Pseudorapidity dependence of anisotropic flows in relativistic heavy-ion collisions

• Published in: Physics letters. B Vol. 605; no. 1-2; pp. 95 - 100
• Main Authors: Chen, Lie-Wen, Greco, Vincenzo, Ko, Che Ming, Kolb, Peter F.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 06.01.2005; Elsevier Science
• Subjects: Exact sciences and technology; Monte carlo simulations; Nuclear physics; Nuclear reactions: general; Nuclear reactions: specific reactions; Nuclear-reaction models and methods; Physics; Relativistic heavy-ion reactions (collisions induced by light ions studied to calibrate relativistic heavy ion collisions, should be classified under both 001b20e75 and the 001b10c ou 001b20e category appropriate to the light ions); 24.10.Lx; 25.75.Ld; Hadrons; Heavy ions; Partons; Antiquark; Ion collisions; Models; Quarks; Cross sections
• ISSN: 0370-2693; 1873-2445
• DOI: 10.1016/j.physletb.2004.11.017

The pseudorapidity dependence of anisotropic flows v1, v2, v3 and v4 of charged hadrons in heavy-ion collisions at the relativistic heavy-ion collider is studied in a multi-phase transport model. We find that while the string melting scenario, in which hadrons that are expected to be formed from initial strings are converted to their valence quarks and antiquarks, can explain the measured pT-dependence of v2 and v4 of charged hadrons at midrapidity with a parton scattering cross section of about 10 mb, the scenario without string melting reproduces better the recent data on v1 and v2 of charged hadrons at large pseudorapidity in Au+Au collisions at s=200AGeV. Our results thus suggest that a partonic matter is formed during early stage of relativistic heavy-ion collisions only around midrapidity and that strings remain dominant at large rapidities. The pT-dependence of v1, v2, v3 and v4 for charged hadrons at forward pseudorapidity is also predicted, and we find that while v1 and v2 are appreciable at large pseudorapidity the higher-order anisotropic flows v3 and v4 are essentially zero.