Early dissipation and viscosity
arXiv:0804.3952 · doi:10.1088/0954-3899/35/10/104148
Abstract
We consider dissipative phenomena due to the relaxation of an initial anisotropic local pressure in the fireball created in relativistic heavy-ion collisions, both for the Bjorken boost-invariant case and for the azimuthally symmetric radial expansion with boost-invariance. The resulting increase of the entropy can be counterbalanced by a suitable retuning of the initial temperature. An increase of the transverse collective flow is observed. The influence of the shear viscosity on the longitudinal expansion is also studied. Viscosity reduces the cooling rate from the longitudinal work and counteracts the pressure gradients that accelerate the longitudinal flow.
Presented at Quark Matter 2008, February 4-10, 2008, Jaipur India
References in corpus (15)
- Viscosity in Strongly Interacting Quantum Field Theories from Black Hole Physics
- Viscosity Information from Relativistic Nuclear Collisions: How Perfect is the Fluid Observed at RHIC?
- Flow at the SPS and RHIC as a Quark Gluon Plasma Signature
- The Effect of Shear Viscosity on Spectra, Elliptic Flow, and HBT Radii
- Suppression of elliptic flow in a minimally viscous quark-gluon plasma
- Causal Theories of Dissipative Relativistic Fluid Dynamics for Nuclear Collisions
- Dynamics of Hot Bulk QCD Matter: from the Quark-Gluon Plasma to Hadronic Freeze-Out
- Second Order Dissipative Fluid Dynamics for Ultra-Relativistic Nuclear Collisions
- Charged Meson Rapidity Distributions in central Au+Au Collisions at sqrt(s_nn) = 200 GeV
- Causal Viscous Hydrodynamics for Central Heavy-Ion Collisions
- Dissipative hydrodynamics in 2+1 dimension
- Elliptic Flow from a Transversally Thermalized Fireball
- Longitudinal fluid dynamics for ultrarelativistic heavy-ion collisions
- Viscous evolution of the rapidity distribution of matter created in relativistic heavy-ion collisions
- Early evolution of transversally thermalized partons