2007ApJ...670..565L


Query : 2007ApJ...670..565L

2007ApJ...670..565L - Astrophys. J., 670, 565-583 (2007/November-3)

A comprehensive analysis of Swift XRT data. II. Diverse physical origins of the shallow decay segment.

LIANG E.-W., ZHANG B.-B. and ZHANG B.

Abstract (from CDS):

The origin of the shallow decay segment in Swift XRT light curves remains a puzzle. We analyze the properties of this segment with a sample of 53 long Swift GRBs detected before 2007 February. We show that the distributions of the sample's characteristics are lognormal or normal, and its isotropic X-ray energy (Eiso,X) is linearly correlated with the prompt gamma-ray energy but with a steeper photon spectrum, aside from some X-ray flashes. No significant spectral evolution is observed from this phase to the following phase, and the latter is usually consistent with external-shock models, implying that the shallow decay is also of external-shock origin, likely a refreshed external shock. Within the refreshed-shock model, the data are generally consistent with a roughly constant injection luminosity up to the end of this phase, tb. A positive correlation between Eiso,X and tb also favors this scenario. Among the 13 bursts that have well-sampled optical light curves, six have an optical break around tb and the breaks are consistent with being achromatic. However, the other seven either do not show an optical break or have a break at an epoch different from tb. This raises a concern for the energy injection scenario, suggesting that the optical and X-ray emission may not be the same component, at least for some bursts. There are four significant outliers in the sample, GRBs 060413, 060522, 060607A, and 070110. The shallow decay phase in these bursts is immediately followed by a very steep decay after tb, which is inconsistent with any external-shock model. The optical data for these bursts evolve independently from the X-ray data. These X-ray plateaus likely have an internal origin and demand continuous operation of a long-term central engine. We conclude that the observed shallow decay phase likely has diverse physical origins.

Abstract Copyright: ∼

Journal keyword(s): Gamma Rays: Bursts - Radiation Mechanisms: Nonthermal - X-Rays: General

Simbad objects: 53

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Number of rows : 53
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 GRB 070110 gB 00 03 39.270 -52 58 27.00 21.8 21.9 21.2     ~ 220 0
2 GRB 060912 gB 00 21 08.160 +20 58 17.80 17.61   17.56     ~ 42 0
3 GRB 060708 gB 00 31 13.850 -33 45 32.40 19.07 19.79 17.37     ~ 109 0
4 GRB 060719 gB 01 13 43.380 -48 22 55.09           ~ 107 0
5 GRB 060908 gB 02 07 18.360 +00 20 31.20 16.99 18.34 16.85     ~ 217 0
6 GRB 070129 gB 02 28 00.940 +11 41 04.00       21.3   ~ 120 0
7 GRB 060906 gB 02 43 00.900 +30 21 42.12     19.84     ~ 147 0
8 GRB 060306 gB 02 44 22.830 -02 08 55.00           ~ 119 0
9 GRB 050318 gB 03 18 51.000 -46 23 43.61 18.10 18.68 17.58     ~ 189 0
10 GRB 050822 gB 03 24 27.240 -46 01 59.20     20.82     ~ 115 0
11 GRB 060210 gB 03 50 57.370 +27 01 34.40   20.27       ~ 275 0
12 GRB 060124 gB 05 08 25.900 +69 44 26.98   18.91 17.35     ~ 280 0
13 GRB 060507 gB 05 59 50.520 +75 14 55.88 20.52         ~ 40 0
14 GRB 060729 gB 06 21 31.850 -62 22 12.69           ~ 303 0
15 GRB 060510A gB 06 23 27.980 -01 09 46.20 18.19   18.45     ~ 58 0
16 GRB 061202 gB 07 02 06.190 -74 41 54.91           ~ 83 0
17 GRB 060813 gB 07 27 35.380 -29 50 49.40           ~ 62 0
18 GRB 060804 gB 07 28 49.360 -27 12 56.71 18.74 18.94 17.32     ~ 41 0
19 GRB 060428A gB 08 14 10.840 -37 10 11.70     19.97     ~ 54 0
20 GRB 051016B gB 08 48 27.810 +13 39 20.00 20.45         ~ 153 0
21 GRB 050505 gB 09 27 03.300 +30 16 23.70     20.74     ~ 206 0
22 GRB 061021 gB 09 40 36.120 -21 57 05.40 18.21 19.20 16.82     ~ 160 0
23 GRB 060108 gB 09 48 01.980 +31 55 08.59           ~ 107 0
24 GRB 061121 gB 09 48 54.570 -13 11 42.68 17.19 17.71 17.02     ~ 350 0
25 GRB 050319 gB 10 16 47.900 +43 32 53.80   18.02 17.01     ~ 274 0
26 GRB 060323 gB 11 37 44.910 +50 00 33.49           ~ 50 0
27 GRB 050416 gB 12 33 54.600 +21 03 26.69     19.12     ~ 300 1
28 GRB 050726 gB 13 20 11.900 -32 03 51.89     17.58     ~ 70 0
29 GRB 051008 gB 13 31 28.100 +42 08 05.01 17.06   14.11     ~ 90 0
30 GRB 050801 gB 13 36 35.000 -21 55 41.00 15.03 15.82 15.46     ~ 164 0
31 GRB 060204B gB 14 07 14.900 +27 40 36.40           ~ 93 0
32 GRB 050802 gB 14 37 05.820 +27 47 12.62 16.85 17.38 16.97     ~ 186 0
33 GRB 050128 gB 14 38 17.750 -34 45 55.61           ~ 68 0
34 GRB 060805A gB 14 43 43.480 +12 35 11.40           ~ 65 0
35 GRB 060814 gB 14 45 21.480 +20 35 11.80           ~ 241 0
36 GRB 060714 gB 15 11 26.450 -06 33 58.30   20.21 18.54     ~ 209 0
37 GRB 060526 gB 15 31 18.360 +00 17 04.90   18.31 17.16     ~ 288 0
38 GRB 060502A gB 16 03 42.480 +66 36 02.49     18.65     ~ 143 0
39 GRB 050401 gB 16 31 28.84 +02 11 14.5           ~ 348 0
40 GRB 060807 gB 16 50 02.600 +31 35 30.70           ~ 61 0
41 GRB 060109 gB 18 50 43.650 +31 59 26.40           ~ 52 0
42 GRB 060413 gB 19 25 07.850 +13 45 29.90           ~ 69 0
43 GRB 060105 gB 19 50 00.680 +46 20 55.40           ~ 87 0
44 GRB 050315 gB 20 25 54.100 -42 36 02.19           ~ 225 0
45 GRB 050713B gB 20 31 15.570 +60 56 43.70           ~ 72 0
46 GRB 060614 G 21 23 32.140 -53 01 36.10           ~ 714 0
47 GRB 060522 gB 21 31 44.850 +02 53 10.80           ~ 140 0
48 GRB 060607 gB 21 58 50.400 -22 29 46.70 18.49 16.67 15.09     ~ 318 0
49 GRB 051109A gB 22 01 15.320 +40 49 23.70   20.09 20.14     ~ 190 0
50 GRB 060604 gB 22 28 55.010 -10 54 55.80 20.34 20.31       ~ 134 0
51 GRB 050803 gB 23 22 37.910 +05 47 09.00           ~ 127 0
52 GRB 060707 gB 23 48 19.000 -17 54 17.00     19.79     ~ 170 0
53 GRB 061222A gB 23 53 03.419 +46 31 58.60           ~ 177 0

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