relativistic viscous hydrodynamics for multi-component systems with multiple conserved currents
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Reference: AM and T. Hirano, arXiv:1003:3087. Relativistic Viscous Hydrodynamics for Multi-Component Systems with Multiple Conserved Currents. Akihiko Monnai Department of Physics, The University of Tokyo Collaborator: Tetsufumi Hirano. Hot Quarks 2010 - PowerPoint PPT PresentationTRANSCRIPT
Akihiko MonnaiDepartment of Physics, The University of Tokyo
Collaborator: Tetsufumi Hirano
Relativistic Viscous Hydrodynamics for Multi-Component Systems with
Multiple Conserved Currents
Hot Quarks 2010June 25th 2010, La Londe-Les-Maures, France
Reference: AM and T. Hirano, arXiv:1003:3087
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Outline1. Introduction
Relativistic hydrodynamics and Heavy ion collisions
2. Formulation of Viscous HydroIsrael-Stewart theory for multi-component/conserved current systems
3. Results and DiscussionConstitutive equations and their implications
4. SummarySummary and Outlook
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Quark-Gluon Plasma (QGP) at Relativistic Heavy Ion Collisions
• RHIC experiments (2000-)
• LHC experiments (2009-)
T (GeV)
Tc ~0.2
Hadron phase QGP phase
“Small” discrepancies; non-equilibrium effects?
Relativistic viscous hydrodynamic models are the key
Well-described in relativistic ideal hydrodynamic models
Asymptotic freedom -> Less strongly-coupled QGP?
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Hydrodynamic modeling of heavy ion collisions for RHIC
particles
hadronic phase
QGP phase
Freezeout surface Σ
Pre-equilibrium
Hydrodynamic picture
CGC/glasma picture?
Hadronic cascade picture
Initial condition
Hydro to particles
t
z
t
Purpose of Viscous Hydro:1. Explaining the space-time evolution of the QGP2. Constraining the parameters (viscosities, etc.) from experimental data
Hydrodynamics works at the intermediate stage (~1-10 fm/c)
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Introduction Elliptic flow coefficients from RHIC data
Hirano et al. (‘09)
Ideal hydro Glauber1st order
Viscosity
Eq. of state
theoretical prediction experimental data
Ideal hydro works well
Initial condition
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Elliptic flow coefficients from RHIC data
Hirano et al. (‘09)
Ideal hydro Glauber1st order
Viscosity
Eq. of state
theoretical prediction experimental data
Lattice-based
Ideal hydro works… maybe
Initial condition
*EoS based on lattice QCD results
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Elliptic flow coefficients from RHIC data
Viscous hydro in QGP plays important role in reducing v2
Hirano et al. (‘09)
Ideal hydro Glauber
Viscosity
Eq. of state
Initial condition
theoretical prediction experimental data
CGCLattice-based
*Gluons in fast nuclei may form color glass condensate (CGC)
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Introduction Formalism of viscous hydro is not settled yet:
1. Form of viscous hydro equations
2. Treatment of conserved currents
3. Treatment of multi-component systems
Fixing the equations is essential in fine-tuning viscosity from experimental data
# of conserved currents # of particle speciesbaryon number, strangeness, etc. pion, proton, quarks, gluons,
etc.
Low-energy ion collisions are planned at FAIR (GSI) & NICA (JINR)
Multiple conserved currents?
We need to construct a firm framework of viscous hydro
Song & Heinz (‘08)
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Introduction Categorization of relativistic systems
Number of components
Types of interactions
Single component with binary collisions
Israel & Stewart (‘79), etc…
Multi-components with binary collisionsPrakash et al. (‘91)
Single component with inelastic scatterings
(-)
Multi-components with inelastic scatteringsMonnai & Hirano (‘10)
QGP/hadronic gas at heavy ion collisions
Cf.
etc.
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Overview
Energy-momentum conservationCharge conservationsLaw of increasing entropy
START
GOAL (constitutive eqs.)
Onsager reciprocal relations: satisfied
Moment equations,
Generalized Grad’s moment method
, , ,
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Thermodynamic Quantities Tensor decompositions by flow
where is the projection operator
10+4N dissipative currents2+N equilibrium quantities
*Stability conditions should be considered afterward
Energy density deviation:Bulk pressure:
Energy current:Shear stress tensor:
J-th charge density dev.:J-th charge current:
Energy density:Hydrostatic pressure:
J-th charge density:
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Relativistic Hydrodynamics Ideal hydrodynamics
Viscous hydrodynamics
, , ,Conservation laws ( 4+N ) + EoS(1)Unknowns ( 5+N) , ,
We derive the equations from the law of increasing entropy
0th order theory1st order theory2nd order theory
ideal; no entropy production linear response; acausalrelaxation effects; causal
Additional unknowns ( 10+4N ) , , , , , !?Constitutive equations
“perturbation” from equilibrium
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Second Order Theory Kinetic expressions with distribution function :
Conventional formalism
Not extendable for multi-component/conserved current systems
one-component, elastic scattering
Israel & Stewart (‘79)
: degeneracy: conserved charge number
Dissipative currents (14) , , , , ,Moment equations (10)
frame fixing, stability conditions
(9) (9)?
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Extended Second Order Theory Moment equations
Expressions of andDetermined through the 2nd law of thermodynamics
Unknowns (10+4N) ,
Moment eqs. (10+4N),
New eqs. introduced
All viscous quantities determined in arbitrary frame
where
Off-equilibrium distribution is needed
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Extended Second Order Theory Moment expansion
*Grad’s 14-moment method extended for multi-conserved current systems so that it is consistent with Onsager reciprocal relations
Dissipative currents Viscous distortion tensor & vector
Moment equations, ,, ,
,,
Semi-positive definite condition
Matching matrices for dfi
10+4N unknowns , are determined in self-consistency conditions
The entropy production is expressed in terms of and
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Results 2nd order constitutive equations for systems with
multi-components and multi-conserved currentsBulk pressure
1st order terms
: relaxation times, : 1st, 2nd order transport coefficients
2nd order terms
relaxation
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Results (Cont’d)Energy current
1st order terms
2nd order terms
relaxation
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Results (Cont’d)J-th charge current
1st order terms
2nd order terms
relaxation
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Onsager Cross Effects 1st order terms
VectorDufour effect
Soret effect
potato
Thermal gradient
Permeation of ingredients
soup
Chemical diffusion caused by thermal gradient (Soret effect)
Cool down once – for cooking tasty oden (Japanese pot-au-feu)
It may well be important in our relativistic soup of quarks and gluons
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Results (Cont’d)Shear stress tensor
Our results in the limit of single component/conserved current
1st order terms2nd order terms
Consistent with other results based onAdS/CFT approachRenormalization group methodGrad’s 14-moment method Betz et al. (‘09)
Baier et al. (‘08)Tsumura and Kunihiro (‘09)
relaxation
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Discussion Comparison with AdS/CFT+phenomenological approach
Comparison with Renormalization group approach
• Our approach goes beyond the limit of conformal theory • Vorticity-vorticity terms do not appear in kinetic theory
Baier et al. (‘08)
Tsumura & Kunihiro (‘09)
• Consistent, but vorticity terms need further checking as some are added in their recent revision
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Discussion Comparison with Grad’s 14-moment approach
• The form of their equations are consistent with that of ours• Multiple conserved currents are not supported in 14-moment method
Betz et al. (‘09)
Consistency with other approaches suggest our multi-component/conserved current formalism is a natural extension
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Summary and Outlook We formulated generalized 2nd order theory from the entropy
production w/o violating causality1. Multi-component systems with multiple conserved currents
Inelastic scattering (e.g. pair creation/annihilation) implied
2. Frame independentIndependent equations for energy and charge currents
3. Onsager reciprocal relations ( 1st order theory)Justifies the moment expansion
Future prospects include applications to…• Hydrodynamic modeling of Quark-gluon plasma at relativistic
heavy ion collisions• Cosmological fluid etc…
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
The End Thank you for listening!
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
The Law of Increasing Entropy Linear response theory
Entropy production
: transport coefficient matrix (symmetric; semi-positive definite)
: dissipative current : thermodynamic force
Theorem: Symmetric matrices can be diagonalized with orthogonal matrix
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Thermodynamic Stability Maximum entropy state condition
- Stability condition (1st order)
- Stability condition (2nd order) Preserved for any
*Stability conditions are NOT the same as the law of increasing entropy
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First Order Limits 2nd order constitutive equations
transport coefficients(symmetric)
thermodynamics forces(2nd order)
1st order theory is recovered in the equilibrium limit
Onsager reciprocal relations are satisfied
Equilibrium limit
thermodynamic forces(Navier-Stokes)
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Hydrodynamic modeling of heavy ion collisions for RHIC
particles
hadronic phase
QGP phase
Freezeout surface Σ
Pre-equilibrium
Hydrodynamic picture
CGC/glasma picture?
Hadronic cascade picture
Initial condition
Hydro to particles
t
z
t
Initial condition Hydrodynamic model requires
Equation of stateViscosityHadronization
1st order phase transition, crossover(lattice), etc. Ideal hydro, viscous hydro JAM, UrQMD, etc.
Glauber, color glass condensate, etc.
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Introduction Relativistic hydrodynamics
Macroscopic theory defined on (3+1)-D spacetime
Flow (vector field)
Temperature (scalar field)
Chemical potentials (scalar fields)
Physics should be described by the macroscopic fields only
Gradient in the fields: thermodynamic forceResponse to the gradients: dissipative current
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Distortion of distribution Express in terms of dissipative currents
*Grad’s 14-moment method extended for multi-conserved current systems (Consistent with Onsager reciprocal relations)
Fix and through matching
Viscous distortion tensor & vector
Dissipative currents, ,, ,
,,
: Matching matrices
Moment expansion with 10+4N unknowns ,
10+4N (macroscopic) self-consistency conditions
,
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Second Order Equations Entropy production
Constitutive equations
Semi-positive definite condition
: symmetric, semi-positive definite matrices
Dissipative currents Viscous distortion tensor & vector
Moment equations, ,, ,
,,
Semi-positive definite condition
Matching matrices for dfi
Viscous distortion tensor & vector
Moment equations
,
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Discussion Comparison with AdS/CFT+phenomenological approach
• Our approach goes beyond the limit of conformal theory • Vorticity-vorticity terms do not appear in kinetic theory
Shear stress tensor in conformal limit, no charge current
Mostly consistent w ideal hydro relation
Baier et al. (‘08)
(Our equations)
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Discussion Comparison with Renormalization group approach
in energy frame, in single component/conserved current system
Form of the equations agrees with our equations in the single component & conserved current limit w/o vorticity
Tsumura & Kunihiro (‘09)
Note: Vorticity terms added to their equations in recent revision
(Our equations)
A power point template created by Akihiko MonnaiAkihiko Monnai (The University of Tokyo) , Hot Quarks 2010, La Londe-Les-Maures, France, Jul. 25th 2010
Discussion Comparison with Grad’s 14-momemt approach
Form of the equations agrees with ours in the single component & conserved current limit
Betz et al. (‘09)
*Ideal hydro relations in use for comparison
Consistency with other approaches suggest our multi-component/conserved current formalism is a natural extension
in energy frame, in single component/conserved current system
(Our equations)