Anisotropic flow of Pb+Pb s_(NN)^(1/2)= 5.02 TeV from a multi-phase transport model  

作　　者：冯照 黄光明 刘峰 

机构地区：[1]Key Laboratory of Quark and Lepton Physics (MOE) and Institute of Particle Physics,Central China Normal University, Wuhan 430079, China

出　　处：《Chinese Physics C》2017年第2期101-104,共4页中国物理C（英文版）

基　　金：Supported by National Natural Science Foundation of China(11221504,11420101004);MOST of China 973(2015CB856901)

摘　　要：Anisotropic flow is an important observable in the study of the quark-gluon plasma that is expected to be formed in heavy-ion collisions. With a multiphase transport（AMPT） model we investigate the elliptic（v2）,triangular（v3）, and quadrangular（v4） flow of charged particles in Pb＋Pb collisions at √sNN= 5.02 TeV. We then compare our flow results with the published ALICE flow results. We find our AMPT simulated results are consistent with ALICE experimental data.Anisotropic flow is an important observable in the study of the quark-gluon plasma that is expected to be formed in heavy-ion collisions. With a multiphase transport（AMPT） model we investigate the elliptic（v2）,triangular（v3）, and quadrangular（v4） flow of charged particles in Pb＋Pb collisions at √sNN= 5.02 TeV. We then compare our flow results with the published ALICE flow results. We find our AMPT simulated results are consistent with ALICE experimental data.

关 键 词：azimuthal anisotropy anisotropic flow ALICE Pb＋Pb 5.02 Te V AMPT 

分 类 号：O571.6[理学—粒子物理与原子核物理]