ATLAS-CONF-2013-096 11September2013
ATLAS NOTE
ATLAS-CONF-2013-096
September 11, 2013
Measurement of the centrality dependence of the charged particle pseudorapidity distribution in proton-lead collisions
at √
s
NN= 5.02 TeV with the ATLAS detector
The ATLAS Collaboration
Abstract
The ATLAS experiment at the LHC has measured the centrality dependence of charged particle pseudorapidity distributions,
dNch/dη, in p+Pb collisions at a nucleon-nucleon centre-of-mass energy of
√sNN =
5.02 TeV. Charged particles were reconstructed over
|η|<
2.7 using the ATLAS pixel detector. The proton-lead collision centrality was character- ized by the total transverse energy measured over the pseudorapidity interval 3.2
< η <4.9 in the direction of the lead beam. The
dNch/dηdistributions are found to vary strongly with centrality, with an increasing asymmetry between the proton-going and Pb-going directions as the collisions become more central. Three different calculations of the number of partic- ipants,
Npart, have been carried out using a standard Glauber model as well as two Glauber- Gribov extensions. Charged particle multiplicities per participant pair,
dNch/dη/(hNparti/2),are found to vary differently with
Npartfor these three models, pointing to the importance of the fluctuating nature of nucleon-nucleon collisions in the modeling of the initial state of p+Pb collisions.
c
Copyright 2013 CERN for the benefit of the ATLAS Collaboration.
Reproduction of this article or parts of it is allowed as specified in the CC-BY-3.0 license.
1 Introduction
Proton or deuteron-nucleus (
p/d+A) collisions at the LHC and RHIC provide an opportunity to study the physics of the initial state of ultra-relativistic heavy ion (A+A) collisions without the obscuring effects of thermalization and collective evolution thought to play an important role [1] in A+A collisions. In particular,
p/d+A measurements can shed insight on the e
ffect of an extended nuclear target on the dynamics of soft and hard scattering processes and subsequent particle production. Charged particle multiplicity and pseudorapidity distributions are among the most basic experimental probes of particle production. Historically, measurements of charged particle pseudorapidity distributions have provided important insight on soft particle production dynamics in
p+A collisions both at fixed target [2, 3, 4, 5]
and at collider [6, 7] energies and have provided essential tests of models for inclusive soft hadron production.
More detailed insight can be provided by measurements of the charged particle multiplicities as a function of “centrality”, an experimental quantity that provides an indirect constraint on the
p/d+A col-lision geometry. Previous measurements at fixed-target energies have relied on the number of “grey”
or “knocked-out” protons [8]. Measurements in
d+Au collisions at RHIC have relied on experimental measures of particle multiplicity at large pseudorapidity, either symmetric around mid-rapidity [9] or in the gold fragmentation direction [10]. These measurements have shown that the rapidity-integrated particle multiplicity in
d+Au collisions scales with the number of inelastically interacting, or “partici- pating”, nucleons,
Npart. This scaling behaviour has been interpreted as the result of coherent multiple soft interactions of the projectile nucleon in the target nucleus, and is known as the wounded-nucleon model [11]. Previous measurements of the centrality dependence of charged hadron pseudorapidity dis- tributions (dN
ch/dη) in p/d+A collisions [12, 6] show little growth or even a reduction in yield of veryforward particles and a strong increase in the yield of backward particles with increasing
Npart. Here
“forward” (backward) refers to particles with pseudorapidities closer to the proton (nucleus) rapidity than the nucleus (proton) rapidity. This centrality dependence has been explained using well-known phenomenology of soft hadron production [13].
There exist alternative descriptions of the centrality dependence of
d+Au results at RHIC [14, 15] and the inclusive
p+Pb measurement at the LHC ([15, 16] and references therein) based on parton saturationmodels. A measurement of the centrality dependence of
dNch/dηdistributions will provide an essential test of such models of soft hadron production at the LHC. Such tests have become more urgent given the observation of two-particle [17, 18, 19, 20] and multi-particle [21, 20] correlations in the final state of
p+Pb collisions at the LHC. These correlations are currently interpreted as resulting from either initial-state saturation e
ffects [22, 23, 15] or from collective dynamics of the final state [24, 25, 26, 27, 28]. For either interpretation, information on the centrality dependence of
dNch/dηcan provide important input for determining the mechanism responsible for these structures.
The LHC provided its first proton-nucleus collisions in a short
p+Pb pilot run at
√sNN=
5.02 TeV in September 2012. Over the several-hour run ATLAS collected an event sample corresponding to an estimated integrated luminosity of approximately 1
µb−1. This note presents the measurement of the centrality dependence of
dNch/dηover
−2.7< η <2.7 in
p+Pb collisions at
√sNN =
5.02 TeV, obtained from the data collected during the pilot run. Charged particles were detected in the ATLAS pixel detector and were reconstructed using a two-point tracklet algorithm similar to that used for the Pb+Pb multiplic- ity measurement [29]. Results are presented for several intervals in collision centrality characterised by the total transverse energy measured in the section of ATLAS forward calorimeter spanning the pseudo- rapidity interval 3.2
< η <4.9. A standard Glauber model [30] and its Glauber-Gribov extension [31, 32]
are used to estimate
hNpartifor each centrality interval, allowing a measurement of the
Npartdependence
of the charged particle multiplicity.
2 Experimental setup
During the pilot run the LHC was configured with a 4 TeV proton beam and a 1.57 TeV per-nucleon Pb beam that together produced collisions with a nucleon–nucleon centre-of-mass energy of
√sNN =
5.02 TeV, with a longitudinal boost corresponding to a rapidity shift of
−0.465 relative to the ATLASlaboratory frame
1. In this configuration, the proton had negative rapidity and the lead nucleus had positive rapidity. For the remainder of this note the terms Pb-going and proton-going will be used to refer to positive and negative pseudorapidities, respectively.
The analysis presented in this note was performed using the ATLAS inner detector (ID), calorime- ters, minimum-bias trigger scintillators (MBTS), and the trigger and data acquisition systems [33]. For the nominal collision vertex position, the ATLAS inner detector measures charged particles within the pseudorapidity range
|η|<2.5 using a combination of silicon pixel detectors, silicon microstrip detectors (SCT), and a straw-tube transition-radiation tracker (TRT), all immersed in a 2 T axial magnetic field. In order to measure charged particles down to
pT ∼100 MeV with good efficiency, and thus permit a more precise extrapolation over the full
pTrange, the charged particle pseudorapidity density measurement was performed using only the pixel detector [34]. The pixel detector is divided into “barrel” and “end- cap” sections. The barrel section consists of three layers of staves, inclined at an angle of 20
◦, at radii of 50.5, 88.5, and 122.5 mm from the nominal beam axis, and extending
±400.5 mm from the nominalcentre of the detector in the
zdirection. The endcap consists of three disks placed symmetrically on each side of the interaction region at
zlocations of
±493,±578 and±648 mm from the nominal centre of thedetector region. The typical pixel size is 50
µm×400
µm in theφ−zplane. For events with
zvtx=0, the barrel section of pixel detector measures charged particles up to
|η| <2.2. The endcap sections extend the detector coverage, spanning the pseudorapidity interval 1.6
<|η|<2.7.
The ATLAS forward calorimeter (FCal) consists of two sections, labeled A and C, that cover 3.2
<|η| <
4.9. The FCal modules are composed of tungsten and copper absorbers with liquid argon as the active medium, which together provide 10 interaction lengths of material. The MBTS is sensitive to charged particles in the range 2.1
< |η| <3.9 using two hodoscopes, each of which is subdivided into 16 counters positioned at
z = ±3.6 m. Minimum-bias p+Pb collisions were selected by a trigger that required a signal in at least two MBTS counters.
3 Event selection
In the o
ffline analysis, charged particle tracks and collision vertices were reconstructed from clusters in the pixel detector and the SCT using an algorithm optimized for
p+pminimum-bias measurements [35].
Separately, “pixel tracks” were reconstructed using only pixel clusters. The
p+Pb events selected for thisanalysis were required to have a collision vertex satisfying
|zvtx| <175 mm, at least one hit in each side of the MBTS, and a difference between the times measured in the two MBTS hodoscopes of less than 10 ns. Events containing multiple
p+Pb collisions (pileup) were suppressed by rejecting events with tworeconstructed vertices that are separated in
zby more than 15 mm. The residual pileup fraction has been estimated to be 10
−4[21].
The
p+Pb inelastic cross-section has significant contributions from diffractive and electromagneticprocesses. The lead nucleus can excite the proton via incoherent di
ffractive, coherent di
ffractive, and electromagnetic processes, and the proton can quasi-di
ffractively excite nucleons in the nucleus. The
1The ATLAS reference system is a Cartesian right-handed coordinate system, with the nominal collision point at the origin.
The anti-clockwise beam direction defines the positivez-axis, while the positivex-axis is defined as pointing from the collision point to the centre of the LHC ring and the positivey-axis points upwards. The azimuthal angleφis measured around the beam axis, and the polar angleθis measured with respect to thez-axis. Pseudorapidity is defined asη=−ln (tan(θ/2)). All pseu- dorapidity values quoted in this latter are defined in laboratory coordinates. Rapidity is definedy=0.5 ln(E+pz)/(E−pz), whereEis the energy andpzis the longitudinal momentum.
different contributions to the excitation of the proton cannot be easily distinguished without large- acceptance forward detectors, including the zero degree calorimeters, which were not operational during the pilot run. To remove potentially significant contributions from electromagnetic processes, a rapidity gap analysis similar to that applied in a measurement of diffraction in 7 TeV proton-proton collisions [36]
was applied to the
p+Pb data. The full pseudorapidity coverage of the detector,
−4.9< η <4.9, was di- vided into
∆η=0.2 intervals, and each interval containing one or more reconstructed tracks or calorime- ter clusters with
pT >200 MeV was considered as occupied. Then the edge-gaps on each side of the detector were calculated as the distance in pseudorapidity between the detector edge (-4.9 or 4.9) and the nearest occupied interval. Events with large edge-gaps on the Pb-going side of the detector,
∆ηPbgap &2, typically result from electromagnetic or diffractive excitation of the proton. These two contributions cannot be easily distinguished, and both of them have no significant signal in Pb-going FCal, so they were both excluded from this analysis. No requirement was imposed on gaps on the proton-going side.
The gap requirement removed a fraction,
fgap =6%, of the events passing the vertex and MBTS cuts and yielded a total of 2131219 events for use in this analysis.
4 Monte Carlo data sets
The response of the ATLAS detector and the performance of reconstruction algorithms were evaluated using 1 million minimum-bias 5.02 TeV Monte Carlo
p+Pb events produced by version 1.38b of the HIJING event generator [37] with diffractive processes disabled, and fully simulated using GEANT4 [38, 39]. The momentum four-vector of each generated particle was longitudinally boosted by a rapidity of -0.465 to match the LHC
p+Pb beam conditions. The simulated Monte Carlo events were then digitized using data conditions appropriate to the pilot
p+Pb run and fully reconstructed using the same algorithmsthat were applied to the experimental data. Separate PYTHIA6 [40] and PYTHIA8
p+psamples were generated at
√s =
5.02 TeV with particle kinematics boosted to match the
p+Pb beam conditions.
Separate samples of 5.02 TeV minimum-bias, single diffractive, and non-diffractive
p+pcollisions with 1 million events each were produced using PYTHIA6 (version 6.425, AMBT2 tune [41], CTEQ6L1 PDFs) and PYTHIA8 (version 8.150, 4C tune [42], MSTW2008LO PDFs) and fully simulated in the same manner as the
p+Pb events.5 Centrality selection
For Pb+Pb collisions, ATLAS uses the total transverse energy,
PET, measured in the two forward calorimeter sections to characterize the collision centrality [43]. However, the intrinsic asymmetry of
p+Pb collisions and the rapidity shift of the centre-of-mass causes a di
fferent response of the two sides of the ATLAS calorimeter to soft particle production. For
p+Pb collisions included in this analysis,Fig. 1 shows the correlation between the summed transverse energies measured in the proton-going (−4.9
< η < −3.2) and Pb-going (3.2 < η <4.9) directions,
ΣETpand
ΣEPbT, respectively. The trans- verse energies shown in the figure and used in this analysis were evaluated at the electromagnetic energy scale and have not been corrected for hadronic response. Figure 1 shows that
ΣEpTrapidly saturates with increasing
ΣEPbTfor
ΣETPb&30 GeV, indicating that
ΣETpis less sensitive than
ΣEPbTto the increased par- ticle production expected to be associated with multiple interactions of the proton in the target nucleus in central collisions. Thus,
ΣEPbTis used to characterize
p+Pb collision centrality for the analysis presentedhere.
The distribution of
ΣETPbfor events passing the applied
p+Pb analysis selections is shown in Fig. 2.
Following standard techniques [29], centrality intervals were defined in terms of percentiles of the
ΣEPbTdistribution after accounting for an estimated ine
fficiency (see Appendix A) for inelastic
p+Pb events to
[GeV]
Pb
ET
Σ
0 50 100 150 200
[GeV]p TEΣ
0 20 40 60 80 100
1 10 102
103
104
ATLAS Preliminary
b-1
µ = 1 Lint
= 5.02 TeV, sNN
+Pb, p
Figure 1: Distribution of proton-going (
ΣEpT) versus Pb-going (
ΣEPbT) forward calorimeter total trans- verse energy (see text) for
p+Pb collisions included in this analysis.pass the applied event selections of 1
−εinel =2
±2%. The following centrality intervals were used in this analysis: 0–1%, 1–5%, 5–10%, 10–20%, 20–30%, 30–40%, 40–60%, 60–90%. The
ΣEPbTranges corresponding to these centrality intervals are indicated by the alternating filled and unfilled regions in Fig. 2. The most peripheral 90–100% collisions were excluded from the analysis due to uncertainties
[GeV]
Pb
ET
Σ
0 100 200
]-1 [GeVPb TEΣ/dN devtN1/
10-6
10-5
10-4
10-3
10-2
ATLAS Preliminary
b-1
µ = 1 Lint
= 5.02 TeV, sNN
p+Pb,
Figure 2: Distribution of
ΣETPbvalues for events satisfying all analysis cuts including the Pb-going rapidity gap exclusion (see text). The alternating shaded and unshaded bands indicate centrality intervals, from right to left, 0–1%, 1–5%, 5–10%, 10–20%, 20–30%, 30–40%, 40–60%, 60–90% and 90–100%
(not used in this analysis).
regarding their composition and their reconstruction efficiency.
Following standard procedures, a Glauber analysis [30] was applied to estimate
hNpartifor each of the centrality intervals used in this analysis. A detailed description of that analysis, which uses the convolution properties of gamma distributions to describe the measured
ΣEPbTdistribution, is provided in Appendix A. Only a summary of the method is given here.
A Glauber Monte Carlo program [44] was used to simulate the geometry of inelastic
p+Pb collisions
and calculate the probability distribution for
Npart,
P(Npart). The simulations used a Woods-Saxon nu- clear density distribution and an inelastic nucleon-nucleon cross-section of
σNN=70
±5 mb. Separately, PYTHIA8 simulations of
p+pevents were used to obtain a detector-level nucleon-nucleon
ΣETPbdistri- bution, to be used as input to the Glauber model. This was fit to a gamma distribution. Then, an extension of the wounded-nucleon (WN) model that included non-linear dependence of
ΣEPbTon
Npartwas used to define
Npart-dependent gamma distributions for
ΣETPb, with the constraint that the distributions reduce to the PYTHIA8 distribution for
Npart =2. The gamma distributions were summed over
Npartwith a
P(Npart) weighting to produce a hypothetical
ΣETPbdistribution. That distribution was fit to the measured
ΣEPbTdistribution shown in Fig. 2 with the parameters of the extended WN model allowed to vary freely.
From the results of the fit, the distribution of
Npartvalues and the corresponding
hNparti, were calculatedfor each centrality interval.
In addition to the usual Glauber Monte Carlo simulation, an extension of the Glauber model was also used to calculate
P(Npart). This takes into account event-to-event fluctuations in the nucleon-nucleon cross-section,
σNN, [31, 32], and is referred to in the rest of this note as “Glauber-Gribov.” Two sets of Glauber-Gribov
Npartresults were obtained for two di
fferent values of the parameter,
Ω, that determines the width of the assumed Gaussian fluctuations in
σNN. For the purposes of this analysis, both values
Ω =0.55 and
Ω =1.01 are considered plausible and results from both parameters are studied to evaluate the potential physics implications of the Glauber-Gribov extension.
The
hNpartivalues calculated using the above-described procedure are shown in Fig. 3 for the three di
fferent
P(Npart) simulations. The error bars in the figure show asymmetric systematic uncertainties determined by varying di
fferent assumptions of the Glauber
/Glauber-Gribov modeling including
σNN,
εinel, the form of the WN extension, and the properties of the nuclear density distribution. For central collisions, the
hNpartiuncertainties are dominated by the uncertainty in the WN model extension and
σNN. For more peripheral collisions the uncertainty on
εinelalso makes a significant contribution.
The differences in the
hNpartivalues between the Glauber and the two Glauber-Gribov models results from the di
fferent shapes of the
p+Pb
Npartdistributions in these models. The narrower
Npartdistribution in the Glauber model requires larger fluctuations in
ΣETPbat fixed
Npartto describe the tail of the
ΣEPbTdistribution. In contrast, the broader
Npartdistributions associated with the Glauber-Gribov models re- quire smaller intrinsic fluctuations in
ΣEPbTat fixed
Npart. As a result, the
hNparticorresponding to events with large
ΣETPbis systematically larger for the Glauber-Gribov models and is largest for
Ω =1.01.
6 Measurement of charged particle multiplicity
As described previously, the multiplicity measurement was performed using only the pixel detector to maximize the efficiency for reconstructing charged particles with low transverse momenta. Two ap- proaches are used in this analysis. The first is the two-point tracklet method used widely in heavy ion collision experiments [29, 45, 46]. Two variants of this method have been implemented in this analysis to produce the
dNch/dηresult and to estimate the systematic uncertainties, as described below. The second is the use of pixel tracks, described in Section 3. It has a smaller acceptance, but provides measurements of the particle
pT. The
dNch/dηmeasured using pixel tracks is used as a cross-check to that measured using the two-point tracklets.
In the two-point tracklet algorithm, the event vertex and clusters on an inner pixel layer define a
search region for clusters in the outer layers. The algorithm uses all clusters, except for those which
1) have low energy deposits inconsistent with minimum-ionizing particles originating from the primary
vertex, 2) are duplicate clusters resulting from the overlap of the pixel modules or 3) include a small set
of pixels at the centre of the pixel modules that share readout channels [34]. Clusters in the same layer
of the pixel detector were considered as one if they were separated by less than a certain distance. Such
clusters have a high probability to be correlated to the same particle.
centrality
60-90%40-60%30-40%20-30%10-20% 5-10% 1-5% 0-1% 0-90%
〉
partN 〈
0 5 10 15 20 25 30
Simulation Preliminary ATLAS
= 5.02 TeV sNN
p+Pb, b-1
µ = 1 Lint
Glauber
= 0.55 Ω Glauber-Gribov
= 1.01 Ω Glauber-Gribov
Figure 3:
hNpartivalues resulting from fits to the measured
ΣEPbTdistribution (see Fig. 2) using Glauber and Glauber-Gribov
Npartdistributions. The error bars indicate asymmetric systematic uncertainties (see Appendix A).
The pseudorapidity and azimuthal angle of the cluster in the innermost layer (η, φ) and the difference between those parameters for the cluster in two layers (∆
η,∆φ) are taken as the parameters of the re-constructed tracklet. The
∆ηof a tracklet is largely determined by the multiple scattering of the incident particles in the material of the beam pipe and detector. This effect plays a less significant role in the
∆φof a tracklet, which is driven primarily by the bending of charged particles in the magnetic field, and hence one expects
∆φto be larger. The tracklet selection cuts are:
|∆η|<
0.015,
|∆φ|<0.1,
|∆η|<|∆φ|.
(1)
Keeping tracklets with
|∆φ| <0.1 corresponds to accepting particles with
pT &100 MeV. The depen- dence of the multiple scattering on particle momentum suggests the requirement on the relation between
∆η
and
∆φof the tracklet given in the second row of Eq. 1.
The Monte Carlo (MC) simulation for the
dNch/dηanalysis is based on the HIJING event generator, which is described in Section 4. Generator (truth) level particles are defined as primary particles if they originate directly from the collision or result from decays of particles with
cτ <1 mm. All other particles are defined as secondaries. Tracklets are classified as primary or secondary depending on whether the as- sociated truth particle is primary or secondary. Tracklets can also be formed from the random association of hits produced by unrelated particles, or hits in the detector which are not associated to any generated particle. These tracklets are referred to as “fakes”.
The contribution of fake tracklets is relatively di
fficult to model in the simulation, because of the a priori unknown contributions of multiple sources, such as noise clusters or very low energy particles.
To address this problem, the tracklet algorithm is used in two di
fferent implementations referred to as
“Method 1” and “Method 2”. In Method 1, at most one tracklet is reconstructed for a given cluster on the first pixel layer. If multiple clusters on the second pixel layer fall within the search region, the resulting tracklets are merged into a single tracklet. This approach limits, but does not eliminate, the presence of fake tracklets. Method 2 reconstructs tracklets for all combinations of clusters in only two pixel layers.
To account for the fake tracklets arising from random combinations of clusters, the same analysis is
performed after inverting the
xand
ypositions of all clusters on the second layer with respect to the
primary vertex (x
− xvtx, y−yvtx)
→(−(x
− xvtx),
−(y−yvtx)). The tracklet yield from this “flipped”
analysis is then subtracted from the original tracklet yield to obtain an estimated yield of true tracklets
N2p,
N2p
(η)
=N2pev(η)
−N2pfl(η), (2) where
N2pevrepresents the yield of two-point tracklets using Method 2 and
N2pflrepresents the yield ob- tained by flipping the clusters in the second pixel layer.
Distributions of
∆ηand
∆φof reconstructed tracklets for data and simulated events are shown in Fig. 4 for the barrel (upper) and endcap (lower) parts of the pixel detector. The data is indicated by
η
-0.01 0 0.01 ∆
)η∆ / d(raw tracklet dNevt1/N
102
103
104
Barrel data MC primary MC secondary MC fakes Preliminary
ATLAS b-1
µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
φ
-0.1 0 0.1 ∆
)φ∆ / d(raw tracklet dNevt1/N
10 102
103 Barreldata
MC primary MC secondary MC fakes Preliminary
ATLAS b-1
µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
η
-0.01 0 0.01 ∆
)η∆ / d(raw tracklet dNevt1/N
10 102
103
Endcaps data MC primary MC secondary MC fakes Preliminary
ATLAS b-1
µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
φ
-0.1 0 0.1 ∆
)φ∆ / d(raw tracklet dNevt1/N
1 10 102
Endcaps data MC primary MC secondary MC fakes Preliminary
ATLAS b-1
µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
Figure 4:
∆η(left) and
∆φ(right) for the tracklets reconstructed with Method 1 measured in the data (circles) and MC (histograms) in
p+Pb collisions at √sNN =
5.02 TeV. The lowest (green) histogram are the fake tracklets, the middle region (cyan) are secondary particles, and the upper (yellow) region is the contribution of the primary particles.
black circles and simulated events are shown with filled histograms. The simulation results show the three contributions from primary (yellow), secondary (cyan) and fake (green) tracklets. The selection criteria specified by Eq. 1 are shown in Fig. 4 with vertical lines and applied in
∆φfor
∆ηplots and vice versa. Outside those lines, the contributions of secondary and fake tracklets are more di
fficult to control, especially in the endcap region.
The left panel of Fig. 5 shows the distributions of the number of tracklets reconstructed with Method 2
and satisfying the criteria of Eq. 1 as a function of pseudorapidity in the 0-10% centrality interval for data
(markers) and for the MC (lines). The results of flipped reconstruction are also shown in the plot. Data
and MC distributions are similar but not identical, reflecting the fact that HIJING does not reproduce
-3 -2 -1 0 1 2 η3 η / draw tracklet dNevt1/N
0 5 10 15 20 25 30 35 40
45 ATLAS Preliminary b-1
µ
int= 1 p+Pb L
= -0.465 = 5.02 TeV ycm
sNN
0 - 10%
Method 2 DATA flipped DATA Method 2 MC flipped MC
-3 -2 -1 0 1 2 η3
η/dtracklet dNevt1/N
0 5 10 15 20 25 30 35 40
45 ATLAS Simulation Preliminary
= -0.465 = 5.02 TeV ycm
sNN
p+Pb 0 - 10 %
primary secondary fakes flipped
Figure 5:
η-distribution of number of tracklets reconstructed with Method 2. Left panel shows compar-ison of the data (markers) to MC (lines). The results of the flipped reconstruction are shown with open markers for data and dashed line for MC. Right panel shows the result of MC for three contributions: pri- mary (yellow) secondary (cyan) and fake (green). Square markers show the result of simulation obtained with flipped reconstruction events.
the data in detail. A breakdown of the MC distribution into primary, secondary and fake contributions is shown in the right panel of Fig. 5. The distribution of
N2pfl(η) given in eq. 2 and plotted with open markers follows exactly the green histogram, which justifies the subtraction of the fake component in Method 2. Of the three methods used in this analysis, Method 2 has the largest contribution of fakes. In the 0-10% centrality interval, the fake contribution amounts to 8% of the yield at mid-rapidity and up to 16% at large pseudorapidity. In the same centrality interval, the contribution of fakes in Method 1 varies from 2% to 10% and from 0.2% to 1.5% in the pixel track method. Method 1 and the pixel track method rely on the MC to correct for the contribution from fakes and all three methods rely on the MC to correct for the contribution of secondary particles.
The data analysis and corresponding corrections were performed in 8 intervals of detector occupancy (O) parametrized using the number of reconstructed clusters in the first pixel layer, and in 7 intervals of
zvtx, each 50 mm wide. For each analysis method, a multiplicative correction factor was obtained from the MC simulations. It corrected for several effects: inactive areas in the detector and reconstruction e
fficiency; contributions of residual fakes and secondary particles; and losses due to track or tracklets selection cuts including particles with
pTbelow 100 MeV. The correction factor is evaluated as a function of occupancy
O, event vertexzvtx, and pseudorapidity as:
C(O,zvtx, η)≡ Npr
(O,
zvtx, η)Nrec
(O,
zvtx, η),(3) where
Nprand
Nrecrepresent the number particles at the generator level and the number of tracks or tracklets at the reconstruction level respectively. These factors are then applied to obtain the corrected, per-event charged particle pseudorapidity distributions according to
dNch dη =
1
Nevt X
zvtx
∆Nraw
(O,
zvtx, η)C(O,zvtx, η)∆η ,
(4)
where
∆Nrawindicates either the number of reconstructed pixel tracks or two-point tracklets and
Nevtis the total number of analysed events.
Figure 6 shows the effect of the applied correction for all three methods. The left panel shows the
-3 -2 -1 0 1 2 η3 η/dch dNevt1/N
0 10 20 30 40 50 60
Simulation Preliminary ATLAS
= -0.465 = 5.02 TeV ycm
sNN
p+Pb 0 - 10 %
generated primary Method 1 Method 2 pixel tracks method
-3 -2 -1 0 1 2 η3
η/dch dNevt1/N
0 10 20 30 40 50 60
Preliminary ATLAS
b-1
µ
int= 1 p+Pb L
= -0.465 = 5.02 TeV ycm
sNN
0 - 10 %
Method 1 raw Method 2 raw pixel tracks method raw Method 1 corrected Method 2 corrected pixel tracks method corrected
Figure 6: Left:
η-distribution from the MC for the generated primary charged particles (histogram),tracklets from Method 1 (circles), tracklets from Method 2 after flipped event subtraction (squares), and pixel tracks (diamonds). Right: Open markers represent the same distributions as in the left panel, reconstructed in the data. Filled markers of the same shape represent corrected distributions.
MC results based on HIJING. The distribution of generated primary charged particles is shown by a solid line and the distributions of reconstructed tracks and tracklets are indicated by markers. Among the three methods, the correction factors for Method 1 are the smallest, while the pixel track method requires the largest corrections. The variation of the reconstructed distribution for the pixel track method around
η = ±2 is related to the transition between the barrel and endcap regions of the detector. Theopen markers in the right panel of Fig. 6 show the reconstructed distribution from the data and the filled markers are the corresponding distribution for the three methods after applying corrections. The corrected results are in good agreement with each other, which demonstrates that the rejection of fakes and the rest of the correction procedure are well understood. In this analysis Method 1 is chosen as the default result for
dNch/dη, Method 2 is used for systematic uncertainties and the pixel track method isused primarily as a consistency test, as discussed in detail below.
7 Systematic uncertainties
The systematic uncertainties on
dNch/dηmeasurement arise from three main sources: 1) inaccuracies of detector description in simulations, 2) sensitivity to selection criteria used in the analysis, including the residual contributions of fakes and secondaries and 3) differences between the generated particles used in the simulation and the data. To extract uncertainties for each source, one of the parameters used in the analysis, such as tracklets selection criteria, simulated particle composition, etc. was altered within acceptable limits. The analysis was performed fully for each variation of the parameters and compared to the standard results of Method 1.
The uncertainty on the detector description arises primarily from the details of the pixel detector acceptance and efficiency. The locations of the inactive pixel modules were precisely matched between the data and simulation. Areas smaller than a single module which were found to have intermittent ine
fficiencies were estimated to contribute less than 1.7% uncertainty to the final result. This uncertainty has no centrality dependence, and is approximately independent of pseudorapidity.
The uncertainties related to the description of the inactive detector material were evaluated using a
MC sample with 10% extra material. The net e
ffect on the final result is found to be 2%, independent of
centrality.
Uncertainties due to tracklet selection cuts were evaluated by independently varying the cuts on
|∆η|and
|∆φ|up and down by 40%. The e
ffect of these variations is less than 1%, except at high-η, and has only a weak centrality dependence.
The HIJING event generator used in the analysis is known to be inconsistent with the
pTdistributions measured in data. This was addressed by re-weighting the HIJING distribution using the reconstructed spectrum measured with the pixel track method. Since a full spectral analysis was not performed in the framework of this
dNch/dηmeasurement, the systematic uncertainty on this procedure was assigned to be equal to the magnitude of the variation produced by the re-weighting procedure. This is less than 0.5%
for
|η| <1.5 and grows to 3.0% towards the edges of the
ηacceptance. The uncertainty has a centrality dependence because the
pTdistributions in central and peripheral collisions are different.
Tracklets are reconstructed in Method 1 for particles with
pT >100 MeV. The unmeasured region of the spectrum contributes approximately 6% to the final
dNch/dη. The systematic uncertainty on the ex-trapolation to
pT=0 is partially included in the variation of the tracklet∆φselection criteria. In addition, this uncertainty was evaluated by varying the shape of the spectra below 100 MeV. This uncertainty was conservatively estimated to reach up to 2.5% at high
ηand has a weak centrality dependence.
To test the sensitivity to the particle composition in HIJING, the fraction of pions, kaons and protons in HIJING were varied within a range according to the di
fferences between
p+pand Pb
+Pb measured by the CMS and ALICE experiments [47, 48]. The resulting changes of
dNch/dηare found to be less than 1% for all centrality intervals.
The three methods have quite di
fferent sensitivities to fake tracks and tracklets. While all three meth- ods agree with each other very well, Method 1 and Method 2 require corrections of a similar magnitude while the pixel track method requires significantly larger correction. The uncertainties due to the pres- ence of residual fakes are estimated by comparing the results between the two tracklet methods. The di
fference in the most central collisions is found to be less than 1.5% in the barrel region and increases to about 2.5% at the far edges of the measured pseudorapidity range.
The uncertainty related to the event selection procedure described in Section 5 is evaluated by varying the
ΣEPbTranges used to define centrality intervals, according to an overall trigger and event selection efficiency of 98
±2%. The variation is performed by generating new centrality intervals assuming this e
fficiency is 96% and 100%. This resulting change of the
dNch/dηis less than 0.5% in central collisions and increase to 6% in peripheral collisions.
The systematic uncertainties are summarized in Table 1. All uncertainties are treated as independent, so the resulting total systematic uncertainty is a quadratic sum of the individual contributions.
Uncertainty 60-90% Uncertainty 0-1%
Source barrel endcap barrel endcup
MC detector description 1.7% 1.7%
Extra material 1% 2% 1% 2%
Tracklet selection 0.5% 1.5% 0.5% 1.5%
pT
re-weighting 0.5% 0.5% 0.5% 3.0%
Extrapolation to
pT=0 1% 2.5% 1% 2%
Particle composition 1% 1%
Analysis method 1.5% 2.0% 1.5% 2.5%
Event selection 5.0% 6.0% 0.5% 0.5%
Table 1: Summary of the various sources of systematic uncertainties and their estimated impact on the
dNch/dηmeasurement in central (0-1%) and peripheral (60-90%)
p+Pb collisions.
8 Results
Figure 7 presents the charged particle pseudorapidity density for
p+Pb collisions at
√sNN =
5.02 TeV in the pseudorapidity interval
|η| <2.7 for eight centrality intervals. In the most peripheral collisions
-3 -2 -1 0 1 2 η 3
η /d
chdN
0 10 20 30 40 50 60
70
ATLAS Preliminary b-1µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
0-1%
1-5%
5-10%
10-20%
20-30%
30-40%
40-60%
60-90%
Figure 7:
dNch/dηmeasured in different centrality intervals. Statistical uncertainties, shown with vertical bars are typically smaller than the marker size, colour band shows the systematic uncertainty of the results.
(centrality interval 60-90%)
dNch/dηhas what appears to be a double-peak structure, similar to that seen in proton-proton collisions [35, 49]. In more central collisions, the shape of
dNch/dηbecomes progres- sively more asymmetric, with more particles produced in the Pb-going direction than in the proton-going direction.
To investigate further the centrality evolution, the distributions in the various centrality intervals are divided by the distribution in the 60-90% centrality interval. The ratios are shown in Fig. 8. The double peak structure seen in the distributions in Fig. 7 disappears in the ratios. The ratios are observed to grow nearly linearly with pseudorapidity, with a slope that increases from peripheral to central collisions. In the 0-1% centrality interval, the ratio increases by almost a factor of two over the measured
η-range. Theseratios are fit with a second-order polynomial function, and the fit results are summarized in Table 2.
Figure 9 shows the
dNch/dηdivided by the number of participant pairs (
hNparti/2) as a functionof
hNpartifor three different implementations of the Glauber model; standard Glauber (top panel) and Glauber-Gribov model with
Ω =0.55 and 1.01 in the middle and lower panels respectively. Since the charged particle yields have significant pseudorapidity dependence, the
dNch/dη/(hNparti/2) is presentedin five
ηintervals including the full pseudorapidity interval,
−2.7< η <2.7.
The
dNch/dη/(hNparti/2) values from the standard Glauber model are approximately constant up to hNparti ≈10 and then increase for larger
hNparti. This trend is absent in the Glauber-Gribov model with
Ω =0.55, which shows a relatively constant behaviour for the integrated yield divided by the number of
participant pairs. Finally, the
dNch/dη/(hNparti/2) values from the Glauber-Gribov model withΩ =1.01
-3 -2 -1 0 1 2 η 3 )
60-90%| η /d
ch) / (dN
cent.| η /d
ch(dN
0 1 2 3 4 5 6 7 8
9
ATLAS Preliminary b-1µ
int= 1 p+Pb L
= 5.02 TeV sNN
= -0.465 ycm
0-1%
1-5%
5-10%
10-20%
20-30%
30-40%
40-60%
Figure 8: Ratios of
dNch/dηdistributions measured in di
fferent centrality intervals,
dNch/dη|cent, to that in the peripheral (60-90%) centrality interval. Lines show the results of second order polynomial fits to the data points.
Centrality ratio
c b a0 - 1%
/60 - 90% 6.78
±0.28 0.77
±0.05 -0.033
±0.006 1 - 5%
/60 - 90% 5.35±0.22 0.515±0.031 -0.030±0.005 5 - 10%
/60 - 90% 4.49±0.18 0.377±0.021 -0.0218±0.0035 10 - 20%
/60 - 90% 3.77
±0.14 0.269
±0.014 -0.0169
±0.0025 20 - 30%
/60 - 90% 3.11±0.11 0.182±0.010 -0.0113±0.0020 30 - 40%
/60 - 90% 2.61±0.08 0.122±0.006 -0.0076±0.0016 40 - 60%
/60 - 90% 1.95
±0.06 0.0595
±0.0031 -0.0037
±0.0011
Table 2: Parameters of second order polynomial fits (c
+bη+aη2) to
dNch/dηratios shown in Fig. 8. The stated uncertainties combined statistical and systematic contributions, with the latter making the larger contribution.
show a slight decrease with
hNpartiin all
ηintervals.
The presence or absence of
hNpartiscaling does not in itself suggest a preference for one or another of
the implementations of the Glauber model. However, this study emphasizes that considering fluctuations
of the nucleon-nucleon cross section in the Glauber-Gribov model may lead to significant changes in the
Npartscaling behaviour of the
p+Pb
dNch/dηdata and, thus, their possible interpretations.
0 10 20 30
/2) 〉
partN 〈 / ( η /d
chdN
2 4 6
8
ATLAS Preliminary b-1µ = 1 p+Pb Lint
= 5.02 TeV sNN
= -0.465 ycm
< 2.7 η -2.7 <
< 2.7 η 2 <
< 1 η 0 <
< 0 η -1 <
< -2 η -2.7 <
Glauber
0 10 20 30
2 4 6 8
=0.55 Ω Glauber-Gribov
〉 N
part0 10 20 〈 30
2 4 6 8
0
=1.01 Ω Glauber-Gribov
Figure 9:
dNch/dη/(hNparti/2) as a function ofhNpartiin several
η-regions for the three implementationsof the Glauber model: the standard Glauber model (top panel), the Glauber-Gribov model with
Ω=0.55(middle panel) and the Glauber-Gribov model with
Ω=1.01 (bottom panel). The open boxes representthe systematic uncertainty of the
dNch/dηmeasurement only, and the width of the box is chosen for better visibility (they are not shown for
−1.0
< η <0 and 0
< η <1). The shaded boxes represent the total uncertainty, which is dominated by the uncertainty on the
hNpartigiven in Table 4 and Fig. 3.
They are shown for
−2.7 < η <2.7. Note that this uncertainty is asymmetric in both directions, due to the asymmetric nature of the uncertainties on
hNparti. The statistical uncertainties are smaller than themarker size for all points.
9 Conclusions
This note presents ATLAS measurements of the centrality dependence of the charged particle pseu- dorapidity distribution,
dNch/dη, in p+Pb collisions at a nucleon-nucleon centre-of-mass energy of
√sNN =
5.02 TeV. The results are shown as a function of pseudorapidity over the range
−2.7
< η <2.7
and for the 90% most central
p+Pb collisions. The analysis was performed primarily with the ATLASpixel detector, and the collision centrality was defined using a forward calorimeter covering 3.2
< η <4.9
in the Pb-going direction. The average number of participants in each centrality interval,
hNparti, was es-
timated using a Monte Carlo Glauber model. The Glauber modeling was performed both in the standard
way, with a fixed nucleon-nucleon cross section, as well as in a Glauber-Gribov approach, which allows
the nucleon-nucleon cross section to fluctuate event-by-event.
The shape of
dNch/dηevolves gradually with centrality from an approximately symmetric shape in the most peripheral collisions to a highly asymmetric distribution in the most central collisions. The ratios of
dNch/dηdistributions in different centrality intervals to the
dNch/dηin the most peripheral interval are approximately linear in
ηwith a slope that is strongly dependent on centrality.
The
Npartdependence of
dNch/dη/(hNparti/2) was found to be sensitive to the Glauber modeling,especially in the most central collisions: while the standard Glauber modeling leads to a strong increase in the multiplicity per participant pair for the 30% most central collisions, the Glauber-Gribov approach leads to a much milder centrality dependence. These results point to the importance of understanding not just the initial state of the nuclear wave function, but also the fluctuating nature of nucleon-nucleon collisions themselves. A deeper understanding of this physics is needed before more precise connections can be made between particle production and the geometry of the initial state.
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Appendix A: Glauber and Glauber-Gribov analysis
The geometry of nucleus-nucleus (A
+A) and proton
/deuteron-nucleus (p
/d+A) collisions is often stud- ied using Glauber Monte Carlo models [30, 44] that simulate the interactions of the incident nucleons using a semi-classical eikonal approximation. However, it has been argued that in high energy
p+Acollisions, the Glauber model must be corrected to account for the fact that the incoming proton is o
ffshell between successive interactions in the target nucleus[50]. In addition, event-to-event fluctuations in the configuration of the incoming proton can change its effective scattering cross-section [51, 31, 32].
At high energies, the configuration of the proton is taken to be frozen over the time scale of the
p+A collision. To evaluate the impact of these frozen fluctuations of the projectile proton, a modified ver- sion of the PHOBOS Glauber Monte Carlo [44], referred to as “Glauber-Gribov” in the rest of this note, was developed that implemented event-to-event variations in the Glauber Monte Carlo nucleon-nucleon cross-section. Following Refs. [31] and [32], the probability distribution of
σtotvalues was taken to be
2Ph
(σ
tot)
=ρ σtot σtot+σ0exp
(
−
(σ
tot/σ0−1)
2 Ω2)
.
(5)
Here,
ρis a normalization constant,
Ωcontrols the width of the
Ph(σ
tot) distribution, and
σ0determines
hσtoti. The inelastic fraction of the total cross-section is taken to be constant [32],σNN = λσtot, so the probability distribution for
σNNis given by
PH
(σ
NN)
=1
λP(σNN/λ)
(6)
Estimates of
Ωwere provided in Ref. [31] for centre-of-mass energies 1.8, 9, and 14 TeV. An interpola- tion of those values to
√sNN =
5.02 TeV for use in this analysis yielded
Ω =0.55, a value that is only marginally larger than the value at 9 TeV,
Ω =0.52. The corresponding value of
σ0=78.6 mb was de- termined by requiring a total cross-section,
σtot=86 mb, consistent with the Donnachie and Landshoff [52] parameterization used in [31]. An alternative choice of
σtotconsistent with more recent measure- ments [53] has only a small e
ffect on the final distribution. Recently, updated estimates,
Ω =1.01 and
σ0 =72.5 mb corresponding to
σtot=94.8 mb were obtained [32] using results of diffraction measure- ments at the LHC. For the purposes of this note, the Glauber-Gribov analysis was performed using both
Ω =0.55 and 1.01 in order to evaluate the sensitivity of the physics conclusions to the choice of
Ω. For each of the
Ωvalues,
λwas chosen to produce a
σNNvalue of 70 mb with the results
λ=0.82 and 0.74, respectively, for
Ω =0.55 and 1.01.
The Glauber-Gribov
PH(σ
NN) distributions are shown in the left panel of Fig. 10 for both values of
Ωand corresponding
σ0and
λvalues. The distribution of the number of participants,
Npart, obtained from the two Glauber-Gribov formulations are shown in the right panel of Fig. 10 together with a standard Glauber MC
Npartdistribution obtained using a fixed inelastic cross-section,
σNN=70 mb. For all three calculations, the lead nucleon density distribution was taken to be Woods-Saxon with radius and skin depth parameters,
R=6.62 fm and
a=0.546 fm [54]. The Glauber-Gribov
Npartdistributions are much broader than the Glauber distribution due to the
σNNcross-section fluctuations in the Glauber-Gribov formulations.
To connect an experimental measurement of collision centrality such as
ΣEPbTto the results of the Glauber or Glauber-Gribov Monte Carlo, a model for the
Npartdependence of the
ΣETPbdistribution is required. The usual basis for such models, previously applied to A+A and
p/d+A collisions, is the WNmodel [11]. When applied to this analysis, this model predicts that
ΣETPbwould increase proportionally to
Npartwith the proportionality constant equal to one half the corresponding average FCal
PETin
p+p2The first arXiv version of [32] contained a subsequently fixed typographical error that made the distribution exponential instead of Gaussian.