Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
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Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Transport Coefficients in Classical Summary Relativistic Field Theories Marietta M. Homor
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Viscosity of hadronic matter
Figure: Heavy-ion collisions Figure: η/s [1]
◮ observation: nearly ideal
liquid
◮ relevant quantity: η/s
(damping of hydrodynamic waves)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Motivation
◮ small transport coefficient ⇔ strongly interacting
system (strength: g)
◮ η s ∼ 1 g4 log g ◮ non-perturbative ◮ Monte Carlo simulation: less sensitive for ω → 0,
large systematic errors
◮ Boltzmann equation: only if 2-2 collision is enough ◮ objective: transport coefficient in classical field
theory
◮ scheme: „leap-frog” algorithm (dynamics)→
correlators (direct count) → transport coefficient from Green-Kubo - formula
◮ test: classical Φ4 theory
H = 1 2Π2 + 1 2(∇Φ)2 + m2 2 Φ2 + λ 24Φ4 (1)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Simulation
◮ canonical equations, periodic boundary
conditions, leap-frog algorithm
◮ initial conditions:
- Π
- t0 + δt
2
- , Φ(t0)
- ◮ Canonical eq. of ˙
Φ (1st part of time step): Initial condition → Φ(t0 + δt)
◮ Canonical eq. of ˙
Π (2nd part of time step):
- Φ(t0 + δt), Π
- t0 + δt
2
- → Π
- t0 + 3δt
2
- ◮ energy controlled simulation
◮ input parameters: N3 lattice size, a = 1 (grid), λ
(interaction), m2 Lagrangian-mass
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Energy and Temperature
◮ time independent total energy:
E =
- i∈U
1 2Π2
i + 1
2(∇Φ)2
i + m2
2 Φ2
i + λ
24Φ4
i
(2)
◮ in canonical ensemble:
|Πk|2 = 1 Zk
k
dΠkdΦk|Πk|2e−βH (3)
◮ Fourier transformation:
fk∈¯
U = x∈U exp−2πi(kx)/N fx∈U ◮ Temperature using numerical schemes:
|Πk|2 = 2N3T (4)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Temperature
◮ Temperature in this simulation: given Π lattice
→ |Πk|2 counted directly
◮ equilibrium: equipartition and time independece
Temperature (2N3T) Mode (¯ k)
Typical data Time average
Figure: Equipartition (¯ k2 = 3
i=1 sin2
2π kei
N
- )
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Energy and Temperature
Total Energy (E) Temperature (2N3T)
Data
ax + b cx + d
a = 0,63, b = 1,00 c = 0,71, d = −9392,47
- intersect. = 125987
Figure: Temperature dependence of total energy (N3 = V = 503), λ = 5, m2 = −0,5
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Definitions
- 1. based on the oscillation of Φ(x)
◮ neglectable △Φ and ∇Φ ◮ weak interaction → Gauss-approximation:
Φ4 ≈ 3Φ2Φ2
◮ ¨
Φ +
- m2 + λ
2 Φ2
Φ = 0
◮ M = 2π
T
- 2. G(t, x) := Φ(t + t′, x)Φ(t, y) correlator
◮ Fourier →
G(t, k) = 1 tmax − tmin tmax
tmin
dt′Φ(t + t′, k)Φ(t′, −k) (5)
◮ non-interacting, oscillating solution:
G(t, k) =
- |Φk|2
cos ωkt, (6) where ω2
k = k2 + m2
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Mass definition
◮ non-interacting theory:
Φ(t′, k)Φ(t′ + t, −k) = |Φk|2 cos ωkt
◮ Interacting system:
Φ(0, |k| = 0)Φ(t, 0) = a exp(−t/τ) cos(ωt + φ)
Time (t) Φ(0, |k| = 0)Φ(t, 0)
Figure: Effective mass determined by correlator
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Temperature dependency
Mass controlled simulation
◮ initial conditions:
- Π
- t0 + δt
2
- , Φ(t0)
- ◮ time developement then calculation of E,T,M
◮ if M = Mwanted system change ◮ additive and multiplicative noise → exponential
decay of total energy → new system → recalculation
0.4 0.5 0.6 0.7 0.8 0.9 1 1.1 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8
Temperature (2T)
Effective mass (M)
(a) various volumes
0.4 0.5 0.6 0.7 0.8 0.9 1 1.1 100000 200000 300000 400000 500000 600000
Effective mass (M)
Temperature (2N3T)
(b) various Lagrangian m Figure: Temperature dependence of the effective mass
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Spontaneous symmetry breaking
◮ if m2 < 0 → min. of potential energy at:
Φ0 = ±
- 6|m|2
λ ◮ 2nd order phase transition
0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 1.1 1.2 100000 200000 300000 400000
Effective Mass (M) Temperature (2N3T) various (λ)
Figure: Temperature dependence of the effective mass
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Mass near phase-shift
Φ(0, 0)Φ(t, 0) Time (t)
data fit
(a) m = 0.88
Φ(0, 0)Φ(t, 0) Time (t)
data fit
(b) m = 0.69
Φ(0, 0)Φ(t, 0) Time (t)
data fit
(c) m = 0.53
Φ(0, 0)Φ(t, 0) Time (t)
data fit
(d) m = 0.43 Figure: Different mass, same interaction strength λ = 5
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Viscosity from Green-Kubo - formula
◮ Spectral function for bosonic A and B operators:
SBA(t) = B(t)A(0).
◮ Fluctuation-dissipation theorem on finite
temperature: [B, A](ω, k = 0) = (1 − e−βω)SBA(ω, k = 0). (7)
◮ if βω << 1 (ω → 0):
lim
ω→0
1 ω[B, A](ω, k = 0) = βSBA(ω = 0, k = 0). (8)
◮ Linear response theory (Kubo-formula for
transport): η = lim
ω→0
[T12, T12](ω, k = 0) ω , (9) where T12 = ∂xΦ∂yΦ.
◮ Green-Kubo - formula: η = βT12T12(k=0)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
T12T12
2000 4000 6000 8000 10000 12000 5 10 15 20 25 30 35 40
(t)
T12T12(t, 0)
20000 40000 60000 80000 100000 120000 140000 160000 180000 2 4 6 8 10 12 14 16
(ω)
T12T12(ω, 0) Figure: Result of simulation and Fourier-transform
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Classical viscosity
0.1 0.2 0.3 0.4 0.5 0.6 0.7 100000 200000 300000 400000
η = βT12T12
Temperature (2N3T) Classical viscosity λ = 5
5e-07 1e-06 1.5e-06 2e-06 2.5e-06 3e-06 3.5e-06 100000 200000 300000 400000
η/T
Temperature (2N3T) λ = 5
Figure: Classical viscosity
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Interpretation
◮ validity range of classical approximation: pmax ≪ T ◮ role of cut-off: phase-volume: Λ3 6π2 , extreme case:
Λ ≈ T
◮ 1st assumption: transport is dominated by
classical fields
◮ ⇒ η = ηclass
T3 6π2
◮ 2nd assumption: key element in entropy is the
entropy of free boson gas (QM)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
η/s
0.1 0.2 0.3 0.4 0.5 0.6 0.2 0.4 0.6 0.8 1 1.2
η/s T/M
λ = 5 1/(4π)
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Summary
◮ canonical equations + leap-frog algorithm ◮ given Π and Φ fields → E, T ◮ mass by correlator, various system sizes and
interaction strengths
◮ viscosity determinated by Green-Kubo formula
(η = βT12T12(ω = 0, k = 0))
◮ ⇒ practicable method for determining transport
coefficients
◮ extra: spontaneous symmetry breaking, η/s ◮ future plans: more complicated and physically
relevant systems
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary
Bibliography
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- W. G. Holzmann, M. Issah, A. Taranenko, P
. Danielewicz, and Horst Stöcker. Has the qcd critical point been signaled by observations at the bnl relativistic heavy ion collider?
- Phys. Rev. Lett., 98:092301, Mar 2007.
Edward Shuryak. Why does the quark gluon plasma at RHIC behave as a nearly ideal fluid? Prog.Part.Nucl.Phys., 53:273–303, 2004. Jakovác Antal. Véges h˝
- mérséklet˝
u térelméletek jegyzet. El˝
- adás jegyzet.
Pavel Kovtun, Dam T. Son, and Andrei O. Starinets. Holography and hydrodynamics: Diffusion on stretched horizons. JHEP, 0310:064, 2003.
Transport Coefficients in Classical Relativistic Field Theories Marietta M. Homor Introduction Energy and Temperature Mass Classical viscosity Summary