4.5 Article

Possible octupole deformation of 208Pb and the ultracentral v2 to v3 puzzle

Journal

PHYSICAL REVIEW C
Volume 102, Issue 5, Pages -

Publisher

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevC.102.054905

Keywords

-

Funding

  1. US-DOE Nuclear Science Grant [DE-SC0019175]
  2. Alfred P. Sloan Foundation
  3. Illinois Campus Cluster
  4. University of Illinois at Urbana-Champaign
  5. FAPESP [2016/24029-6, 2017/05685-2, 2018/24720-6]
  6. project INCT-FNA [464898/2014-5]
  7. U.S. Department of Energy (DOE) [DE-SC0019175] Funding Source: U.S. Department of Energy (DOE)

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Recent measurements have established the sensitivity of ultracentral heavy-ion collisions to the deformation parameters of nonspherical nuclei. In the case of Xe-129 collisions, a quadrupole deformation of the nuclear profile led to an enhancement of elliptic flow in the most central collisions. In Pb-208 collisions a discrepancy exists in similar centralities, where either elliptic flow is overpredicted or triangular flow is underpredicted by hydrodynamic models; this is known as the v(2)-to-v(3) puzzle in ultracentral collisions. Motivated by low-energy nuclear structure calculations, we consider the possibility that Pb-208 nuclei could have a pear-shape deformation (octupole), which has the effect of increasing triangular flow in central PbPb collisions. Using the recent data from ALICE and ATLAS, we reexamine the v(2)-to-v(3) puzzle in ultracentral collisions, including new constraints from recent measurements of the triangular cumulant ratio v(3){4}/v(3){2} and comparing two different hydrodynamic models. We find that while an octupole deformation would slightly improve the ratio between v(2) and v(3), it is at the expense of a significantly worse triangular flow cumulant ratio. In fact, the latter observable prefers no octupole deformation, with beta(3) less than or similar to 0.0375 for Pb-208, and is therefore consistent with the expectation for a doubly-magic nucleus even at top collider energies. The v(2)-to-v(3) puzzle remains a challenge for hydrodynamic models.

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