Can the Weibel-Instability explain fast thermalisation in heavy ion collisions? Dénes Sexty TU Darmstadt Collaborators: Jürgen Berges, Sebastian Scheffler 1. Weibel Instabilities 2. Classical approximation on the lattice 3. Results Growth rates Prolate vs oblate initial conditions Comparison of SU(2) with SU(3) 4. Power law solutions 5. Summary April 3, 2009, Budapest
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Can the Weibel-Instability explain fast thermalisation in heavy ion collisions?
Dénes Sexty
TU Darmstadt
Collaborators: Jürgen Berges, Sebastian Scheffler
1. Weibel Instabilities2. Classical approximation on the lattice3. Results Growth rates Prolate vs oblate initial conditions Comparison of SU(2) with SU(3)4. Power law solutions5. Summary
April 3, 2009, Budapest
The Thermalization Puzzle
Applicability of hydrodynamic models for predicting the collective flow in heavy in collisions suggests local thermal equilibrium for times:
eq~1−2 fm/c
from Boltzmann eq.: Xu, Greinger, Phys. Rev. C (2005) 064901;...
Prethermalisation is enough for hydrodynamics?Berges, Borsányi, Wetterich, PRL 93 (2004) 142002
Way out?
Plasma Instabilites is faster than scattering processes
No artificial separation of scales: all modes live on the same lattice
Berges, Scheffler, Sexty PRD (2008)
Lattice formulations of classical EOM for gauge fields
Lagrange formulation:
Hamiltonian formulation
Space time lattice with temporal and spatial links
DSDUx
=0EOM is calculated from the action:
Electric fields live in group space (represented by temporal plaquettes)
Space discretisation first: H Ea ,U=
12E
a2∑spatial plaq.
Tr U
Ea t t /2=E
a t− t /2−DaH Ea ,U
Ut t =expi t aEaUt
Electric fields live in Lie algebra space
Then Hamiltonian EOM is discretised in time
Needed: matrix exponentialization
Tr U a=ba U=?Needed: inversion of Tr U a
Lagrangian Lattice implementation
Wilson action: S=s∑1
2Tr1TrUspatial−t∑
12Tr1
TrUtemporal
Link variables: Ux=eigAax aa
Equations of Motion
DSDUix
=0Gauss Constraint
DSDU0x
=0
parellel transporter from toxa x
U x=U xU xaU −1xaU
−1xplaquette variable
t=2Tr1
g02 s=
2Tr1gs
2=
as
at
Temporal axial gauge
g0=gs=1 ≈10 N s3=64 3⋯128 3
U 0=1 A0a=0
initially G.C.=0 later also fulfilled
Simulation at
Initial Conditions
anisotropic distribution: lots of particles in the transverse planefew particles in the longitudinal planes
Gaussian initial configuration with:
⟨∣A iak ,t=0∣2⟩=Cexp −kx
2ky2
22 −kz
2
2z2 ≫z
is given by fixing energy densityC
zero initial momenta Gauss constraint is trivially fulfilled
To avoid numerical problems, a small plateau is addedmimicing the quantum n=1/2
⟨∣A iak ,t=0∣2⟩=MAX Cexp −kx
2ky2
22 −kz
2
2z2 ,Amp
∣k∣ Amp≈10−12
Results
t=log10
∑i ,b ,ppx
2py2∣ Ai
b t ,p∣2
∑i ,b,ppz
2∣ A ibt ,p∣2Anisotropy parameter:
primary
seco
ndar
y
Converting to physical units
=LAT
g2 a−4=400 MeV 4⋯700 MeV 4 “pessimistic” or “optimistic” choice
Using the optimistic value of =30 GeV/fm3 , g=1
Energy density needed for
1/=0.1fm/c
=300 TeV/fm3
fourth root and square root: mild dependence on , g
and
Growth rates
1 / sec≈0.3 fm/c1 / sec≈0.8 fm/c
Timescales from secondary rates:
optimisticallypessimistically
=30 Gev/fm3
=1Gev/fm3
Prolate vs Oblate
Pancakes collide + free streaming leads to oblate distribution: transverse plane highly occupied longitudinal modes are empty
What happens if there's no free streaming regime? instability starts before oblate distribution reached prolate distribution: longitudinal highly occupied transversal plane anoccupied