Upload
majed
View
48
Download
0
Embed Size (px)
DESCRIPTION
Dubna July 14, 2008. Landau Hydrodynamics Cheuk-Yin Wong Oak Ridge National Laboratory. Introduction Landau hydrodynamics -- predictions on total N -- prediction on differential dN/dy -- space-time dynamics Modification of Landau ’ s dN/dy - PowerPoint PPT Presentation
Citation preview
1
Landau Hydrodynamics Cheuk-Yin Wong Oak Ridge National Laboratory
Dubna July 14, 2008
• Introduction• Landau hydrodynamics -- predictions on total N -- prediction on differential dN/dy -- space-time dynamics• Modification of Landau’s dN/dy• Comparison with experiment• Conclusions
C.Y. Wong, Dubna Lecture notes (to be posted on preprint archive).
2
Why study Landau hydrodynamics?
• It gives a good description of experimental data• It gives a simple description of the space-time dynamics
of the dense hot matter produced in heavy-ion collisions• Dense hot matter evolution is needed in many problems• It is very simple
• L.D. Landau, Izv. Akad. Nauk SSSR, 17, 51 (1953)
• Belenkij and L.D.Landau,Usp.Fiz.Nauk. 56, 309 (1955)
3
Recent revived interest in Landau hydrodynamics
• BRAHM dN/dy data agree with Landau hydrodynamics
Murray, J. Phys. G30, S667 (2004)
factorn contractio Lorentz
theof logarithm theis L
2 ln
2exp
2
1 24/1
p
NN
m
sL
Ly
LKs
dydN
4
Landau hydrodynamics give the correct multiplicity in AA collisions
Steinberg, arxiv:nucl-ex/0702019
Ly
LKs
dydN
2exp
2
1 24/1
Landau AA
Landau pp
5
Landau hydrodynamics exhibits limiting fragmentation
byyy
yL
y
LdydN
'
'2
'exp
1~
2
Steinberg, arxiv:nucl-ex/0702019
AA Collisions
6
Unanwsered questions:
• Is Landau’s formula for y or η ?• Landau rapidity distribution is actually
The Gaussian Landau distribution is only an approximation
• Does the original Landau distribution agree with data?
224/1 exp yLAKsdydN
norm
We need to answer these questions in Landau hydrodynamics
7
8
Landau Hydrodynamics • Local thermal equilibrium • Particle number is proportional to entropy• Entropy is conserved in Landau hydrodynamics • First stage, independent
(i) 1-D longitudinal expansion
(ii) transverse expansion• Second stage of rapidity freeze-out
when the transverse displacement is equal
to the transverse dimension of the system
x(tm) = a ; tm=rapidity freeze-out time
.2 ,exp 224/1 KyLAKsdydN
norm
9
Consrvation of Entropy in Landau hydrodynamics
• Mean-free path is small, low viscosity• The only means to destroy entropy conser
vation is shock wave. • Landau hydridyncmics is applied after the
completion of the compression stage. It deals only with the expansion of the dense matter after shock-wave compression
10
Landau hydrodynamics predictions on total Nch
GeV.in for 2 )2/(
particles ofnumber Total
34
34
entropy Total
34
densityopy Entr
34
densityEnergy
; 3
4 volumeInitial
22/energy totalInitial
entropy. initial thefrom particles ofnumber total the
getcan that wemeansentropy ofon Conservati
number particle toalproportion is Entropy
).conserving(entropy isentropic is flow icalHydrodynam
2/1
2/1
2/1
30
4/33
0
4/33
04/3
30
30
NNNNpartch
NN
NN
NN
NN
NN
p
NN
NNNN
sKsKNN
AsN
As
ArrscV
rscc
rsVE
m
sArV
AsAsE
NS
11
Landau prediction on Nch/(Npart/2) agrees with experiment
12
1-D longitudinal expansion
)/ln(
of logarithm Introduce
sinh cosh Introduce
3/
state ofequation simple use We
)(
0
0
equations icHydrodynam
10
1101
0100
ty
t
zttztt
yuyu
p
pguupTzT
tT
zT
tT
13
1-D longitudinal expansion solution
conditions initial of choices limited (ii)
part edge not the fluid, ofpart bulk for theonly (i)
:gesdisadvanatMinor
simplicity :Advantage
on.substitutidirect by solution eapproximatan is that thisprovecan We
2/)(
)(3
4exp
solution eapproximat Simple
0)(
2
0)(
2
becomes equations icHydrodynam
0
2
2
yyy
yyyy
tte
te
ty
y
14
Solution of 1-D longitudinal expansion
15yat
uaut
tx
attx
uu
ttx
tv
ttv
tx
xxp
tv
uu
gpguupT
vuuvuuuupT
xT
tT
xx
x
xx
2
2
00
2
200
22
00
222222
02002002
0202
cosh44)(
3
1)(2
3
4
isequation icHydrodynam
)(2 ;
2
1)(
isnt displaceme Transverse3
1
3
4
becomesequation icHydrodynam
)(
;3
4)(
0 equation icHydrodynam
Transverse expansion during the first stage
16
Landau condition for rapidity freeze-out
Angle (and rapidity ) will not change after the transverse displacement is equal to the transverse dimension.
diameter tranversecosh4
)(2
2
aya
ttx
Rapidity freeze-out occurs at different time t for different rapidity (and z).
17
Rapidity distribution
exp :ondistributirapidity Final
2exp
ondistributientropy Final
2ln
cosh )(exp
)(at on distributirapdity theneed We
.cosh
)(exp
cosh/ cosh/
cosh/sinh
at timeon distributiRapidity
22
22
))((
4/30
4/30
4/3
20
0
yydydN
SN
dyyyydS
yyya
y
ydy
tyyyycdS
ytt
ydy
tyyyycdS
c
ydytydytudS
yytzdzudS
t
b
bb
b
ytt
m
m
18
Comparison with experiment
Modified distribution gives better agreement than Landau distribution
19
Comparison with experiment
Modified distribution gives better agreement than Landau distribution
20
Conclusions• Landau’s prediction on Nch agrees with data
• The rapidity distribution in Landau hydrodynamics should be modified. The modified rapidity distribution gives better agreement with experimental data than the Landau distribution
• The quantitative agreement of Landau hydrodynamics supports its use in other problems of heavy ion collisions, such as J/psi suppression, jet quenching, and ridge jet-medium interaction,….