/
dη
andtheasymmetryisnotduetoasystematic effectofashiftintheinteractionvertex.Toeliminateanypossible systematicbiasonthemeasureddistributions,thedN/
dη
distribu-tionsare correctedbyweightfactorsobtainedbynormalisingthe numberofeventsinasymmetricandsymmetricregionsineach1% centralityintervalandeach1cmrangeofvertexpositions.For the 15–20% centrality interval, the distributions of these factorsinthetwocasescorrespondingtotheasymmetryregions 1 and 2 havea mean of 1.0and an rms of 0.05 and0.06 respec-tively.Theweightfactorsdonotshowanysystematicdependence onthepositionofthevertex.Thisisexpectedconsideringthelarge distancebetweentheZNsascomparedtovariationsinthevertex position.Thefactorsshowasystematicdependenceon1% central-itybinswithineach centralityinterval.The1% centralitybinwith thegreaternumberofparticipantstendstohavemoreasymmetric events,presumablytocompensateforthedecreaseintheeffective CMenergyduetothemotionoftheparticipantzone;theweight
factoris1.08forthemostcentral15–16%centralitybinandis0.94 forthe19–20%centralitybin.
The ratio of dN
/
dη
for events corresponding to different re-gions of asymmetry,asshowninFig. 1,is determined.For|
η
|
<
1
.
0, the ratio is obtained using dN/
dη
for tracks. For|
η
|
>
1.
0, the ratioshowninFig.2(a) and(b)isobtainedfromamplitudes measured inV0Aandthe oneshownin Fig.2(c)and(d)isfrom amplitudesmeasuredinV0C.ThesquaresinFig.2(a)and(c) rep-resent the ratio ofdN/
dη
inthe asymmetry Region1 to that in Region3(R13),andthestarsrepresentthecorresponding ratioin Region2toRegion3(R23).Thefilledcircles inFig.2(b)and(d) are obtained by (i) reflecting thedata points labelled R23 acrossη
=
0 and (ii) taking the averages of R13 and reflected-R23 for|
η
|
<
1.
0.Athirdorderpolynomial isfittedto thepointsandthe values of the coefficients cn along with theχ
2 are shown. ThepolynomialfittotheratioofdN
/
dη
distributionhasadominantly linearterm.Asmallresidualdetectoreffectisobservedwhen de-termining c1 using data measured in V0A andwhen using datameasured in V0C. In all subsequent discussion, the values of c1
quoted are the mean ofvalues obtainedfrom themeasurements inV0AandV0C.
Considering thatthe eventsamplescorresponding to different regions ofasymmetry areidenticalinall aspectsother thantheir valuesofmeasured
α
ZN,theobservationofnon-zerovaluesofc1can be attributedto the asymmetry.For a fixed centrality inter-val, c1 depends on the choice of
α
ZNcut. The analysis is repeatedfor differentvalues of
α
cutZN andthe dependenceof c1 on
α
ZNcut isshown in Fig. 3, for different centralities. For each centrality in-terval thecoefficient c1 has alineardependenceon
α
ZNcut andtheslope increaseswithdecreasingcentrality;c1 increasesforevents
corresponding to larger values of average event asymmetry. The rangeofvaluesof
α
cutZN wasguidedbytheresolutionandthewidth
of the distribution of
α
ZN, as mentioned in reference to Fig. 1.Increasing thevalue of
α
cutZN increasesthe mean
α
ZN foreventsfrom theasymmetric class (Region 1or Region2), andincreases theRMSof
α
ZNforeventsfromthesymmetricclass(Region3).3.2. Systematicuncertainties
The current method of analysisuses the ratio of two dN
/
dη
distributions from events divided on the basis of measurements inZNs,within acentralityinterval.Alleffects duetolimited effi-ciency,acceptanceorcontamination wouldcancelwhileobtaining the value oftheratio.The contributionsto thesystematic uncer-taintiesonc1 areestimatedduetothefollowingsources:
1. Centralityselection: the ratioofdN
/
dη
is obtainedfromthe measurements of tracks in the ITS+TPC at midrapidity and charge particlesignalamplitudesintheV0atforward rapidi-ties. For theformer, theeventcentrality isdetermined using themeasurementsintheV0andforthelatterusingthetrack multiplicityintheTPC.Theanalysisisrepeatedby interchang-ingthecentralitycriteriaandtheresultantchangeinthe val-uesofc1 fordifferentcentralityintervalsisintherange0.1%to3.6%.
2. V0AandV0C:thesystematicuncertaintyonthemeanvalueof
c1 isestimatedbyassumingauniformprobabilitydistribution
forthecorrectvalue ofc1 to lie betweenthe twovalues
ob-tainedusingthecharged-particle signalamplitudesmeasured intheV0AandtheV0C.The uncertaintyisintherange2.1% to4.6%anddoesnotdependonthecentralityvalue.
3. Vertexposition:theanalysisis repeatedforthe zpositionof theinteraction vertex
|
Vz|
≤
3.
0 cm.ForthemostcentralFig. 2. TheratioofdN/dηdistributionforeventsfromthedifferentregionsofαZN distributionofFig.1.ThedN/dηdistributionsareobtainedasdescribedinSect.2.
(a) Thesquare(star)symbolscorrespondingtoR13(R23)areobtainedbytakingtheratioofdN/dηofeventsfromRegion1(Region2)toRegion3.(b)Thedatapointsare obtainedafterreflectionacrossη=0 asdescribedinthetext.Thedatafor|η|>1.0 inpanels(a)and(b)arefrommeasurementsinV0Aandinpanels(c)and(d)arefrom measurementsinV0C.
Fig. 3. Thecoefficient
c1
characterisingthechangeindN/dηdistributionfor asym-metricregionsisshownfordifferentvaluesofαcutZN (αZNcutdemarcatesthe
asymmet-ricandsymmetricevents)foreachcentralityinterval.
centralityinterval,theresultschangeby3.3%andforallother centralityintervals,thechangesarelessthan1.3%.
4. Weightfactorsfornormalisation:theanalysisisalsorepeated withouttheweightfactorsmentionedinSect.3.1forthe cen-tralityandthevertexnormalisationinthenumberofevents. Thechangeintheresultsis4.9%inthemostcentralclassand lessthan1%forallothercentralityintervals.
Thetotalsystematicuncertaintyisobtainedbyaddingthefour uncertainties in quadrature. The resultant uncertainty is in the range2.3%to5.8%andisshownbythebandinFig.8.
4. Simulations
Thesimulationusedforobtaining arelationbetween rapidity-shift y0 andthe measurableasymmetry
α
ZN is described in thissection.Thissimulationhasthreecomponents:(i)aGlauberMonte Carlo to generate number of participants and spectator protons andneutrons, (ii) a function parametrised to fit the average loss ofspectator neutrons dueto spectatorfragmentation(the loss of spectatorneutrons ineacheventissmeared aroundthisaverage) and (iii)the response of the ZNto single neutrons. The simula-tion encompassing the above is referred to in the presentwork asTunedGlauberMonteCarlo(TGMC),andreproducestheenergy distributions in the ZNs. The effect of y0 on the pseudorapidity
distributionshasbeenestimatedusingadditionalsimulationsfora GaussiandN
/
d y andarealsodescribedinthissection.4.1. Asymmetryandrapidity-shift
TheGlauberMonteCarlomodel [21] usedinthepresentwork assumesa nucleon–nucleoninteractioncrosssection of64mb at
√
sNN
=
2.76TeV. The model yields the numberof participatingnucleonsintheoverlapzonefromeachofthecollidingnuclei.The rangeofimpactparametersforeach5%centralityintervalistaken fromourPb–Pbcentralitypaper [20].Foreach centralityinterval, 0.4millioneventsaregenerated.
Foreachgenerated event,thenumberofparticipatingprotons andneutronsisobtained,enablingadeterminationofthe rapidity-shift y0 andthevarious longitudinalasymmetries.IfAandBare
thenumberofspectators(spectatorneutrons)inthetwocolliding nuclei,theasymmetryisreferredtoas
α
spec(α
spec−neut).Fig.4(a)showsthe correspondencebetween y0 and
α
part.Figs. 4 (b)and(c) show the relation between y0 and
α
spec andα
spec−neutre-spectively [2].Thesefiguresshowthattherapidity-shifty0 canbe
estimatedbymeasuring
α
specorα
spec−neutinanyexperimentthatFig. 4. Rapidity-shift
y0
asafunctionofasymmetryin(a)numberofparticipants, (b)numberofspectators, (c)numberofspectatorneutronsand(d)energyinZNobtained usingTGMCasdescribedinthetext.Theresultsinallfourpanelsareshownforthe15–20%centralityinterval.Fig. 5. (a)DistributionofenergyinZNCineach5%centralityintervalforeventssimulatedusingTGMCandfortheexperimentaldata.Thepeakofthedistributionshiftsto smallervaluesof
EZNC
withincreasingcentrality.(b) DistributionoftheasymmetryparameterαZNinthesimulatedeventsandinexperimentaldatafordifferentcentralities.Thewidthofthedistributionincreaseswithincreasingcentrality.Forclarity,only5distributionsareshown.Thedistributionscorrespondingto20–25% and25–30%lie betweenthoseof15–20%and30–35%.
onthenumberofparticipantsworsenstheprecisionin determin-ing y0.Fig.4(d)showstherelationbetweeny0and
α
ZNobtainedinTGMC,asdescribedinthenextparagraph.
The Glauber MonteCarloistuned to describe the experimen-tal distributions of ZN energy. For each 1% centrality interval, the mean number of spectator neutrons (Ns) is obtained in the
GlauberMonteCarlo.FoldingtheZNresponseyieldsthesimulated valuesofmeanenergyasafunctionofcentrality.The experimen-tallymeasuredmeanenergyintheZNisalsodeterminedforeach 1%centralityinterval.Theratioofthemeasuredvalueofmean en-ergy to the simulated value of mean energy gives the fractional loss(f )ofneutronsduetospectatorfragmentsthatveerawaydue tothemagneticfield. Thevalueoff forthe0–5%centrality inter-valis0.19. Forallother centralities itvariesfrom0.40 for5–10% to0.55for30–35%centralityinterval.Afluctuationproportionalto thenumberofremaining neutrons(Ns
× (
1−
f)
)is incorporatedtoreproducetheexperimentaldistributionoftheenergydeposited intheZNshowninFig.5(a).ThepeakandtheRMSoftheenergy distributions matchwell.The fractional difference intheposition of the peak varies between3.7% for the 0–5% centrality interval and0.1% for the30–35% centrality interval. The fractional differ-enceinRMSforthemostcentralclassis8.6%andisintherange 1.0–2.0%forall other centralityintervals. Thedistributions ofthe asymmetryparameterfortheTGMCeventsandthemeasureddata foreachcentralityintervalareshowninFig.5(b).TheTGMC
con-tains information of y0 and
α
ZN for each event. A scatter plotbetween y0 and
α
ZNisshowninFig.4(d)forthe15–20%central-ityinterval.Thisconstitutestheresponsematrix.Foranymeasured value of
α
ZN,the distribution of y0 can be obtained. Anydiffer-ence in the experimental and TGMC distributions of
α
ZN can beaccountedforby scalingthe y0 distributionbythe ratioof
num-berofeventsindatatothenumberinTGMCas
f
(
y0,
α
ZNData)
=
f(
y0,
α
ZNTGMC)
NDataevents
NTGMCevents
,
(3)withData(TGMC)inthesuperscriptofnumberofevents,Nevents,
denoting the experimental data (TGMC events). For each of the three regions of asymmetry shown in Fig. 1, corresponding to a chosenvalueof
α
cutZN
=
0.
1,thedistributionofrapidity-shift y0ob-tained using the response matrix is shown in Fig. 6. It isworth mentioningthatthewidthofthedistributionofy0foreventsfrom
Region 3,corresponding to
−
α
cutZN
≤
α
ZN<
α
cutZN, is comparabletothewidthsofthecorresponding distributionsfromRegions1and 2.Theeffectofdifferenceinthevalueofthemeansofthey0
dis-tributionsisinvestigatedinthepresentwork.
4.2. Effectofrapidity-shiftonpseudorapiditydistributions
The effect ofa shift inthe rapidity distribution by y0 on the
measurablepseudorapiditydistribution(dN
/
dη
)isinvestigated us-ingsimulations.Foreachevent,therapidityofchargedparticlesisFig. 6. Thedistributionofrapidity-shifts forthe eventsfromthe threedifferent regionsofmeasuredasymmetryshowninFig.1.Determinationof
y0
usesthe dif-ferenceinnumberofnucleons.Forsmallvaluesofthisdifference,thechangesin valuesneary0
=0 arediscrete,andaresmearedintoacontinuousdistributionasy0increases.
generatedfromaGaussiandistributionofachosenwidth
σy
[22]. ThepseudorapidityisobtainedbyusingtheBlast-Wavemodelfit to the data for the transverse momentum distributions and the experimentally measured relativeyields ofpions, kaonsand pro-tons [23].Tosimulatetheeffectofdifferentwidthsoftheparent rapidity distribution fordifferent centralities, differentσ
y widthsarechosentoreproducethemeasured FWHM(FullWidthatHalf Maximum) of the pseudorapidity distribution [24]. Forthe most central(0–5%)class,a value3.86isusedforthewidthofthe ra-pidity distribution,anda value 4.00 isused forthe widthofthe leastcentralclassemployedinthisanalysis(30–35%).
Thedistributionof rapidity-shift y0,similar tothe oneshown
in Fig. 6, is obtained for each centrality interval and each
α
cut ZNusingTGMC.Fig.7(a)showsthe
y0asafunctionofα
cutZN fordif-ferentcentralities.Oneobservesalinearrelationbetweenthetwo quantities, showing that an asymmetry in the ZN measurement, arisingfromtheunequal numberofparticipatingnucleons, is re-latedtothe meanrapidity-shift
y0.The rapidity distributionoftheparticlesproducedineacheventisgeneratedassuminga Gaus-sianformcentred abouta y0,which isgeneratedrandomly from
the y0 distribution.Events witharapidity distributionshifted by
y0
=
0 yieldanasymmetricpseudorapiditydistribution.Athirdor-derpolynomialfunctionin
η
isfittedtotheratioofthesimulated dN/
dη
fortheasymmetricregiontothesimulateddN/
dη
forthe symmetricregion. Thevaluesofthe coefficientsintheexpansion dependupontherapidity-shift y0andtheparameterscharacteris-ingthedistribution [2].
The simulations described above were repeated for different valuesof
α
cutZN to obtainthepseudorapiditydistributions for
sym-metric and asymmetric regions. Fitting third order polynomial functions to the ratios of the simulated pseudorapidity distribu-tions determines the dependenceof c1 on
α
ZNcut.Fig. 7 (b)showsthat c1 hasalineardependenceon
α
cutZN foreachcentralityinter-val. The difference in the slopes for different centralities is due to differencesinthedistributions of y0 andtodifferencesin the
widthsoftherapiditydistributions.
Itisimportanttonotethattheparameterc1,characterisingthe
asymmetry inthe pseudorapidity distribution,showsa linear de-pendence on the parameter
α
cutZN in the event sample generated
usingTGMCandsimulationsforaGaussiandN
/
d y,akintothe de-pendenceoftheestimatedvalueofrapidity-shift y0 forthesamesampleofevents.
5. Results
The longitudinalasymmetry ina heavy-ioncollision has been estimatedfromthedifference intheenergyofthespectator neu-tronson both sidesofthe collisionvertex. The effectof the lon-gitudinal asymmetry is observed in the ratioof dN
/
dη
distribu-tions corresponding to differentasymmetries. The linear term in a polynomial fitto thedistribution ofthe ratiois dominant, and ischaracterisedbyitscoefficientc1.Thecentralitydependenceofthe coefficient c1 for
α
ZNcut=
0.
1 is shown in Fig. 8. It is worthemphasising thatthevaluesofc1 andhenceits centrality
depen-dence are affected by (i) the distribution of rapidity-shift y0 for
each centralityinterval, (ii) the chosen value of
α
cutZN, as seen in
Fig.7and(iii) the shapeorthewidthofthe parentrapidity dis-tributionforeachcentrality.Fig.8alsoshowstheresultsobtained usingsimulationsasdescribed inSec. 4.2for
α
cutZN
=
0.
1.Thesys-tematicuncertaintyonthesimulatedeventsampleisestimatedby (i) varying the resolution ofZNs from 20% to 30%, (ii) assuming all charged particles are pions and(iii) varying thewidth of the parentrapiditydistributionwithintherangecorresponding tothe uncertainties onFWHMquoted inRef. [24]. Thesimulatedevents showagoodagreementwiththeexperimentaldataproviding
cre-Fig. 7. (a)Theestimatedmeanvalueofrapidity-shifty0fortheasymmetricregioncharacterisedbydifferentvaluesofαcut
ZN foreachcentralityinterval.(b)Thecoefficient c1characterisingthechangeinthepseudorapiditydistributionsfordifferentvaluesofαcut
ZN,foreachcentralityinterval.TheseresultsareobtainedusingTGMCandsimulated
Fig. 8. Themeanvaluesofthecoefficient
c1
areshownasfilledcirclesfordifferentcentralities.ThesecorrespondtotheratioofdN/dηdistributionsofpopulationsofevents demarcatedbyαcutZN =0.1.Thesquaresshowthecorrespondingvaluesfromsimulations,andcorrespondtoαcutZN=0.1 inFig.7,fordifferentcentralities.Thesystematic
uncertaintiesareshownasbands.
Fig. 9. Foreachsetofeventscharacterisedbyαcut
ZN,themeasuredvaluesof
coef-ficient
c1
asafunctionofestimatedvaluesofmeanrapidity-shiftobtainedusing TGMCasdescribedinthetext.Theresultsareshownfordifferentcentralities.The uncertaintiesfory0shownarestatisticalandwithinitssymbolsize.Thelinesare linearfitspassingthroughtheorigin.dencetotheassumptions ofthesimulation,inparticularthatthe asymmetryinthedistributionsarisesfromtheshiftofrapidity of theparticipantzone.
There are two quantities fromindependent measurements for eachselection ofasymmetricevents.Theseare (i) c1,the
param-eter characterising the effect of asymmetry in the dN
/
dη
distri-butions andshowninFig.3and(ii) themeanrapidity-shift y0obtainedfromthemeasured asymmetry,filteredthrough the cor-responding responsematrix (Fig. 4 (d)), andshown inFig. 7 (a). Therelationbetweenc1 and
y0isshowninFig.9.Theparame-terc1 showsalineardependenceon
y0foreachcentrality.Thedifferenceintheslopesindicatesthesensitivityofthelongitudinal asymmetry tothedetails oftherapidity distribution.Fora Gaus-sianrapiditydistributionthecorrespondingparameterc1wouldbe
relatedtotherapidity-shiftasc1
=
σy0y2
[2],implyingthattheslope isinverselyproportionaltothesquareofthewidthofthe distribu-tion.Theobservationofan increaseintheslopewithanincrease in the centrality in the present data indicates a decrease in the widthofthepseudorapiditydistributionwithincreasingcentrality. Such a decrease in the width of the pseudorapidity distribution withincreasingcentralityhasbeenobservedindependentlyby
fit-tingthe pseudorapiditydistributions ina broadrangeof pseudo-rapidity [24].
6. Conclusions
The present analysis demonstratesthe existence ofa longitu-dinalasymmetry inthe collisionofidenticalnucleidueto fluctu-ationsin thenumberofparticipants fromeachcollidingnucleus. This asymmetry has beenmeasured in the ZNs inthe ALICE ex-periment (Fig. 1), andaffects thepseudorapidity distributions, as demonstratedbytakingtheratioofdistributionofeventsfromthe asymmetric region tothe corresponding onefromthe symmetric region(Fig.2).Theeffectcanbecharacterisedbythecoefficientof thelinearterminthepolynomialexpansionoftheratio.The coef-ficientsshowalineardependenceon
α
cutZN,aparametertoclassify
the events into symmetric and asymmetric regions (Fig. 3). Dif-ferent values of
α
cutZN correspond to different valuesof the mean
rapidityshift
y0(Fig.7(a)).Theparameterdescribingthechangeinthepseudorapiditydistributions(c1)hasasimpleexplanationin
the rapidity-shift
y0of theparticipantzone (Fig.9). Theanaly-sisconfirms thatthelongitudinaldistributions areaffectedbythe rapidity-shiftoftheparticipantzonewithrespecttothenucleon– nucleonCMframe.Theresultsprovidesupporttotherelevanceof numberofnucleons affectingtheproductionofchargedparticles, evenatsuchhighenergies.
The longitudinal asymmetry is a good variable to classify the eventsandprovidesinformationontheinitialstateofeach event. Asystematicstudyoftheeffectsoflongitudinalasymmetryon dif-ferentobservables, e.g.theoddharmonicsofanisotropicflow, the forward-backwardcorrelations, thesourcesizes, inheavy-ion col-lisions may reveal other characteristics ofthe initial state andof particleproductionphenomena.
Acknowledgements
The ALICECollaboration would like to thank all its engineers andtechniciansfortheirinvaluablecontributionstothe construc-tion of the experiment and the CERN accelerator teams for the outstanding performance of the LHC complex. The ALICE Collab-oration gratefully acknowledges the resources and support pro-videdbyallGridcentresandtheWorldwideLHCComputingGrid (WLCG) collaboration. The ALICE Collaboration acknowledges the following fundingagenciesfortheir supportin buildingand run-ningthe ALICEdetector:A.I. AlikhanyanNationalScience Labora-tory(YerevanPhysicsInstitute)Foundation (ANSL),State Commit-teeofScienceandWorldFederationofScientists(WFS),Armenia;
AustrianAcademy ofSciences andNationalstiftung fürForschung, Technologie und Entwicklung, Austria; Ministry of Communica-tions and High Technologies, National Nuclear Research Center, Azerbaijan; Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), Universidade Federal do Rio Grande do Sul (UFRGS), Financiadora de Estudos e 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-cation andSport and Croatian Science Foundation, Croatia; Min-istryofEducation,YouthandSportsoftheCzechRepublic, Czech Republic; The Danish Council for Independent Research | Natu-ral 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 des Particules (IN2P3)andCentre National de laRecherche Scientifique (CNRS), France; Bundesministerium für Bildung, Wissenschaft, Forschung und Technologie (BMBF) and GSI Helmholtzzentrum für Schw-erionenforschung GmbH, Germany; General Secretariat for Re-search andTechnology,Ministry ofEducation, Researchand Reli-gions,Greece;NationalResearch,DevelopmentandInnovation Of-fice,Hungary;DepartmentofAtomicEnergy,GovernmentofIndia (DAE),DepartmentofScienceandTechnology,GovernmentofIndia (DST),University Grants Commission, Governmentof India(UGC) andCouncil ofScientificandIndustrialResearch(CSIR), India; In-donesian Institute of Science, Indonesia; Centro Fermi – Museo StoricodellaFisicaeCentroStudieRicercheEnricoFermiand Isti-tutoNazionalediFisicaNucleare(INFN),Italy;Institutefor Innova-tiveScienceandTechnology,NagasakiInstituteofAppliedScience (IIST),Japan Societyforthe PromotionofScience(JSPS)KAKENHI andJapanese Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan; Consejo Nacional de Ciencia (CONA-CYT)yTecnología,throughFondodeCooperaciónInternacionalen CienciayTecnología (FONCICYT)andDirección Generalde Asun-tosdelPersonalAcademico(DGAPA),Mexico;Nederlandse Organ-isatievoorWetenschappelijk Onderzoek(NWO),Netherlands; The ResearchCouncil ofNorway, Norway;CommissiononScienceand TechnologyforSustainableDevelopmentintheSouth(COMSATS), Pakistan;PontificiaUniversidadCatólicadelPerú,Peru;Ministryof ScienceandHigherEducationandNationalScienceCentre,Poland; KoreaInstituteofScienceandTechnologyInformationandNational ResearchFoundationofKorea(NRF),RepublicofKorea;Ministryof EducationandScientificResearch,Institute ofAtomicPhysicsand Romanian National Agency for Science, Technology and Innova-tion,Romania;JointInstituteforNuclear Research(JINR),Ministry ofEducation andScience of the Russian FederationandNational Research Centre Kurchatov Institute, Russia; Ministry of Educa-tion,Science,ResearchandSportoftheSlovakRepublic, Slovakia; NationalResearch Foundation of SouthAfrica, South Africa; Cen-tro de Aplicaciones Tecnológicas y Desarrollo Nuclear (CEADEN), Cubaenergía,Cuba,Ministeriode CienciaeInnovacion andCentro de Investigaciones Energéticas, Medioambientales y Tecnológicas (CIEMAT),Spain; Swedish Research Council (VR) and Knut& Al-iceWallenbergFoundation(KAW),Sweden;EuropeanOrganization forNuclear Research, Switzerland; NationalScience and Technol-ogyDevelopment Agency (NSDTA), Suranaree University of Tech-nology(SUT)andOfficeoftheHigherEducationCommissionunder NRUprojectofThailand,Thailand;TurkishAtomic EnergyAgency (TAEK),Turkey;NationalAcademyofSciencesofUkraine,Ukraine; ScienceandTechnologyFacilitiesCouncil(STFC),UnitedKingdom; NationalScienceFoundationoftheUnitedStatesofAmerica(NSF)
andUnitedStatesDepartmentofEnergy,OfficeofNuclearPhysics (DOENP),UnitedStatesofAmerica.
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ALICECollaboration