- J. Milošević
University of Belgrade and Vinča Institute of Nuclear Sciences, Belgrade, Serbia
08.08.2016 Reimei 2016, Tokai, Japan 1
Initial state fluctuations from SPS to LHC J. Milo evi University - - PowerPoint PPT Presentation
Initial state fluctuations from SPS to LHC J. Milo evi University of Belgrade and Vin a Institute of Nuclear Sciences, Belgrade, Serbia 08.08.2016 Reimei 2016, Tokai, Japan 1 Outline v Azimuthal anisotropy conventional
08.08.2016 Reimei 2016, Tokai, Japan 1
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 2 ¡
² conventional methods ² Initial-state fluctuations (ISF) and higher order Fourier harmonics
² ISF on sub-nucleonic level
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 3 ¡
y
x y z
vn = cosn(φ−Ψn)
event plane x-z
Ideal circle-like geometry – v2
η Δ
2 4 φ Δ 2 4
φ Δ d η Δ d
pair
N
2
d
trig
N 1
1.6 1.7 1.8
110 ≥
trk
= 5.02 TeV, N
NN
s CMS pPb < 3 GeV/c
T
1 < p (b)
1<pT<3 GeV/c pPb 5.02 TeV
0-3% centrality N>110
PLB 718 (2013) 795
cos(nΔφ)
Advantage wrt 2-part.corr.: removes two- and three- particle non- flow correlation
u vn from even higher order cumulants: vn{6}, vn{8}, ….
correlates all particles of interest
|Δη| > 3
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 4 ¡
p
Phys.Rev. ¡C89 ¡(2014) ¡044906 (arXiv:1310.8651) JHEP ¡1402 ¡(2014) ¡088 (arXiv:1312.1845) Phys.Le8. ¡B724 ¡(2013) ¡213 (arXiv:1305.0609)
geometry – v2 ISF – v3
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 5 ¡
PRC ¡81(2010) ¡054905 The triangular initial shape è triangular hydrodynamic flow
track
N
80 100 120 140 160 180 200 220 240
〉 )]
3 (b)
Ψ
(a)
Ψ cos[3( 〈 2 1/
2 4 6 8 10 12
=17.3 A GeV
≈30M PbAu collisions collected during 2000 data taking period
σ/σgeo=<5.5%>
Reimei ¡2016, ¡Tokai, ¡Japan ¡ 6 ¡
(GeV/c)
T
p
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
)
T
(p
3
v
0.01 0.02 0.03 0.04 0.05
= 5.5% 〉
geo
σ / σ 〈
not corrected for HBT correlations
corrected for HBT correlations
0.21 < η < 0.86 in center-of-mass system
accepted ¡to ¡Nucl.Phys.A
beam UV detector 2 UV detector 1 W-shield target SDD1/SDD2 RICH 1 mirror 1 RICH 2 mirror 2 8
TPC read-out chamber TPC coils
1 2 3 4 5m 1/r E-field HV cathode voltage divider
Ψ3 = 1 3arctan wi(pTi)sin(3φi)
i=1 Ntrack
∑
wi(pTi)cos(3φi)
i=1 Ntrack
∑
08.08.2016 ¡
sNN
EP ¡method ¡is ¡used
a ¡huge ¡HBT ¡effect ¡at ¡ ¡low-‑pT
T
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
T
3
0.01 0.02 0.03 0.04 0.05 0.06 0.07
< 10.0%
geo
σ / σ ALICE 0 < < 10.0%
geo
σ / σ PHENIX 0 < = 5.5% 〉
geo
σ / σ 〈 CERES
±
= 2.76 TeV, h
NN
s ALICE PbPb
±
= 200 GeV, h
NN
s PHENIX AuAu
= 17.3 GeV,
NN
s CERES PbAu 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 7 ¡
v First pT dependent measurement of the triangular flow at the top SPS energy v Top RHIC and LHC energy gives very similar v3 magnitudes v The v3 at the top SPS energy is about half of those at top RHIC and LHC v Linear increase but with different slopes accepted ¡to ¡Nucl.Phys.A
² Note limited pT range restricted to the CERES acceptance ² ALICE uses large |Δη| gaps ² Jet yield is for more than one
magnitude smaller at SPS ² No option to include |Δη| gap at CERES
PHENIX
PRL 107 (2011) 252301
ALICE
PLB 719 (2013) 18
NN
10
2
10
3
10
3
3
0.6 0.7 0.8 0.9 1
±
= 2.76 TeV, h
NN
s ALICE PbPb
±
= 200 GeV, h
NN
s PHENIX AuAu
±
= 19.6 GeV, h
NN
s STAR AuAu
= 17.3 GeV,
NN
s CERES PbAu
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 8 ¡
v RHIC 19.6 GeV is quite close to the top SPS energy of 17.3 GeV v Comparison is done at very similar centralities (<σ/σgeo> ≈ 5%) v A rather good agreement with an AMPT prediction for the ratio of about 0.6 at 19.6 GeV RHIC energy Accepted ¡to ¡Nucl.Phys.A
² As a referent level is taken v3 value at the top RHIC energy ² v3 values integrated over 0.3 < pT < 2.1 GeV/c !
a good agreement same v3 at the top RHIC and LHC
PHENIX
PRL 107 (2011) 252301
ALICE
PLB 719 (2013) 18
STAR
PRL 116 (2016) 112302
(GeV/c)
T
p
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
)
T
(p
3
v
0.01 0.02 0.03 0.04 0.05
= 2.4% 〉
geo
σ / σ 〈 = 9.8% 〉
geo
σ / σ 〈
08.08.2016 ¡
(GeV/c)
T
p
0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
)
T
(p
n
v
0.01 0.02 0.03 0.04 0.05
= 2.4% 〉
geo
σ / σ 〈
n = 2 n = 3
(GeV/c)
T
p
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2 0.01 0.02 0.03 0.04 0.05
= 9.8% 〉
geo
σ / σ 〈
n = 2 n = 3
Reimei ¡2016, ¡Tokai, ¡Japan ¡ 9 ¡
v Elliptic flow reflects the initial anisotropy and thus depends strongly on centrality v Triangular flow comes from the ISF and weakly depends on centrality v The different centrality behavior between v2 and v3 v For very central collisions (<σ/σgeo> = 2.4%), v3 becomes close to the v2 accepted ¡to ¡Nucl.Phys.A
² Triangular flow is dominant anisotropy for ultra-central collisions at the LHC energies
CMS
JHEP 1402 (2014) 088
T
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
T
3
0.01 0.02 0.03 0.04 0.05
= 5.5% 〉
geo
σ / σ 〈 ,
CERES < 7% σ , 0 <
hydro+UrQMD 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 10 ¡
v Relativistic hydrodynamics + transport models (hybrid models)
² vHLLE viscous hydrosolver + UrQMD hadron cascade (I. Karpenko, P. Huovinen, H. Petersen
and M. Bleicher PRC 91 (2015) 064901)
v The model predictions for hadrons within 0.2 < pT <2.0 GeV/c and -1 < η < 1 v Cerentrality samples roughly correspond to the experimental ones accepted ¡to ¡Nucl.Phys.A
² Particlization at constant energy density 0.5 GeV fm3 ² Kinetic and chemical freeze-out are dynamical ² Model predictions in a very good agreement with the CERES results ² A small disagreement appears at low-pT
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 11 ¡
20 40 60 80
n
v
0.0 0.1 0.2
0 - 5% (GeV/c)
T
p
20 40 60 80
n
v
0.0 0.1 0.2
30 - 40%
20 40 60 80
0.0 0.1 0.2
5 - 10% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
40 - 50%
20 40 60 80
0.0 0.1 0.2
10 - 20% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
50 - 60%
20 40 60 80
0.0 0.1 0.2
20 - 30% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
= 5.02 TeV
NN
s PbPb CMS Preliminary
{SP}
2
v {SP}
3
v
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 12 ¡
v low-pT - hydrodynamic flow (v2 – geometry, v3 – ISF on nucleonic level) v v2 non-zero up to very high pT v high-pT - may reflect the path-length dependence of parton energy loss v v2 is complementary to RAA measurements v v3 mainly consistent with zero at high-pT
up to 100 GeV/c
CMS ¡PAS ¡HIN-‑15-‑014
20 40 60 80
n
v
0.0 0.1 0.2
5 - 10%
= 5.02 TeV
NN
s PbPb CMS Preliminary
(GeV/c)
T
p
20 40 60 80
n
v
0.0 0.1 0.2
30 - 40%
20 40 60 80
0.0 0.1 0.2
10 - 20% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
40 - 50%
20 40 60 80
0.0 0.1 0.2
20 - 30% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
50 - 60% {SP}
2
v {4}
2
v {6}
2
v {8}
2
v
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 13 ¡
v low-pT – ratio v2{2k}/v2{SP} ≈ 0.8 and v2{4} ≈ v2{6} ≈ v2{8} ç hydrodynamics v high-pT – SP and multi-particle correlation tend to converge to the same value v v2{4} ≈ v2{6} ≈ v2{8} ≠ 0 ç collectivity (likely to be related to jet quenching) CMS ¡PAS ¡HIN-‑15-‑014
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 14 ¡
v A slight increase of v2 wrt results (EP method) from 2.76 TeV collision energy v CUJET3 predictions roughly compatible with the data at high-pT (over 40 GeV/c) v At lower pT, CUJET3 overpredicts the experimental v2 CMS ¡PAS ¡HIN-‑15-‑014
20 40 60 80
2
v
0.0 0.1 0.2
0 - 5% (GeV/c)
T
p
20 40 60 80
2
v
0.0 0.1 0.2
30 - 40%
20 40 60 80
0.0 0.1 0.2
5 - 10% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
40 - 50%
20 40 60 80
0.0 0.1 0.2
10 - 20% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
50 - 60%
20 40 60 80
0.0 0.1 0.2
20 - 30% (GeV/c)
T
p
20 40 60 80
0.0 0.1 0.2
= 5.02 TeV
NN
s PbPb CMS Preliminary 2.76 TeV {EP}
2
v {SP}
2
v CUJET3 5.02 TeV
low 2
v
0.05 0.10 0.15
high 2
v
0.05 0.10
< 20 GeV/c
T
14 < p CMS Preliminary = 5.02 TeV
NN
s PbPb
low 2
v
0.05 0.10 0.15 0.05 0.10
< 26 GeV/c
T
20 < p
{SP}
2
v {4}
2
v
low 2
v
0.05 0.10 0.15 0.05 0.10
< 35 GeV/c
T
26 < p < 1.25 GeV/c
T
1.0 < p
low 2
v 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 15 ¡
v Correlation between low-pT v2 and high-pT v2 over a wide centrality range v Each point represents one centrality bin v Strong correlation may indicate that low-pT v2 and high-pT v2 may have the same
v Within uncertainties, slopes between v2{SP} and v2{2k} are compatible v Extrapolations compatible to 0 within uncertainties CMS ¡PAS ¡HIN-‑15-‑014
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 16 ¡
p
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ η Δ
2 4
φ Δ
2 4
φ Δ d η Δ d
pair
N
2
d
trig
N 1
3.1 3.2 3.3 3.4 N < 260 ≤ = 5.02 TeV, 220
NN
s CMS pPb < 3 GeV/c
trig T
1 < p < 3 GeV/c
assoc T
1 < p
17 ¡ η Δ
2 4
φ Δ
2 4
φ Δ d η Δ d
pair
N
2
d
trig
N 1
2.4 2.6 2.8 N < 260 ≤ = 2.76 TeV, 220
NN
s CMS PbPb < 3 GeV/c
trig T
1 < p < 3 GeV/c
assoc T
1 < p
JHEP 09 (2010) 091 PLB 718 (2013) 795 PLB 724 (2013) 213
high-multiplicity high-multiplicity
100 200 300
{2}
sub 2
v
0.05 0.10
= 5 TeV
NN
s pPb = 2.76 TeV
NN
s PbPb = 13 TeV s pp = 7 TeV s pp = 5 TeV s pp
Preliminary CMS < 3 GeV/c
T
0.3 < p | > 2 η Δ |
trk
N
100 200 300
{2}
sub 3
v
0.01 0.02 0.03
< 3 GeV/c
T
0.3 < p | > 2 η Δ |
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 18 ¡
v There is no or a very weak energy dependence of v2 in pp collisions v v2{2} in pp collisions shows a similar pattern as the one seen in pPb collisions (gets flat at the highest multiplicities) v The v2{2} magnitude is ordered: it is highest in PbPb, gets smaller in pPb and become smallest in pp collisions v In difference of the v2, the v3 magnitude is comparable to those in pPb and PbPb collisions v At low multiplicities, the systematic uncertainties are large for all the three systems v At high multiplicities, v3 in pp increases at a slower rate than in pPb and PbPb systems CMS ¡PAS ¡HIN-‑16-‑010
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 19 ¡
v Multi-particle correlations are used to reduce jet correlations from the away side and to explore collective nature of the long-range correlations in pp. v2{4} and v2{6} are extracted v Clear negative c2{4} at high multiplicities in pp at 13 TeV is seen v and positive c2{6} v Statistical limitations CMS ¡PAS ¡HIN-‑16-‑010
trk
N
50 100 150 200
{4}
2
c
0.00 0.01 0.02 0.03
3 −
10 × = 13 TeV s = 7 TeV s = 5 TeV s = 5 TeV
NN
s Preliminary CMS pp pPb < 3 GeV/c
T
0.3 < p | < 2.4 η |
trk
N
50 100 150 200
{6}
2
c
0.00 0.05 0.10
6 −
10 × = 13 TeV s pp = 5 TeV
NN
s pPb Preliminary CMS < 3 GeV/c
T
0.3 < p | < 2.4 η |
vn 4
{ }=
−cn 4
{ }
4
vn{6} =
1 4 cn{6} 6
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 20 ¡
v Elliptic flow in pp measured using 2- and multi-particle correlations – compared to pPb and PbPb results v v2{2}/v2{4}(pp) ≤ v2{2}/v2{4}(pPb) ç related to initial-state (IS) fluctuations v smaller v2{2}/v2{4} ç less IS fluctuating sources (PRL 112 (2014) 082301) v2{2} ≥ v2{4} ≈ v2{6} collectivity! CMS ¡PAS ¡HIN-‑16-‑010
trk
N
50 100 150
2
v
0.05 0.10
= 13 TeV s pp < 3.0 GeV/c
T
0.3 < p | < 2.4 η | Preliminary CMS
|>2} η Δ {2, |
sub 2
v {4}
2
v {6}
2
v {8}
2
v {LYZ}
2
v
trk
N
100 200 300 0.05 0.10
= 2.76 TeV
NN
s PbPb < 3.0 GeV/c
T
0.3 < p | < 2.4 η |
trk
N
100 200 300 0.05 0.10
= 5 TeV
NN
s pPb < 3.0 GeV/c
T
0.3 < p | < 2.4 η |
η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 0.10 0.12
Preliminary = 13 TeV s CMS pp < 20
trk
N ≤ 10 < 3 GeV/c
assoc T
, p
trig T
1 < p
±
±
h η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 0.12 0.14 0.16 ±
S
K η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 0.12 0.14 0.16 ±
Λ / Λ η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 1.65 1.70 1.75
Preliminary = 13 TeV s CMS pp < 150
trk
N ≤ 105 < 3 GeV/c
assoc T
, p
trig T
1 < p
±
±
h η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 1.70 1.75 1.80 ±
S
K η Δ
4 2 − 2 4
( r a d i a n s ) φ Δ
2 4 φ Δ d η Δ d
pairN
2d
trigN 1 1.60 1.65 ±
Λ / Λ
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 21 ¡
v charged-charged or charged- strange (KS
0 and / )
particles v particles are correlated within given multiplicity bin v The ridge, at Δϕ ≈ 0 and elongated at Δη, is seen only in high-multiplicity pp events v The ridge is present not only for charged, but also for strange particles v What is the origin of the ridge in the smallest pp system? CMS ¡PAS ¡HIN-‑16-‑010
Λ
Λ Λ
(GeV/c)
T
p
2 4
{2}
sub 2
v
0.00 0.05 0.10 0.15
Preliminary = 13 TeV s CMS pp | > 2 η Δ | < 20)
trk
N ≤ < 150) - (10
trk
N ≤ (105
S
K Λ / Λ
±
h
0.0 0.5 1.0 1.5 q
/n {2}
sub 2
v
0.00 0.02 0.04
S
Polynomial fits to K
(GeV)
q
/n
T
KE
0.0 0.5 1.0 1.5
Data/Fit
0.5 1.0 1.5
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 22 ¡
0.0 0.1 0.2 0.3
(GeV)
T
p
2 4
2
v
0.0 0.1 0.2 0.3 = 5.02 TeV
NN
s CMS pPb
1 −
= 35 nb
int
L < 150
trk
N ≤ 120 (0.5-2.5%)
S
K Λ / Λ
±
h
0.0 0.00 0.05 0.10 0.0 0.5 1.0 1.5 2.0
q
/n
2
v
0.00 0.05 0.10
S
Polynomial fits to K
0.0 0.6 0.8 1.0 1.2 1.4
(GeV)
q
/n
T
KE
0.0 0.5 1.0 1.5 2.0
Data/Fit
0.6 0.8 1.0 1.2 1.4 0.0 0.1 0.2 0.3
(GeV)
T
p
2 4
2
v
0.0 0.1 0.2 0.3 = 2.76 TeV
NN
s CMS PbPb
1 −
b µ = 2.3
int
L < 150
trk
N ≤ 120 3%) ± (67
S
K Λ / Λ
±
h 0.0 0.00 0.05 0.10 0.0 0.5 1.0 1.5 2.0
q
/n
2
v
0.00 0.05 0.10
S
Polynomial fits to K
0.0 0.6 0.8 1.0 1.2 1.4
(GeV)
q
/n
T
KE
0.0 0.5 1.0 1.5 2.0
Data/Fit
0.6 0.8 1.0 1.2 1.4
CMS ¡PAS ¡HIN-‑16-‑010 Phys.Le8.B ¡742 ¡(2015) ¡200 Phys.Le8.B ¡742 ¡(2015) ¡200
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 23 ¡
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 24 ¡
Not a smooth but a lumpy structure ² The goal is to map initial-state and its fluctuations in 3D ² Local hotspots perturb the EP of a smooth medium, so Ψn(pT) contains information about initial-state fluctuations Phys.Rev.C 92 (2015) 034911 ² Within hydrodynamics, initial-state fluctuations could appear as (sub-leading) flows fluctuations Δε(r,ϕ,η)
v3
(2)
a very tiny effect Example: sub-leading triangular flow
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 25 ¡
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 26 ¡
' ( ) ) * ) ) + , ) )
)
² Heinz-Shen VISH2+1: PRC 87 (2013) 034913 ² Kozlov et. al.: ¡arXiv:1405.3976
08.08.2016 ¡
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1 = 2.76 TeV
NN
s CMS PbPb
0-0.2% centrality
< 1.5 GeV/c
T a
1.0 < p
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
0-5%
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
5-10%
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
10-20%
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
20-30%
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
30-40%
(GeV/c)
T b
T a
p
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.8 1
40-50%
0.5 1 1.5 2
< 2.0 GeV/c
T a
1.5 < p Data
VISH2+1 Hydro /s = 0.12 η MC-Glauber, /s = 0.12 η MC-KLN,
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 0.8 1 0.5 1 1.5 2
< 2.5 GeV/c
T a
2.0 < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 0.8 1 0.5 1 1.5 2
< 3.0 GeV/c
T a
2.5 < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 2.5
Reimei ¡2016, ¡Tokai, ¡Japan ¡ 27 ¡
trig
0-0.2% 40-50% v The effect increases with rise of pT
trig and
pT
trig-pT assoc
v Approaching the central collisions, the effect dramatically increases achieving value over 20% v For semi-central collisions, the effect achieves only a size of 2−3% arXiv: ¡1503.01692 ¡ ¡ PRC 92 (2015) 034911
08.08.2016 ¡
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1 = 2.76 TeV
NN
s CMS PbPb
0-0.2% centrality
< 1.5 GeV/c
T a
1.0 < p
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
0-5%
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
5-10%
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
10-20%
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
20-30%
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
30-40%
(GeV/c)
T b
T a
p
0.5 1 1.5 2
)
T b
,p
T a
(p
3
r
0.8 1
40-50%
0.5 1 1.5 2
< 2.0 GeV/c
T a
1.5 < p Data
VISH2+1 Hydro /s = 0.12 η MC-Glauber, /s = 0.12 η MC-KLN,
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 0.8 1 0.5 1 1.5 2
< 2.5 GeV/c
T a
2.0 < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 0.8 1 0.5 1 1.5 2
< 3.0 GeV/c
T a
2.5 < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
(GeV/c)
T b
T a
p
0.5 1 1.5 2 2.5
Reimei ¡2016, ¡Tokai, ¡Japan ¡ 28 ¡
trig
0-0.2% 40-50% arXiv: ¡1503.01692 ¡ PRC 92 (2015) 034911
v Factorization holds better for V3 v Breaking visible
pT
trig-pT assoc ¡
v Very weakly depends on centrality
)
T b
,p
T a
(p
2
r
0.7 0.8 0.9 1
= 5.02 TeV
NN
s pPb /s = 0.08 η = 0.4fm, σ Kozlov et al., = 2.76 TeV
NN
s PbPb /s = 0.12 η VISH2+1, MC-Glauber, /s = 0.12 η VISH2+1, MC-KLN, /s = 0.08 η = 0.4fm, σ Kozlov et al.,
PbPb centrality(%)
CMS
2.0 GeV/c ≈
T b
T a
p < 3.0 GeV/c
T a
2.5 < p
0.1 2.5 7.5 15.0 25.0 35.0 45.0 55.0
tracks |<2.4 η |
N
3
10
)
T b
,p
T a
(p
3
r
0.9 1 1.1 1.2 1.3
0.1 2.5 7.5 15.0 25.0 35.0 45.0 55.0
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 29 ¡
arXiv: 1503.01692 PRC 92 (2015) 034911
v Dramatic increase at ultra- central PbPb. For small centralities (>5%) ≈ few % v The r2 in pPb is a bit smaller than in PbPb v Strong r3 multiplicity dependence in pPb, but very weak in PbPb v A non-flow effect in pPb for the highest pT
trig in lower
multiplicities v VISH2+1 qualitatively describes CMS data v Kozlov et al. hydro model describes pPb. Gives stronger effect for PbPb and fails for r3 at lower multiplicity
VISH2+1: PRC 87 (2013) 034913 Kozlov et al.: ¡arXiv:1405.3976
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 30 ¡
Bozek et al., arXiv: 1011.3354 Global twist Dumitru et al., arXiv: 1108.4764
08.08.2016 ¡
η a a b
5.2
3.0
2.4
)
b
η ,
a
η (
Δ n
V )
b
η ,
a
η (-
Δ n
V
)
b
η ,
a
η (
Δ n
V )
b
η ,
a
η (-
Δ n
V ≡ )
b
η ,
a
η (
n
r
Reimei ¡2016, ¡Tokai, ¡Japan ¡ 31 ¡
r
n ηa,ηb
cos n Ψn −ηa
$ % & ' ( ) cos n Ψn ηa
$ % & ' ( )
For symmetric collision: For asymmetric collision:
r
n ηa,ηb
n −ηa,−ηb
cos n Ψn −ηa
% & ' ( ) * cos n Ψn ηa
% & ' ( ) * cos n Ψn ηa
% & ' ( ) * cos n Ψn −ηa
% & ' ( ) *
08.08.2016 ¡
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
2
r × )
b
η ,-
a
η (-
2
r
0.7 0.8 0.9 1.0
< 150
trk
N ≤ 120 = 5.02 TeV
NN
s CMS pPb
= 35 nb
int
L
< 5.0
b
η 4.4 < < 4.0
b
η 3.0 < Exponential fits
a
η
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
2
r × )
b
η ,-
a
η (-
2
r
0.7 0.8 0.9 1.0
< 220
trk
N ≤ 185
0.0 0.5 1.0 1.5 2.0 0.7 0.8 0.9 1.0 < 3.0 GeV/c
a T
0.3 < p > 0 GeV/c
b T
p
< 185
trk
N ≤ 150
a
η
0.0 0.5 1.0 1.5 2.0 0.7 0.8 0.9 1.0
< 260
trk
N ≤ 220 Reimei ¡2016, ¡Tokai, ¡Japan ¡ 32 ¡
v A significant factorization breakdown in η found in pPb collisions with increase of ηa v The effect increases approximately linearly with ηa v Parameterization with Fn
η
is purely empirical introduced just to quantify behavior of the data
n ηa,ηb
ηηa
arXiv: 1503.01692 PRC 92 (2015) 034911
08.08.2016 ¡
tracks |<2.4 η |
N
2
10
3
10
n η
F 0.00 0.02 0.04 0.06 0.08
0.1 2.5 7.5 15.0 25.0 35.0 45.0 55.0
PbPb centrality(%)
CMS = 2.76 TeV
NN
s PbPb = 5.02 TeV
NN
s pPb
n = 2, 0-0.2% n = 2 n = 3 n = 4 n = 2 Reimei ¡2016, ¡Tokai, ¡Japan ¡ 33 ¡
arXiv: 1503.01692 PRC 92 (2015) 034911
v In PbPb, higher-orders F3
η and F4 η, show much stronger
factorization breaking than for the second order v The F2
η has a minimum
around midcentral PbPb and increases for peripheral and most central collisions v At similar multiplicity, F2
η in pPb larger than
the one in PbPb v Except for the most central PbPb, there is a very weak centrality dependence of F3
η
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 34 ¡
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 35 ¡
v Random data generated by 2D multivariate Gauss distribution
v a matrix
v eigenvectors ei and eigenvalues λi by diagonalization Σ
T Σ e
v First Principal Component: eigenvector e1 points to maximum variance of data
v Second Principal Component: eigenvector e2 points to the next maximum variance of data cloud. Its magnitude is λ1e1 λ2e2
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 36 ¡
Two very recent theoretical papers: R.S.Bhalerao, ¡J-‑Y. ¡Ollitrault, ¡S.Pal ¡and ¡D.Teaney, ¡ ¡ Phys.Rev.LeQ. ¡114 ¡(2015) ¡152301 ¡and A.Mazeliauskas ¡and ¡D.Teaney, ¡Phys.Rev. ¡C91 ¡(2015) ¡ 044902 ¡introduced the PCA as a new method to study hydrodynamics flows
S −
B
S and
B
are calculated for pairs with |Δη|>2 v 7 pT bins (0.3<pT<3.0 GeV/c); the eigenvalue problem of a matrix [VnΔ(pi,pj)] where
PhysRev.C 92 (2015) 034911 arXiv:1503.01692 and other CMS analyses
v Input: two-particle Fourier coefficients measured as
v “The simplest correlations are pairs. The principal component analysis is a method which extracts all the information from pair correlations in a way which facilitates comparison between theory and experiment.” J.-Y. Ollitrault
In this analysis:
e(1) e(2) . . . . e(7) ! " # $ % & VnΔ(p1, p1) VnΔ(p2,p1) VnΔ(p3,p1) . . . . VnΔ(p1, p2) VnΔ(p2, p2) VnΔ(p3, p2) . . . . VnΔ(p1, p3) VnΔ(p2, p3) VnΔ(p3, p3) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . VnΔ(p7, p7) ( ) * * * * * * * * * * + ,
e(2) . . . . e(7) ! " # # # # # # # # # # $ % & & & & & & & & & & = diag λ(1) λ(2) . . . . λ(7) ! " # $ % &
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 37 ¡
v experimental data è VnΔ(pi,pj) è it has its own statistical error ΔVnΔ(pi,pj) v The error propagation through Vn
(α) up to vn (α)
v The new introduced pT dependent variable, flow mode, is defined as
(α)(pi) =
v corresponding single-particle flow mode vn
(α)(p) = Vn (α)(p)
v Δλα and Δeα as RMS of the distributions like ones shown above. Matrix elements VnΔ were perturbed (10k times) within its ΔVnΔ à matrix [VnΔ] nonlinearly perturbed where α=1,…,7
λ distribution, α=2 e distribution, α=2 α=2 signal 200 times smaller wrt α=1 α=2 ¡ α=1 ¡ 2.5<pT<3.0 GeV/c
CMS Preliminary
1 2 3
2 ) α (
v
0.1 0.2 0.3
<260
trk
N ≤ 220
= 5.02 TeV
NN
s pPb
(GeV/c)
T
p
1 2 3
2 ) α (
v
0.1 0.2 0.3
CMS Preliminary
<185
trk
N ≤ 150
(GeV/c) p
1 2 3
n
v
0.1 0.2 0.3
, PLB 724 (2013) 213 |>2} η Δ {2, |
2
v =1 α =2 α
<220
trk
N ≤ 185
(GeV/c)
T
p
1 2 3
n
v
0.1 0.2 0.3
<150
trk
N ≤ 120 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 38 ¡
v The leading flow mode, α=1, practically identical to the v2 measured using two-particle correlations v The sub-leading flow mode, α=2, is essentially equal to zero at small pT and increases up to 4-5% going to the high-pT v The first experimental measurement of the elliptic sub-leading flow v Systematical uncertainties small or comparable to statistical ones only at high-pT CMS ¡PAS ¡HIN-‑15-‑010
1 2 3
2 ) α (
v
0.1 0.2
= 2.76 TeV
NN
s PbPb
CMS Preliminary
0-0.2%
(GeV/c)
T
p
1 2 3
2 ) α (
v
0.1 0.2
20-30%
(GeV/c) p
1 2 3
0.1 0.2
0-5%
(GeV/c)
T
p
1 2 3
0.1 0.2
30-40%
(GeV/c) p
1 2 3
0.1 0.2
0-10%
(GeV/c) p
1 2 3
0.1 0.2
PLB 708 (2012) 249 ALICE , |>0.8} η Δ {|
2
v =1 α =2 α
10-20%
(GeV/c)
T
p
1 2 3
0.1 0.2
40-50%
(GeV/c)
T
p
1 2 3
0.1 0.2
50-60%
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 39 ¡
v The leading flow mode, α=1, essentially equal to the v2 measured by ALICE using two-particle correlations v The sub-leading flow mode, α=2, is positive at UCC and for collisions with centralities above 20% v In the region 0-20% centrality comparable with zero v Similar behavior wrt the r2 results (10.1103/PhysRevC.92.034911, arXiv: 1503.01692) CMS ¡PAS ¡HIN-‑15-‑010
1 2 3
3 ) α (
v
0.05 − 0.05 0.1
= 5.02 TeV
NN
s pPb
<260
trk
N ≤ 220
(GeV/c)
T
p
1 2 3
3 ) α (
v
0.05 − 0.05 0.1
<185
trk
N ≤ 150
CMS Preliminary
(GeV/c) p
1 2 3
n
v
0.05 0.05 0.1
, PLB 724 (2013) 213 |>2} η Δ {2, |
3
v =1 α =2 α
<220
trk
N ≤ 185
(GeV/c)
T
p
1 2 3
n
v
0.05 0.05 0.1
<150
trk
N ≤ 120 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 40 ¡
v The leading triangular flow mode, α=1, nearly identical to the v3 measured using two- particle correlations v The sub-leading flow mode, α=2, is comparable with zero within the given uncertainties. v The first experimental measurement of the triangular sub-leading flow CMS ¡PAS ¡HIN-‑15-‑010
1 2 3
3 ) α (
v
0.1 0.2 0.3
= 2.76 TeV
NN
s PbPb
CMS Preliminary
0-0.2%
(GeV/c)
T
p
1 2 3
3 ) α (
v
0.1 0.2 0.3
20-30%
(GeV/c) p
1 2 3
0.1 0.2 0.3
0-5%
(GeV/c)
T
p
1 2 3
0.1 0.2 0.3
30-40%
(GeV/c) p
1 2 3
0.1 0.2 0.3
0-10%
(GeV/c) p
1 2 3
0.1 0.2 0.3
10-20%
PLB 708 (2012) 249 ALICE , |>0.8} η Δ {|
3
v =1 α =2 α
(GeV/c)
T
p
1 2 3
0.1 0.2 0.3
40-50%
(GeV/c)
T
p
1 2 3
0.1 0.2 0.3
50-60%
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 41 ¡
v Again, the leading flow mode, α=1, essentially equal to the v3 measured by ALICE using two-particle correlations v The sub-leading flow mode, α=2, is, within the uncertainties, equal to zero v Results have a similar centrality dependence to that observed for r3 (Phys. Rev C 92
(2015) 034911, arXiv: 1503.01692)
CMS ¡PAS ¡HIN-‑15-‑010
(GeV/c)
T
p
0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 2.2
)
T
(p
3
v
0.01 0.02 0.03 0.04 0.05
= 5.5% 〉
geoσ / σ 〈 ,
CERES < 7% σ , 0 <
hydro+UrQMD
trk
N
50 100 150 2
v
0.05 0.10
= 13 TeV s pp < 3.0 GeV/c
T
0.3 < p | < 2.4 η | Preliminary CMS |>2} η Δ {2, |
sub 2
v {4}
2
v {6}
2
v {8}
2
v {LYZ}
2
v
0.05 0.10
20 40 60 80
0.0 0.1 0.2
20 - 30%
42 ¡ 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡
CMS Preliminary
up to 100 GeV/c
vn ¡
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 43 ¡
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 44 ¡
arXiv: ¡1503.01692, ¡PRC ¡92 ¡(2015) ¡034911
trig and pT trig-pT assoc
VISH2+1: ¡PRC ¡87 ¡(2013) ¡034913
trig-pT assoc (GeV/c)
(GeV/c)
T b
T a
p
0.5 1 1.5 2
)
T b
,p
T a
(p
2
r
0.6 0.7 0.8 0.9 1
< 1.5 GeV/c
T a
1.0 < p 0-0.2% centrality
= 2.76 TeV
NN
s CMS PbPb
Data
(GeV/c)
T b
T a
p
0.5 1 1.5 2
< 2.0 GeV/c
T a
1.5 < p VISH2+1 Hydro MC-Glauber /s = 0.20 η /s = 0.12 η /s = 0.08 η MC-KLN /s = 0.20 η /s = 0.12 η /s = 0.08 η
(GeV/c)
T b
T a
p
0.5 1 1.5 2
< 2.5 GeV/c
T a
2.0 < p
(GeV/c)
T b
T a
p
0.5 1 1.5 2 2.5
< 3.0 GeV/c
T a
2.5 < p
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
CMS Preliminary = 5.02 TeV
NN
s pPb < 260
trk
N ≤ 220
< 1.5 GeV/c
T trig
1.0 GeV/c < p
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<220
trk
N ≤ 185
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<185
trk
N ≤ 150
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<150
trk
N ≤ 120
0.5 1 1.5 2
< 2.0 GeV/c
T trig
1.5 GeV/c < p
CMS
0.5 1 1.5 2
2
r
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
< 2.5 GeV/c
T trig
2.0 GeV/c < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 2.5
< 3.0 GeV/c
T trig
2.5 GeV/c < p
0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5
45 ¡
trig
trig-pT assoc (GeV/c)
220<Ntrk
trig and
trig-pT assoc
arXiv: ¡1503.01692 ¡ PRC 92 (2015) 034911
120<Ntrk
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
CMS Preliminary = 5.02 TeV
NN
s pPb < 260
trk
N ≤ 220
< 1.5 GeV/c
T trig
1.0 GeV/c < p
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<220
trk
N ≤ 185
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<185
trk
N ≤ 150
0.5 1 1.5 2 0.96 0.97 0.98 0.99 1 1.01
<150
trk
N ≤ 120
0.5 1 1.5 2
< 2.0 GeV/c
T trig
1.5 GeV/c < p
CMS /s=0.08 η Kozlov et. al.,
0.5 1 1.5 2
2
r
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
< 2.5 GeV/c
T trig
2.0 GeV/c < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 2.5
< 3.0 GeV/c
T trig
2.5 GeV/c < p
0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5
46 ¡
trig
trig-pT assoc (GeV/c)
220<Ntrk
arXiv: ¡1503.01692 ¡ PRC 92 (2015) 034911
120<Ntrk
Kozlov et al.: ¡arXiv:1405.3976
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 47 ¡
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<260
trk
N ≤ 220
< 1.5 GeV/c
T trig
1.0 GeV/c < p
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<220
trk
N ≤ 185 CMS Preliminary = 5.02 TeV
NN
s pPb
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<185
trk
N ≤ 150
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<150
trk
N ≤ 120
0.5 1 1.5 2
< 2.0 GeV/c
T trig
1.5 GeV/c < p
CMS
0.5 1 1.5 2
3
r
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
< 2.5 GeV/c
T trig
2.0 GeV/c < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 2.5
< 3.0 GeV/c
T trig
2.5 GeV/c < p
0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5
trig
trig-pT assoc (GeV/c)
220<Ntrk
trig in lower
arXiv: ¡1503.01692 ¡ PRC 92 (2015) 034911
120<Ntrk
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<260
trk
N ≤ 220
< 1.5 GeV/c
T trig
1.0 GeV/c < p
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<220
trk
N ≤ 185 CMS Preliminary = 5.02 TeV
NN
s pPb
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<185
trk
N ≤ 150
0.5 1 1.5 2 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4
<150
trk
N ≤ 120
0.5 1 1.5 2
< 2.0 GeV/c
T trig
1.5 GeV/c < p CMS /s=0.08 η Kozlov et. al.,
0.5 1 1.5 2
3
r
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2
< 2.5 GeV/c
T trig
2.0 GeV/c < p
0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 0.5 1 1.5 2 2.5
< 3.0 GeV/c
T trig
2.5 GeV/c < p
0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5 0.5 1 1.5 2 2.5
48 ¡
trig
trig-pT assoc (GeV/c)
220<Ntrk
trig
arXiv: ¡1503.01692 ¡ PRC 92 (2015) 034911 120<Ntrk
Kozlov et al.: ¡arXiv:1405.3976
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 49 ¡
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
2
r
0.85 0.90 0.95 1.00
0-0.2% centrality = 2.76 TeV
NN
s CMS PbPb
< 5.0
b
η 4.4 < < 4.0
b
η 3.0 < Exponential fits
a
η
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
2
r
0.85 0.90 0.95 1.00
20-30%
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
0-5%
< 3.0 GeV/c
a T
0.3 < p > 0 GeV/c
b T
p
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00 30-40% 0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
5-10%
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
40-50%
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
10-20%
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
50-60%
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
3
r
0.85 0.90 0.95 1.00
0-0.2% centrality = 2.76 TeV
NN
s CMS PbPb
< 5.0
b
η 4.4 < < 4.0
b
η 3.0 < Exponential fits
a
η
0.0 0.5 1.0 1.5 2.0
)
b
η ,
a
η (
3
r
0.85 0.90 0.95 1.00
20-30%
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
0-5%
< 3.0 GeV/c
a T
0.3 < p > 0 GeV/c
b T
p
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00 30-40% 0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
5-10%
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
40-50%
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
10-20%
a
η
0.0 0.5 1.0 1.5 2.0 0.85 0.90 0.95 1.00
50-60%
v The r2 factorization
increases with increase of ηa v Except for the most central collisions, the increase is approximately linear v The effect of factorization breaking is much stronger for higher-order harmonic r3 – opposite to the pT dependence v Almost linear increase
v Parameterization:
n ηa,ηb
ηηa
arXiv: 1503.01692 PRC 92 (2015) 034911
)
T b
,p
T a
(p
2
r
0.7 0.8 0.9 1
= 5.02 TeV
NNs pPb /s = 0.08 η = 0.4fm, σ Kozlov et al., = 2.76 TeV
NNs PbPb /s = 0.12 η VISH2+1, MC-Glauber, /s = 0.12 η VISH2+1, MC-KLN, /s = 0.08 η = 0.4fm, σ Kozlov et al.,
PbPb centrality(%)
CMS
2.0 GeV/c ≈
T b
T a
p < 3.0 GeV/c
T a
2.5 < p
0.1 2.5 7.5 15.0 25.0 35.0 45.0 55.0
tracks |<2.4 η |
N
3
10
)
T b
,p
T a
(p
3
r
0.9 1 1.1 1.2 1.3
0.1 2.5 7.5 15.0 25.0 35.0 45.0 55.0
50 ¡ 08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡
rn = VnΔ(pT1, pT2) VnΔ(pT1, pT1) VnΔ(pT2, pT2) = vn(pT1)vn(pT2)cos n(Ψn(pT1) − Ψn(pT2))
# $ % &
vn 2(pT1)vn 2(pT2) = 1 <1 >1
' ( ) ) * ) ) + , ) )
)
holds brakes non-flow Phys.Rev. ¡C87 ¡(2013) ¡031901 Phys.Rev. ¡C87 ¡(2013) ¡034913
(arXiv:1503.01692)
08.08.2016 ¡ Reimei ¡2016, ¡Tokai, ¡Japan ¡ 51 ¡
(α)∗(pi)Vn (α)∗(pj) α=1 k≤Nb
Phys.Rev.LeQ. ¡114 ¡(2015) ¡152301 ¡ ¡
1.0 2.0 3.0