Abstract

Azimuthal distributions of radial velocities of charged hadrons produced in nucleus-nucleus (AB) collisions are compared with the corresponding azimuthal distribution of charged hadron multiplicity in the framework of a multiphase transport (AMPT) model at two different collision energies. The mean radial velocity seems to be a good probe for studying radial expansion. While the anisotropic parts of the distributions indicate a kind of collective nature in the radial expansion of the intermediate “fireball,” their isotropic parts characterize a thermal motion. The present investigation is carried out keeping the upcoming Compressed Baryonic Matter (CBM) experiment to be held at the Facility for Antiproton and Ion Research (FAIR) in mind. As far as high-energy heavy-ion interactions are concerned, CBM will supplement the Relativistic Heavy-Ion Collider (RHIC) and Large Hadron Collider (LHC) experiments. In this context our simulation results at high baryochemical potential would be interesting, when scrutinized from the perspective of an almost baryon-free environment achieved at RHIC and LHC.

Highlights

  • When two heavy nuclei collide with each other at highenergy it is expected that a color deconfined state composed of strongly coupled quarks and gluons is formed

  • The study is based on the azimuthal distributions of total transverse velocity, mean transverse velocity, and multiplicity of charged hadrons produced in Au + Au collisions at Elab = 10 A GeV and 40 A GeV

  • We note that in our simulation results the azimuthal anisotropy of the final state particles is predominantly due to the asymmetry of particle multiplicity distribution, and only a small fraction of this asymmetry is due to kinematic reasons

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Summary

Introduction

When two heavy nuclei collide with each other at highenergy it is expected that a color deconfined state composed of strongly coupled quarks and gluons is formed. Of all the efforts in this regard, the study on the emission of final state particles with respect to the reaction plane of an AB collision, a plane spanned by the beam direction and the impact parameter vector, has been a popular technique that can characterize the thermodynamic and hydrodynamic properties of the QGP matter [3, 4]. In this technique the Fourier decomposition of the anisotropic azimuthal distribution has been widely employed to explore the collective behavior of the final state particles.

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