Low Energy Spectral Index and evolution of Quasi-thermal Photosphere Emission of Gamma-Ray Bursts
arXiv:1402.5364 · doi:10.1088/0004-637X/785/2/112
Abstract
Recent observations by the Fermi satellite suggest that a photosphere emission component is contributing to the observed spectrum of many GRBs. One important question is whether the photosphere component can interpret the typical ``Band'' function of GRBs with a typical low energy photon spectral index . We perform a detailed study of the photosphere emission spectrum by progressively introducing several physical ingredients previously not fully incorporated, including the probability distribution of the location of a dynamically evolving photosphere, superposition of emission from an equal-arrival-time ``volume'' in a continuous wind, the evolution of optical depth of a wind with finite but evolving outer boundary, as well as the effect of different top-hat wind luminosity () profiles. By assuming a co-moving blackbody spectrum emerging from the photosphere, we find that for an outflow with a constant or increasing , the low-energy spectrum below the peak energy (), can be modified to (). A softer () or flat () spectrum can be obtained during the decreasing phase or high-latitude-emission-dominated phase. We also study the evolution of as a function of wind and photosphere luminosity in this photosphere model. An tracking pattern can be reproduced if a certain positive dependence between the dimensionless entropy and is introduced. However, the hard-to-soft evolution pattern cannot be reproduced unless a contrived condition is invoked. In order to interpret the Band spectrum, a more complicated photosphere model or a different energy dissipation and radiation mechanism are needed.
Accepted by ApJ, 15 pages, 17 figures
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