伽玛暴(Gamma-Ray Burst)笔记。记录有关伽玛暴的新文章,另外也包括看的老文章、自己的想法、以及跟天文相关的一些东西。 Feel free to leave me a message by comments or by email.

星期三, 五月 28, 2008

Salvaterra 2008 长暴函数存在演化的证据

主要内容:
“GRBs were more luminous in the past as we see them today.”什么意思?

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文章信息:

· arXiv e-print (arXiv:0805.4104)
· References in the Article
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Title:
Evidence for Luminosity Evolution of Long Gamma-ray Bursts in Swift Data
Authors:
Salvaterra, R.; Guidorzi, C.; Campana, S.; Chincarini, G.; Tagliaferri, G.
Publication:
eprint arXiv:0805.4104
Publication Date:
05/2008
Origin:
ARXIV
Keywords:
Astrophysics
Comment:
5 pages, 2 figures, submitted to MNRAS
Bibliographic Code:
2008arXiv0805.4104S

Abstract

We compute the luminosity function (LF) and the formation rate of long gamma ray bursts (GRBs) by fitting the observed differential peak flux distribution obtained by the BATSE satellite in two different scenarios: i) the GRB luminosity evolves with redshift and ii) GRBs form preferentially in low-metallicity environments. In both cases, model predictions are consistent with the Swift number counts and with the number of detections at z>2.5 and z>3.5. To discriminate between the two evolutionary scenarios, we compare the model results with the number of luminous bursts (i.e. with isotropic peak luminosity in excess of 10^53 erg s^-1) detected by Swift in its first three years of mission. Our sample conservatively contains only bursts with good redshift determination and measured peak energy. We find that models in which GRBs are characterised by a constant LF are ruled out, underproducing the number of luminous GRBs. Only for a metallicity threshold for GRB formation as low as 1/10 \Zsun, the model is marginally consistent with the observed number of bright GRBs. Using these new constraints, we derive robust upper limits on the bright-end of the GRB LF, showing that this can not be steeper than ~2.5. In conclusion, we find that available Swift observations (both the number of high-z GRBs and of bright GRBs) point to a scenario in which GRBs were more luminous in the past as we see them today.
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