4.7 Article

The origin of the photospheric emission of GRB 220426A

Journal

MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 517, Issue 2, Pages 2088-2102

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/mnras/stac2764

Keywords

radiation mechanisms: thermal; radiative transfer; scattering; gamma-ray burst: individual

Funding

  1. National Program on Key Research and Development Project [2021YFA0718500]
  2. International Partnership Program of Chinese Academy of Sciences [113111KYSB20190020]
  3. Horizontal Subject [Y990FWG]

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Researchers performed several tests to speculate the origin of the photospheric emission in GRB 220426A, and concluded that a hybrid outflow is the most likely source, while other possible origins such as non-dissipative hybrid outflow or magnetic reconnection are not well-supported.
GRB 220426A is a bright gamma-ray burst (GRB) dominated by the photospheric emission. We perform several tests to speculate the origin of this photospheric emission. The dimensionless entropy eta is large, which is not usual if we assume that it is a pure hot fireball launched by neutrino-antineutrino annihilation mechanism only. Moreover, the outflow has larger eta with lower luminosity L in the first few seconds, so that the trend of time-resolved eta - L can not be described as a monotonically positive correlation between eta and L. A hybrid outflow with almost completely thermalized Poynting flux could account for the quasi-thermal spectrum as well as large eta. More importantly, the existence of magnetic field could affect the proton density and neutron-proton coupling effect, so that it could account for the observed trend of time-resolved eta - L. The other origins for the photospheric emission, such as non-dissipative hybrid outflow or magnetic reconnection, are not supported because their radiation efficiencies are low, which is not consistent with non-detection of the afterglow for GRB 220426A. Therefore, we think the hybrid outflow may be the most likely origin.

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