A&A 484, 143-157 (2008)
DOI: 10.1051/0004-6361:20078399
S. Foley1 - S. McGlynn1 - L. Hanlon1 - S. McBreen2 - B. McBreen1
1 - UCD School of Physics, University College Dublin, Dublin 4, Ireland
2 - Max-Planck-Institut für extraterrestrische Physik, 85748 Garching, Germany
Received 2 August 2007 / Accepted 4 March 2008
Abstract
Context. INTEGRAL has two sensitive gamma-ray instruments that have detected and localised 47 gamma-ray bursts (GRBs) from its launch in October 2002 up to July 2007.
Aims. We present the spectral, spatial, and temporal properties of the bursts in the INTEGRAL GRB catalogue using data from the imager, IBIS, and spectrometer, SPI.
Methods. Spectral properties of the GRBs are determined using power-law and, where appropriate, Band model and quasithermal model fits to the prompt emission. Spectral lags, i.e. the time delay in the arrival of low-energy -rays with respect to high-energy
-rays, are measured for 31 of the GRBs.
Results. The photon index distribution of power-law fits to the prompt emission spectra is presented and is consistent with that obtained by Swift. The peak flux distribution shows that INTEGRAL detects proportionally more weak GRBs than Swift because of its higher sensitivity in a smaller field of view. The all-sky rate of GRBs above
is
in the fully coded field of view of IBIS. Two groups are identified in the spectral lag distribution of INTEGRAL GRBs, one with short lags <
(between 25-50 keV and 50-300 keV) and one with long lags >
.
Most of the long-lag GRBs are inferred to have low redshifts because of their long spectral lags, their tendency to have low peak energies, and their faint optical and X-ray afterglows. They are mainly observed in the direction of the supergalactic plane with a quadrupole moment of Q=-0.225
0.090 and hence reflect the local large-scale structure of the Universe.
Conclusions. The spectral, spatial, and temporal properties of the 47 GRBs in the INTEGRAL catalogue are presented and compared with the results from other missions. The rate of long-lag GRBs with inferred low luminosity is 25% of type Ib/c supernovae. Some of these bursts could be produced by the collapse of a massive star without a supernova. Alternatively, they could result from a different progenitor, such as the merger of two white dwarfs or a white dwarf with a neutron star or black hole, possibly in the cluster environment without a host galaxy.
Key words: gamma rays: bursts - gamma rays: observations
The prompt emission of gamma-ray bursts provides valuable insight into the mechanisms from which these extremely explosive events originate. Their short durations
and highly variable temporal structures provide constraints on the
physics of the central engine powering the burst. A number of GRB reviews have been
published (e.g. Zhang & Mészáros 2004; Piran 2005; Mészáros 2006). In recent years, the advent
of missions such as the Compton Gamma-Ray Observatory
(CGRO) (Fishman & Meegan 1995), along with the improved imaging capabilities of missions such as
BeppoSAX (Boella et al. 1997), HETE II (Sakamoto et al. 2005), INTEGRAL (Winkler et al. 2003), and Swift (Gehrels et al. 2004), has led to the precise localisations of GRBs and enabled rapid multi-wavelength follow-up observations. The X-ray, optical and
radio afterglow detections are listed in Table 1 for a total of 423 GRBs well localised by these missions between July 1996 and July 2007, showing in particular the observed
number of afterglows based on INTEGRAL GRB detections. The data are taken from the webpage maintained by Jochen Greiner.
Table 1:
Afterglow detections for GRBs localised by recent -ray missions
between July 1996 and July 2007.
There are two main -ray instruments on board INTEGRAL, namely
IBIS (Ubertini et al. 2003) and SPI (Vedrenne et al. 2003), optimised for high-resolution imaging and spectroscopy of the
-ray sky, respectively. The IBIS instrument is comprised of two separate layers of dectectors, ISGRI in the 15 keV-1 MeV energy range (Lebrun et al. 2003), and PICsIT
in the 180 keV-10 MeV energy range (Labanti et al. 2003). IBIS/ISGRI has 16 384 CdTe detectors, located 3.4 m from a tungsten mask which projects a shadowgram on the detector plane. Maps of the sky are reconstructed by decoding the shadowgram with the mask pattern. IBIS has a fully coded field
of view (FCFoV) of
and a partially coded field of
view (PCFoV) of
at 50% coding and
at zero coding. SPI consists of 19 hexagonal germanium (Ge) detectors covering the energy range 20 keV-8 MeV with high energy resolution of 2.5 keV at 1.3 MeV. A
coded mask is located 1.71 m above the detector plane for imaging
purposes, giving a
corner-to-corner FCFoV and a PCFoV of
.
The SPI and IBIS instruments are supported by
an optical camera (OMC, Mas-Hesse et al. 2003) and an X-ray monitor (JEM-X, Lund et al. 2003).
The INTEGRAL Burst Alert System
(IBAS, Mereghetti et al. 2003b) is an automatic ground-based system for the accurate localisation of GRBs and the rapid
distribution of GRB coordinates, providing, on average,
0.8 GRBs per month with an error radius of
3 arcmin. INTEGRAL has detected 46 long-duration GRBs (
s) and 1 short-duration GRB
(
s) between October 2002 and July 2007. INTEGRAL bursts of particular interest include the low-luminosity
GRB 031203 (Sazonov et al. 2004), the very intense
GRB 041219a (McBreen et al. 2006), a number of X-ray rich
GRBs such as GRB 040223 (McGlynn et al. 2005; Filliatre et al. 2006),
GRB 040403 (Mereghetti et al. 2005) and
GRB 040624 (Filliatre et al. 2006), and the short-duration GRB 070707 (McGlynn et al. 2008a).
In addition, Marcinkowski et al. (2006) have detected a bright, hard GRB outside the field of view using the ISGRI Compton mode. Spectroscopic redshifts have been determined for
four INTEGRAL GRBs, i.e. GRB 031203 at
z=0.1055 (Prochaska et al. 2004); GRB 050223 at z=0.584 (Pellizza et al. 2006); GRB 050525a at
z=0.606 (Foley et al. 2005) and GRB 050502a at
z=3.793 (Prochaska et al. 2005). Non-spectroscopic redshifts have been inferred for GRB 040812 (0.3 < z < 0.7, D'Avanzo et al. 2006) and GRB 040827 (0.5 < z < 1.7, de Luca et al. 2005). The low efficiency for measuring redshifts is partially due to the fact that INTEGRAL spends a large amount of observing time pointing towards the galactic plane.
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Figure 1: A selection of GRB lightcurves detected by the Anti-Coincidence Shield at photon energies >80 keV. |
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Gamma-ray burst continuum spectra are in most cases well
described by a smoothly broken power law in the 30 keV-2 MeV
energy range (Band et al. 1993). The -ray spectral shape as
predicted for optically thin synchrotron emission are two asymptotically
broken power laws but many GRBs are not consistent with this model and
it requires modification to fit the observed
spectra (e.g. Lloyd-Ronning & Petrosian 2002). It has been proposed that GRB spectra may contain a thermal
component (e.g. Ryde 2005; Kaneko et al. 2006; McBreen et al. 2006; Ghirlanda et al. 2003). The interpretation
of quasithermal emission as opposed to synchrotron emission
can provide an explanation for the observed spectral
characteristics within a more physical framework (e.g. Ryde et al. 2006; Rees & Mészáros 2005).
The time profiles of GRBs often exhibit a complex and unpredictable nature, displaying considerable diversity both in terms of structure and duration (Quilligan et al. 2002; McBreen et al. 2001). This makes them difficult to classify on the basis of temporal structure alone. One notable feature of GRB time profiles is the tendency for emission in a high-energy band to lead the arrival of photons in a low-energy band (e.g. Hakkila et al. 2008; McBreen et al. 2006; Norris et al. 2000; Wu & Fenimore 2000; Hakkila et al. 2007; Cheng et al. 1995; Bolmont et al. 2006). The energy-dependent lag allows the temporal and spectral properties of the GRB prompt -ray
emission to be combined in a single measurement. The typical lag values
measured for long-duration GRBs detected by the Burst and Transient Source Experiment (BATSE) between the 25-50 keV and 100-300 keV channels concentrate
100 ms (Norris et al. 2000). An anti-correlation between spectral lag and isotropic
peak luminosity was first observed by Norris et al. (2000), using 6 BATSE bursts
with measured redshifts. A similar trend is observed
between lag and luminosity for a number of Swift
GRBs of known redshift (Gehrels et al. 2006). However, there exist notable
outliers, in particular the ultra-low luminosity
bursts GRB 980425, GRB 031203 and GRB 060218, associated with the supernovae
SN 1998bw, SN 2003lw and SN 2006aj, respectively. Short bursts
(T90<2 s) have very small or negligible lags (Zhang et al. 2006a; Yi et al. 2006; Norris & Bonnell 2006) and relatively low peak luminosities and so do not lie on the correlation (Gehrels et al. 2006). On this basis, the spectral lag has been suggested by Donaghy et al. (2006) as one of the criteria to determine whether a burst is long or short. Pulse width and spectral lag are
strongly related, with wider pulses tending to have longer spectral
lags (Norris & Bonnell 2006). Relative spectral lags, defined as the ratio of spectral
lag to pulse width, have been found to have normal distributions
centering on
100 ms for long bursts (Zhang et al. 2006b) and
14 ms for
short GRBs (Zhang et al. 2006a). The
lag-luminosity and
-
(Amati et al. 2007) relationships can be used as distance indicators for GRBs (Schaefer 2007), provided the role of selection effects is understood and quantified (e.g. Butler et al. 2008).
The physical basis underlying spectral lags is not yet well
understood (Schaefer 2004). The observed lag of a burst is a direct consequence of its
spectral evolution because the peak of the
spectrum,
,
decays with time (Hafizi & Mochkovitch 2007; Kocevski & Liang 2003). The internal shock model allows for three possible sources of temporal variations in GRB pulses: cooling, hydrodynamics and
geometric angular effects. Cooling is unable to fully account for the time
lag since the synchrotron timescale is much shorter than the lag timescale (Wu & Fenimore 2000). It has been proposed that the lag-luminosity relation may arise kinematically, based on the
viewing angle at which the GRB jet is observed (Salmonson 2000). In this interpretation, a high-luminosity GRB with short spectral lag corresponds to a
jet with a small viewing angle, while a low-luminosity GRB with long
spectral lag corresponds to a jet with a large viewing angle (Ioka & Nakamura 2001). A correlation has also been observed between spectral lag (or luminosity) and jet-break time,
thereby connecting the prompt and afterglow phases of GRBs. This may
be understood in terms of a model in which the Lorentz factor decreases
away from the axis of the GRB jet (Salmonson & Galama 2002). The connection between spectral lag and the timescales involved in the hydrodynamic processes and radiative mechanisms of the burst has been discussed by Daigne & Mochkovitch (2003).
A subpopulation of local, faint, long-lag GRBs has been suggested
by Norris (2002) from a study of BATSE bursts, which implies that
events with low peak fluxes (
(50-300 keV)
0.25 ph cm-2 s-1) should be predominantly long-lag GRBs. The sensitivity of IBIS is such that bursts fainter than the BATSE limit can be well localised. In this paper we present the spectral, spatial and temporal lag properties of the complete sample of the 47 GRBs detected in the field of view
of IBIS and SPI up to July 2007. Section 2 describes the capabilities
of SPI's anti-coincidence shield as a GRB detector. The spectral and lag analyses are described in
Sect. 3 and results are presented in
Sect. 4. Sections 5 and 6 discuss the
significance of these results, which imply a large population of long-lag GRBs with low luminosities. The cosmological parameters adopted throughout the paper are H0 = 70 km s-1 Mpc-1,
,
.
All errors are quoted at the 1
confidence level.
In addition to SPI and IBIS, the Anti-Coincidence Shield (ACS) surrounding the SPI detectors works as a highly-sensitive GRB detector above 80 keV but lacks spatial and spectral
information (von Kienlin et al. 2003b). The ACS consists of 91 BGO crystals with a total mass of 512 kg surrounding SPI. It has a maximum sensitivity to GRBs at
from
the pointing direction and provides lightcurves in 50 ms intervals. The ACS detects GRBs at a rate of
1 every 2-3 days. A selection of GRBs detected with
SPI-ACS is shown in Fig. 1 using data taken from the publicly available catalogue of SPI-ACS GRBs
. Temporal analysis of a more complete sample is presented in Rau et al. (2005). The ACS is
used as part of the interplanetary network (Hurley et al. 2006).
Spectral analysis of the GRBs was performed using INTEGRAL's
Online Software Analysis version 5.1 available from the INTEGRAL Science Data Centre. The T90 duration (i.e.,
the time during which 5% to 95% of the GRB counts are
recorded) was determined for each GRB in the 20-200 keV energy range and the spectrum was
generated for that time interval. For cases in which the GRB
had a multi-peaked time profile, the GRB was divided into its
constituent pulses and a spectrum was generated for
each pulse to investigate evolution of the spectral
parameters during the burst.
Each GRB was fit by a simple power-law model, the Band
model and a quasithermal (combined power-law + blackbody)
model. Weak GRBs are best fit by a single
power-law model because the limited statistics are insufficient to
constrain any additional parameters. For brighter GRBs, the Band
model or combined power-law + blackbody fits usually result in an
improved value. The peak flux was measured over the
brightest 1 s time interval in the 20-200 keV energy range. The fluence of each GRB
was determined for the T90 interval in the 20-200 keV
energy range for the IBIS spectra, and the 20-200 keV and
20 keV-8 MeV energy ranges for the SPI spectra.
In order to measure the lag, background-subtracted lightcurves were extracted in three
energy bands comparable to those used with BATSE, namely 25-50 keV (Channel 1), 50-100 keV
(Channel 2) and 100-300 keV (Channel 3). The lag, ,
between two energy
channels was determined by computing the
cross-correlation function (CCF) between the two lightcurves
as a function of temporal lag as described by
Band (1997) and Norris et al. (2000). Assuming the time profiles in both energy
channels display sufficient similarity, the peak in the CCF
then corresponds to the time lag of the GRB between the two
energy channels in question. The lag was determined between Channels 1 and 2,
,
Channels 1 and 3,
,
and to account for those cases in which the signal
level in Channel 3 was insufficient to determine an accurate
lag, the counts in Channels 2 and 3 were combined and correlated with Channel 1 to give
.
In this paper, GRBs with
s are defined as long-lag.
The reliability of the cross-correlation technique was limited
primarily by the signal to noise ratio of the data. The faint
nature of many of the GRBs detected by INTEGRAL can result in a noisy CCF
with an ambiguous peak. A denoising technique was used to smooth the lightcurve while retaining the
structure of the burst. This technique involved filtering the signal to remove the high frequency components in order to produce a denoised lightcurve (Quilligan et al. 2002). The wavelet analysis was carried out on the weakest GRBs with
(20-200 keV)
using the wavelet toolbox in MATLAB. As an example, the lightcurves of GRB 070615 in the 25-50 keV and 50-300 keV energy bands are shown in Fig. 2a before and Fig. 2b after denoising. The
CCFs resulting from the raw data and denoised data are plotted in
Fig. 2c. The denoised data results in a smoother CCF peak and a more
significant correlation, while retaining the
position of the peak at a similar lag value to that measured with
the raw data. Six INTEGRAL GRBs were too weak for a reliable lag to be
determined using either the raw or denoised data.
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Figure 2: a) Raw and b) denoised lightcurves of GRB 070615 in the 25-50 keV (dark line) and 50-300 keV (light line) energy bands. c) Cross correlation functions and polynomial fits giving a lag of 0.40+0.15-0.25 and 0.40+0.15-0.20 for the raw and denoised lightcurve data, respectively. The dashed line represents a lag of 0 s. |
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The CCF was fit with a fourth order polynomial in
order to account for the asymmetry of the CCF (Norris et al. 2000).
The peak of the polynomial fit to the CCF was then taken to be the true lag
value. For each GRB, an average spectral
lag over the total burst duration was determined. For the cases in
which separate pulses could be clearly distinguished by eye,
spectral lags were measured for the individual pulses to investigate
the evolution of spectral lag during the burst. In
each case, the spectral lag was determined for regions of the
lightcurve above 10%, 30% and 50% of the peak count rate and over a
number of different lag ranges to ensure that consistent results were
obtained. The optimum lag range was taken to be that for which the CCF was concave
down but short enough that the CCF peak was well fit. Statistical errors
were calculated using a bootstrap method as described in Norris et al. (2000). This involves adding
Poissonian noise based on the observed counts to the
lightcurves in the different energy channels and re-computing
the CCF in 100 realisations for each burst. The 50th ranked
value is then the mean lag and the 16th and 84th ranked
values represent .
The lightcurve data was over-resolved by
a factor of 10 in order to compute the errors at a time resolution
less than the natural binning of the raw data.
The exposure map and spatial distribution of the 47 GRBs observed with IBIS are shown in galactic coordinates in Fig. 3 for the period from October 2002 to July 2007.
The burst distribution is significantly concentrated towards the galactic plane, reflecting the
direction in which the satellite is pointed. INTEGRAL spent 64% of its observing time in the half of the sky at galactic latitudes between .
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Figure 3: a) INTEGRAL exposure map in galactic coordinates from October 2002 up to July 2007 (contours in units of kiloseconds), showing the concentration of exposure in the direction of the galactic plane (Erik Kuulkers, private communication). b) Spatial distribution of 47 INTEGRAL GRBs detected between October 2002 and July 2007 in galactic coordinates. |
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Figure 4:
The off-axis angle distribution of the GRBs in the IBIS FoV as a function of peak flux (20-200 keV). The FCFoV is ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure 5: The cumulative log N-log P distribution of the 47 GRBs detected by IBIS, with peak flux P measured between 20-200 keV. The distribution is biased by the lower sensitivity of IBIS at large off-axis angles (Fig. 4). The small subset of 11 long-lag GRBs is shown separately. |
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Figure 6: T90 distribution of INTEGRAL GRBs (solid line) in comparison to that of BATSE (dashed line). The BATSE distribution is normalised to the peak of the INTEGRAL distribution for clarity. The BATSE data for 2041 GRBs is taken from the Current Catalog at http://www.batse.msfc.nasa.gov/batse/grb/catalog/current. |
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Table 2:
GRBs detected by INTEGRAL. The columns refer to (from left to
right): GRB; right ascension; declination; T90 duration; peak flux; fluence; photon index; /degrees of freedom (d.o.f.); afterglow detections in radio, R, infrared, IR, optical, O and X-ray, X. Peak fluxes, fluences and photon indices are given in the 20-200 keV energy range.
The properties of the 47 INTEGRAL GRBs are presented in
Tables 2 and 3. The coordinates and afterglow information are taken
from the webpage maintained by Jochen Greiner. The typical
size of the INTEGRAL error box is 3
.
GRB 060428c did not trigger IBAS but was discovered during subsequent analysis of INTEGRAL archival data (Grebenev & Chelovekov 2007). The spectral lag for each burst is presented in Table 4, with 11 GRBs having long lags (
s). The off-axis angle distribution of the GRBs in the IBIS FoV is given in Fig. 4. The bursts have preferentially higher peak fluxes at larger angles outside the FCFoV of IBIS due to the reduced sensitivity at lower coding levels. The log N-log P distribution is given in Fig. 5 for all IBIS GRBs and separately for the small subsample of 11 long-lag GRBs. The long-lag GRBs appear to form a separate population at low values of P. The T90 distribution of INTEGRAL GRBs is shown in
Fig. 6 and compared with the bimodal distribution for BATSE GRBs (Kouveliotou et al. 1993). There is reasonable agreement between the two distributions,
especially when the small number of INTEGRAL GRBs is taken
into account. The IBIS lightcurves of 43 INTEGRAL bursts are given in the Appendix in the 25-50 keV and 50-300 keV energy ranges. In general, the faint bursts have smooth, long-duration profiles with only one or two weak pulses.
Table 3:
IBIS and SPI spectral properties of GRBs for which Band and quasithermal (PL + BB) models are fit to spectra. Parameters quoted are low energy power-law index,
,
high energy power-law index,
,
and break
energy, E0, for Band model fits and temperature, kT and power-law index,
for quasithermal model fits.
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Figure 7:
a) IBIS ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure 8: Power-law photon index distribution for INTEGRAL GRBs detected between October 2002 and July 2007 (solid line) and Swift GRBs detected between November 2004 and July 2007 (dashed line), in the 20-200 keV and 15-150 keV energy bands, respectively. The Swift data for 238 GRBs is taken from http://swift.gsfc.nasa.gov/docs/swift/archive/grb_table.html. |
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Figure 9: Peak flux distribution for GRBs detected by INTEGRAL (20-200 keV, solid line) and Swift (15-150 keV, dashed line). The Swift data for 237 GRBs is taken from http://swift.gsfc.nasa.gov/docs/swift/archive/grb_table.html. |
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The spectral information given in Table 2 is obtained from the IBIS detector,
with the exception of GRB 041219a, GRB 050525a, GRB 060901 and GRB 061122 for
which the peak flux and fluence values are measured with SPI
in the 20-200 keV energy range due to telemetry gaps in the IBIS data (McBreen et al. 2006; McGlynn et al. 2008b). Limited spectral information is
available for GRB 021125 due to significant telemetry loss
while the satellite was in calibration mode (Malaguti et al. 2003). Data for
GRB 060930 and GRB 070311 are currently not publicly available and values shown are taken
from Gotz et al. (2006) and Mereghetti et al. (2007), respectively. Peak flux values
are integrated over the brightest 1 s time interval in the 20-200 keV energy band and fluence values are measured over the same energy range. Photon indices are given for a power-law fit to
the spectra in the 20-200 keV energy range. Spectral parameters obtained from IBIS and SPI spectra for which the Band model and quasithermal model are fit are listed in
Table 3. The values obtained from a combined IBIS and SPI spectral fit to GRB 060428c over the 20-400 keV energy range are taken from Grebenev & Chelovekov (2007). GRB 030131 and GRB 050502a were detected during a satellite slew so SPI spectral analysis was not possible for these bursts. A sample of INTEGRAL spectra is shown in Fig. 7.
The distribution of photon indices is shown in Fig. 8 for INTEGRAL and Swift GRBs for which a power-law model was fit to the spectral data in the 20-200 keV and 15-150 keV energy ranges, respectively. In comparison to Swift, INTEGRAL detects proportionally more soft GRBs with steeper power-law photon indices.
Figure 9 compares the peak flux (20-200 keV) distribution of
the GRBs observed by IBIS (solid line) to
the peak flux (15-150 keV) distribution of the GRBs detected by the BAT instrument on Swift. IBIS detects proportionally more
weak GRBs than Swift because of its better sensitivity within a FoV that is smaller by a factor of 12.
The spectral lag results are presented in Table 4. A positive spectral lag follows the usual convention of high energy emission preceding low
energy emission. The time intervals which were correlated to
determine the spectral lags are marked with vertical lines on the lightcurves in the Appendix.
Within these intervals, only those counts above 10% of the peak count rate
were correlated to give the lag values in Table 4. The number distribution of
spectral lags measured over the full burst duration
is given in Fig. 10 for the 28 long-duration
GRBs with a measured lag between Channel 1 (25-50 keV) and Channels 2 and 3 (50-300 keV). No statistically significant negative spectral lags are found. Negative lags, which violate the typical hard-soft evolution of GRBs, have been observed in
a small minority of cases (e.g. Chen et al. 2005) and may be more prevalent in short
bursts (Gupta et al. 2002; Yi et al. 2006). A long tail extending to 5 s is observed in the lag
distribution in Fig. 10 and a clear separation between
short and long lag is drawn at
s. Thus, long-lag bursts have
s and those with
s are
referred to as short-lag GRBs. The 11 long-lag GRBs are identified in Table 4, with 4 in the FCFoV, a further 4 in the PCFoV to the 50% coding level and the remaining 3 GRBs at larger off-axis angles (Fig. 4).
The spectral lag distribution of INTEGRAL GRBs as
a function of peak flux is shown in Fig. 11. The BeppoSAX SN burst GRB 980425 (Galama et al. 1998) is also shown in Fig. 11. The SN burst XRF 060218, with a peak flux of
,
is not included in the figure because it has an extremely long lag of 61
(Liang et al. 2006). The other low luminosity burst shown in Fig. 11 is GRB060505, which has no associated SN (Fynbo et al. 2006; McBreen et al. 2008). The figure shows that both bright and faint GRBs have short spectral lags, but there is an obvious absence of bright long-lag GRBs. Therefore GRBs with long spectral lags tend to be weak bursts with low peak flux. This trend is in good agreement with that
observed using BATSE GRBs (Norris 2002), where the proportion of long-lag GRBs is negligible
among bright BATSE bursts and increases to around 50% at the
trigger threshold. Using 1429 BATSE GRBs, Norris (2002) identified three GRB groups that consist of bright short-lag bursts, weak short-lag bursts and weak long-lag bursts. These groups are also clearly identifiable for the INTEGRAL sample in
Fig. 11.
The isotropic peak luminosity as a function of spectral lag is shown in Fig. 12 and includes the 3 INTEGRAL GRBs with known
redshift for which a lag was measured. The low-luminosity bursts GRB 980425, XRF 060218 and GRB 060505 are also plotted in Fig. 12. The dashed line is the anti-correlation between lag and luminosity proposed
by Norris et al. (2000). The bright INTEGRAL bursts
GRB 050502a and GRB 050525a have peak luminosities of
1.8
1052 erg s-1 and 1.8
1051 erg s-1 and
spectral lags of
0.11+0.07-0.06 s and
0.130+0.003-0.002 s,
respectively and follow the trend of the relation. At z=0.106, GRB 031203 has a peak luminosity of 8.4
1048 erg s-1 and spectral lag of
0.17+0.03-0.04 s, causing it to
fall significantly below the correlation (Gehrels et al. 2006; Sazonov et al. 2004). The HETE burst GRB 030528 has a long lag similar to that of
GRB 980425 but a relatively high luminosity and is consistent with
the lag-luminosity relation (Gehrels et al. 2006). A long spectral lag is
therefore not an exclusive determinant for a low-luminosity GRB.
Table 4:
Spectral lag measurements for INTEGRAL GRBs. The columns refer to (from left to right): GRB; supergalactic longitude (SGL) and latitude (SGB); burst interval used in
spectral lag determination relative to trigger time and as marked on time profiles in
the Appendix; spectral lags measured between Channel 2 (50-100 keV) and Channel 1 (25-50 keV),
,
Channels 2 and 3 combined (50-300 keV) and Channel 1 (25-50 keV),
and Channel 3 (100-300 keV) and Channel 1 (25-50 keV),
.
For the SN burst GRB 031203, spectral lags of 0.24
0.12 s between 20-50 keV and 100-200 keV (Sazonov et al. 2004) and 0.30
0.20 s between 15-50 keV and
50-150 keV (Shrader 2006) have been reported and are consistent with the value
s in Table 4 and Fig. 11. A spectral lag for GRB 040403 of 0.6
between 15-40 keV and
40-200 keV has previously been reported (Mereghetti et al. 2005),
consistent with the value of
s
in Table 4, taking into account the
different energy ranges. The spectral lag of GRB 050525a
was found to be
0.006 s (Norris et al. 2005), in agreement with
the value of
s obtained in Table 4. The spectral lag for the short burst, GRB 070707 is 5
5 ms (
), consistent with
the negligible lag values expected for short GRBs (Zhang et al. 2006a; Norris & Bonnell 2006).
For most of the GRBs with distinct separate pulses, the spectral lag does not
evolve significantly during the burst, i.e. GRB 030320, GRB 040106,
GRB 040422, GRB 040812, GRB 050522 and GRB 050525a. Some evolution is
evident in GRB 050918 for which the lag varies from
0.50+0.05-0.04 s for the first pulse of the burst, to a slightly negative lag of -0.14
0.01 s for the second pulse. For GRB 041219a, the lag of the precursor is relatively long and is much shorter for the main
emission pulses, as discussed in McBreen et al. (2006). Spectral lag evolution is often seen in multi-peaked GRBs (e.g. Hakkila et al. 2008; Chen et al. 2005; Hakkila & Giblin 2004; Ryde et al. 2005), and poses obvious difficulties for the use of the lag as a luminosity indicator.
Spectral lags are measured between wavelet-smoothed lightcurves for
a number of GRBs with
(20-200 keV)
and are denoted by
in Table 4. Table 5 gives the lags
determined with and without denoising for these GRBs. The denoising method allows
the lag to be measured in some cases for very weak GRBs where it
cannot be determined using the raw data and in most cases the
lag is better constrained with smaller errors.
Spectral lag measurements were not possible for 16 GRBs for the following reasons:
GRB 031203 is the third nearest GRB at z=0.1055 (Prochaska et al. 2004)
and is notable for its unambiguous association with the supernova
SN 2003lw (Malesani et al. 2004). It is a confirmed low-luminosity
GRB with an isotropic energy of 4
(20-200 keV) (Sazonov et al. 2004) and a lag of
0.17+0.04-0.03 s between 25-50 and 50-300 keV. The
IBAS localisation of GRB 031203 enabled XMM-Newton to begin
follow-up observations 6 h later (Santos-Lleo et al. 2003). The X-ray observations
showed concentric ring-like structures centred on the GRB location, making this the first detection of a GRB X-ray halo, caused by X-ray scattering from dust columns in our galaxy along
the line of sight to the GRB (Tiengo & Mereghetti 2006; Vaughan et al. 2004). Dust
scattering X-ray halos have recently been observed for two Swift
GRBs (Vianello et al. 2007). The X-ray observations of GRB 031203 inferred a very high
soft X-ray flux for this burst, implying that this GRB may have been an
X-ray Flash (XRF) (Watson et al. 2006,2004; Sazonov et al. 2006).
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Figure 10:
Spectral lag distribution for the 28 INTEGRAL GRBs
for which a lag could be measured between 25-50 keV and 50-300 keV
(
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Figure 11:
Spectral lag distribution of INTEGRAL GRBs
as a function of peak flux (20-200 keV). The SN bursts GRB 980425 and GRB 031203 are identified and represented by open circles, as is GRB 060505 which does not have an associated SN. XRF 060218 has a peak flux of
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GRB 041219a is the brightest burst localised by INTEGRAL (McBreen et al. 2006). The
peak flux of 43 ph cm-2 s-1 (20 keV-8 MeV, 1 s integration) is greater than that for 98% of all bursts and the total duration of
520 s is longer than
all but a small number of bursts. The SPI instrument was used to measure GRB polarisation
through multiple scattering events in its 19 Ge detectors (Kalemci et al. 2004), since the scatter angle distribution depends on the polarisation of the incoming
photons (Lei et al. 1997). A search for linear polarisation in
the most intense pulse (66 s) in GRB 041219a and sub-intervals was
performed. Kalemci et al. (2007) and McGlynn et al. (2007) have shown
that there is evidence for a high degree of polarisation, but at a low significance level.
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Figure 12:
Isotropic peak luminosity (![]() ![]() ![]() ![]() ![]() ![]() |
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Table 5:
Wavelet-denoised spectral lags of weak GRBs. The lags derived
from raw data are shown for comparison where available. Spectral lags
measured between Channels 2 and 3 combined (50-300 keV) and Channel 1 (25-50 keV),
,
with the exception of the XRFs for which the lag is measured between 15-25 keV
and 25-50 keV (Channel 1),
.
X-ray observations were performed for 2 long-lag GRBs with XMM-Newton (Gonzalez-Riestra & Rodriguez-Pascual 2004; Rodriguez-Pascual & Gonzalez-Riestra 2004) and 5 long-lag GRBs with Swift (Kennea et al. 2005; Mangano et al. 2005; Parola et al. 2005; Vergani et al. 2007; Kennea et al. 2006). There were also X-ray observations of 8 of the GRBs with no lag measurement. The median X-ray flux for the long-lag GRBs is 4
10-13 erg cm-2 s-1 between 5 to 10 h after the burst, with an upper limit in the two cases of non-detection of
4
10-14 erg cm-2 s-1, indicating that the long-lag weak GRBs tend to have a weak X-ray afterglow component. In contrast, the other INTEGRAL GRBs with a measured afterglow have a typical flux of
9
10-13 erg cm-2 s-1 between 2 and 12 h after the burst.
Of 300 GRBs localised by Swift up to November 2007,
60% have optical or near-IR afterglows and only
30% have measured redshifts (Coward et al. 2008),
even though deep observations down to
21-22 mag are carried out for most events within 24 h of
the burst. Dark GRBs without a detectable afterglow may therefore make up a significant proportion of the GRB population.
Almost 70% (31/46) of the GRBs observed by INTEGRAL do not have a detected optical counterpart, including 9 of the 11 long-lag GRBs. The optical observations revealed faint afterglows for GRB 040323 and GRB 040827, and near-IR afterglows for GRB 040223 and GRB 040624 (Filliatre et al. 2006). A non-spectroscopic redshift in the range 0.5<z<1.7 was obtained for GRB 040827 (de Luca et al. 2005). The IBIS error box of GRB 060114 contains galaxies from the cluster A1651 (z=0.087) and the optical afterglow was fainter than R=19 just 1.9 min after the GRB (Guidorzi et al. 2006). Only one radio afterglow has been detected for the long-lag GRBs (Frail 2005), compared to a total of 8/46 for all of the INTEGRAL GRBs.
GRB 040223 and GRB 040624 (Filliatre et al. 2006) provide good
examples of GRBs with dark or faint optical
afterglows. GRB 040223 was observed close to the galactic
plane, so NIR observations were carried out to overcome the
high dust obscuration. Observations were undertaken at the NTT
of ESO, 17 h after the GRB and no afterglow was
found. GRB 040624 was located far from the galactic plane at
high latitude where the optical extinction is
negligible. Afterglow observations were carried out 13 h
after the burst using the VLT and TNG. Magnitude limits were
obtained in the optical that are fainter than the very faint
end of the distribution of the magnitudes of a compilation of
39 promptly observed counterparts. The position of GRB 040624 is less than 5
from a galaxy in the cluster A1651. A search for a supernova was carried out up to a month after the GRB but none was found to a faint limit of R > 22.6 (D'Avanzo et al. 2004).
The lack of a detected optical afterglow may be due to a number of
factors. Possible explanations include dust obscuration, a low-density environment, an intrinsically faint afterglow in the optical, a rapidly decaying afterglow or the burst
occuring at a high redshift (e.g. Rol et al. 2005; Jakobsson et al. 2004). Dust
obscuration may be due to a burst environment with a
high gas column density (e.g. Lamb 2001; Castro-Tirado et al. 2007) or dust in the
host galaxy along the line of sight to the GRB (10% of dark
events, Piro et al. 2002). Low-density GRB environments can also produce a
very faint optical afterglow but the association between GRBs and
core-collapse SNe does not favour this scenario (Taylor et al. 1998). Some
GRBs have intrinsically faint afterglows (Fynbo et al. 2001). GRBs at high
redshift can only account for
10% of these dark bursts (e.g. Gorosabel et al. 2004; Castro-Tirado et al. 2006). Using early observations of Swift GRBs, Roming et al. (2006) found that
25% of the sample were extincted by galactic dust,
25% by absorption in the local burst environment and
30% were most probably affected by Ly-
absorption at high redshift.
Most GRB continuum spectra can be fit by the Band model (Band et al. 1993), an
empirical function comprising two smoothly broken power laws. The distributions of the low energy power-law photon index and high energy power-law photon index are distributed around
values of
and
,
respectively, for time-resolved
spectra of 156 GRBs detected by BATSE (Preece et al. 2000). The majority of GRBs have low energy power-law spectral indices in the range -2 <
< 0 (e.g. Preece et al. 2000).
Of the 10 INTEGRAL GRBs fit by the Band model (Table 3), all have low energy spectral indices consistent with synchrotron emission, i.e. -3/2 <
< -2/3.
A thermal component of the prompt emission spectra has been proposed
by several authors (e.g. Ryde 2005; Kaneko et al. 2006; Bosnjak et al. 2006; McBreen et al. 2006; Ghirlanda et al. 2003). In a study of BATSE GRBs with very hard spectra, Ghirlanda et al. (2003) found that the time-resolved spectra were not adequately described by non-thermal emission models and that the
early parts of the bursts were well fit by a blackbody
component. Ryde (2005) has shown that GRB spectra may be composed of a thermal and a power-law
component. McBreen et al. (2006) found that for quasithermal model fits to the precursor and main emission of the INTEGRAL burst GRB 041219a, the blackbody component is more dominant in
the precursor of the burst, while the main burst emission is
well fit by both the Band and quasithermal models. The blackbody temperature decreases from the precursor of GRB 041219a to the main burst emission as expected from Ryde (2005). The
10 bright GRBs in Table 3 are equally well fit by the
Band model and blackbody + power-law model fits to the average
prompt emission spectra, with similar values.
Many of the INTEGRAL GRBs in Table 2 have
steep power-law spectra, which are significantly outside the usual
range of the Band model low-energy spectral index of -3/2 < < -2/3. For these
GRBs, the power-law index is similar to the high energy photon
index above the break energy, with typical values of
between
-2 and -2.5 (Preece et al. 2000). If the steep power-law indices are
assumed to be
,
the break energy, E0, must be at or
below the sensitivity threshold of IBIS,
20 keV. There is therefore an excess of counts in
the X-ray/soft
-ray region, implying that they are
X-ray rich. The peak energy is given by
and has a value of
for a typical value of
.
These GRBs have a low
and will have a low luminosity if they are at low redshift (Amati et al. 2007).
INTEGRAL has detected a number of X-ray rich GRBs. X-ray flashes, X-ray rich GRBs and classical GRBs appear to possess a continuum of spectral properties and it is probable that they have a similar origin (Sakamoto et al. 2005). INTEGRAL X-ray rich bursts tend to be weak and their time profiles consist of long, slow pulses (see Appendix). Examples include GRB 040223 (Fig. A.1i), GRB 040624 (Fig. A.1a), GRB 050626 (Fig. A.1d) and GRB 060130 (Fig. A.1k).
GRBs detected at off-axis angles outside the FCFoV of IBIS have a higher peak flux (Fig. 4) because of the reduction in collecting area. For this reason, we estimate the rate of GRBs both in the FCFoV and in the PCFoV at greater than 50% coding. There are 11 GRBs within the FCFoV of 0.025 sr of IBIS in 4 years of observation time, yielding an all-sky rate of
above the threshold of
in the energy range 20-200 keV. The 4 long-lag GRBs in the FCFoV give a rate of
.
The 33 GRBs within the PCFoV to the 50% coding level yield an all-sky rate of
and
for the 8 long-lag GRBs above the higher threshold of
.
The long-lag GRBs contribute significantly at faint flux levels and appear to form a separate population in the log N-log P distribution (Fig. 5). The rate of GRBs is in good agreement with the values obtained from the more sensitve analysis of BATSE archival data (Stern et al. 2001; Kommers et al. 2001).
The lack of redshift determinations for the weak GRBs detected by IBIS prohibits progress by using individual GRBs. However there are a number of redshift indicators that can be used on weak GRBs. In this case the best redshift indicator is the spectral lag which combines the spectral and temporal properties of the prompt GRB emission. GRBs have a long lag when a typical value of 0.1 s is redshifted by a large factor or alternatively is an intrinsic property of a low-luminosity GRB such as GRB 980425 and XRF 060218. The rate of z>5 GRBs in IBIS has been modelled (Lapi et al. 2008; Salvaterra et al. 2008; Gorosabel et al. 2004; Guetta & Piran 2007) and is unlikely to be more than 1 or 2 GRBs in 5 years of observations. The long lag is therefore taken to be an intrinsic property of most of the long-lag GRBs indicating their low luminosity and we investigate the consequences.
Table 6:
Median properties of the 28 long-duration GRBs with a measured
,
categorised into those with short lags (
)
and long lags
(
.)
The median properties of long and short lag INTEGRAL GRBs are given in Table 6 for the 28 bursts with a measured
value of
.
Approximately 40% of
INTEGRAL GRBs with a measured lag belong to the
long-lag category. The median peak flux for long-lag
GRBs is a factor of
5 lower than for GRBs with short lags.
The distribution of the INTEGRAL GRBs in supergalactic coordinates is shown in
Fig. 13. All of the INTEGRAL GRBs are divided almost equally between the
half of the sky above and below
,
in agreement with the
exposure map which has
52% of the exposure time
within
of the supergalactic plane. However, 10 of the 11 long-lag GRBs are concentrated at supergalactic
latitudes between
.
The quadrupole moment (Hartmann et al. 1996) has a value of Q=0.007
0.043 for all INTEGRAL GRBs and Q=-0.225
0.090 for the long-lag GRBs. The quadrupole moment of the 47 bursts is consistent with zero and an isotropic distribution. The non-zero moment of the long-lag bursts indicates an anisotropy in the distribution of these GRBs with respect to the supergalactic plane. The binomial probability that this is a chance occurrence is 7
10-3. GRB 980425 and XRF 060218 have long lags and lie within
of the supergalactic plane, while GRB 031203 has a relatively short lag and lies at a high supergalactic latitude. The long-lag GRBs observed with BATSE are also significantly concentrated in the direction
of the supergalactic plane with a quadrupole moment
Q = -0.097
0.038 (Norris 2002). The combined results of more than 14 years of observations with IBIS and BATSE lead us to
conclude that long-lag GRBs trace the features of the nearby large-scale structure of the Universe as revealed with superclusters, galaxy surveys (Stoughton et al. 2002; Lahav et al. 2000) and the very high energy cosmic rays (Abraham et al. 2007). This result is a further indication that most long-lag GRBs are nearby and have low luminosity. The local supercluster seems to be appended to a web of filaments and sheets, rather than an isolated pancake structure, with superclusters evident to
400 Mpc. It has been pointed out that weak BATSE GRBs appear to be correlated with galaxies out to distances of
155 Mpc with the limit determined by galaxy surveys (Chapman et al. 2007).
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Figure 13:
a) INTEGRAL exposure map in supergalactic co-ordinates up to July 2007 (contours in units of kiloseconds). b) The distribution of INTEGRAL GRBs
in supergalactic co-ordinates; the open circles represent short-lag GRBs (
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A nearby population of long-lag, low-luminosity GRBs has previously been
proposed based on the detections of GRB 980425, GRB 031203 and
XRF 060218 (e.g. Daigne & Mochkovitch 2007; Guetta et al. 2004). GRB 980425 has an isotropic-equivalent
-ray energy release of
1048 erg, approximately 3 orders of magnitude lower
than that of ``standard'' GRBs, assuming
its association with SN 1998bw (Galama et al. 1998) and redshift of z=0.0085 (Tinney et al. 1998).
XRF 060218, the second closest GRB localised to date,
was detected at a redshift of z=0.033 (Mirabal et al. 2006). This burst had an extremely
long duration (
s), a very low isotropic energy of
6
1049 erg and is classified as an XRF (Campana et al. 2006). The distance to the long-lag GRBs can also be constrained by association and comparison with the two low luminosity bursts GRB 980425 (
)
and XRF 060218 (
). The distances to GRB 980425 (Galama et al. 1998) and XRF 060218 (Soderberg et al. 2006) are 36 Mpc and 145 Mpc, respectively, and these bursts would have been detected in the FCFoV of IBIS to 135 Mpc and 290 Mpc. The association of the long-lag GRBs with the known low luminosity GRBs and with the supergalactic plane implies that they are at similar distances. GRB 060505 has no SN to faint limits and has a smaller lag of
0.4 s and a distance of 404 Mpc (Fynbo et al. 2006; McBreen et al. 2008).
The region marked with a box on the lag-luminosity plot (Fig. 12) contains the long-lag GRBs if they belong to the low luminosity population at an adopted distance of 250 Mpc. The box contains the prototype low luminosity GRB 980425 and is bracketed on one side by GRB 060218 and on the other by GRB 060505 (
)
and GRB 031203 (
)
and at short lag by GRB 060614 which lies in the region occupied by short GRBs (Gehrels et al. 2006). With a long lag of
2.8 s, GRB 980425 qualitatively follows
the lag-luminosity trend but falls significantly below the relation in Fig. 12 (Norris 2002), as do GRB 031203 (Sazonov et al. 2004) and GRB 060218 (Liang et al. 2006).
The solid line in Fig. 12 is the proposed lag-luminosity relationship for low-luminosity GRBs and is parallel to but shifted from the corresponding fit for the long cosmological GRBs by a factor of
103.
Both GRB 980425 and GRB 031203 violate the Amati correlation (Amati et al. 2007) between isotropic energy,
,
and peak energy,
(Ghisellini et al. 2006).
GRB 060218 however is consistent with the the Amati relation, fuelling the debate that GRB 980425 and GRB 031203 may just be apparent outliers and their intrinsic
properties may be consistent with the relations. Invoking a jet geometry, the low observed luminosities for these GRBs may be due to such factors as wider jet opening angle,
variations in viewing angle such that the more off-axis a burst is
viewed the lower its luminosity or profiled jets with the Lorentz
factor decreasing off-axis (Yamazaki et al. 2003; Ramirez-Ruiz et al. 2005).
It has also been proposed that GRBs 980425 and 031203 are intrinsically sub-energetic events seen on-axis, based on afterglow observations (Soderberg et al. 2004) and within the constraints of the internal shock model (Daigne & Mochkovitch 2007). Such inherently sub-luminous events would be permitted by the internal shock model, where the burst is produced by a mildly relativistic outflow. If intrinsically low-luminosity, the rate of bursts such as GRB 980425 may be far higher than that of ``standard'' cosmological GRBs but only detectable locally.
The possibility that low luminosity GRBs could be part of the same population as cosmological GRBs or form a separate sub-energetic population with a much higher rate has been considered (Le & Dermer 2007; Soderberg et al. 2006; Coward et al. 2008; Liang et al. 2007; Guetta & Della Valle 2007; Cobb et al. 2006; Chapman et al. 2007; Virgili et al. 2008). The large number of long-lag GRBs detected with IBIS favours the latter conclusion and indicates that low redshift GRBs are dominated by the low luminosity class.
The collapsar model can account for low-luminosity GRBs if they have low
Lorentz factors and fail to produce highly-relativistic jets due to
baryon loading (Woosley & MacFadyen 1999). It has also been proposed that the nature of the central engine
may be different, e.g., a magnetar progenitor as opposed to a black
hole (e.g. Soderberg et al. 2006; Toma et al. 2007). Some authors suggest that the
-rays are produced in a supernova shock breakout (e.g. Matzner & McKee 1999; Ghisellini et al. 2007). A very luminous X-ray outburst was observed from the core collapse SN in NGC 2770 (Soderberg et al. 2008) that may be the shock breakout as recently observed from a red supergiant in a galaxy in the COSMOS field (Schawinski et al. 2008) or an X-ray flash (Xu et al. 2008; Li 2008).
We evaluate the rate of GRBs over the whole sky using the 8 long-lag GRBs in the PCFoV (Table 4) at 50% coding (0.1 sr) over an exposure time of 4 years, adopting a distance of 250 Mpc and assuming that 2 of the 8 GRBs are not at low redshift. We obtain
which is
25% of the local rate of type Ib/c SNe (Soderberg et al. 2006). The major uncertainty in this estimate is the distance, where a change of only a factor of 2 increases or decreases this number by 8 to
and
,
respectively.
The rate of low-luminosity GRBs at the adopted distance of 250 Mpc exceeds the upper limit of 3% or <
of type Ib/c SN producing GRBs, which was derived assuming that all low luminosity GRBs would produce a SN and be as radio bright as the SN GRBs (Soderberg et al. 2006). However, the low luminosity GRB 060605 has no associated SN to faint limits and is evidence for a quiet end for some massive stars (Fynbo et al. 2006; Dado et al. 2006; McBreen et al. 2008). A GRB may occur without a corresponding SN being observed if the 56Ni does not have sufficient energy to escape the black hole or if the progenitor star has a low angular momentum. The association of low luminosity GRBs with the supergalactic plane is not proof that they are associated with clusters of galaxies but indicates that clusters may play a role. It is interesting to note that the rate of type Ia SNe is higher in elliptical galaxies in clusters than in field ellipticals by a factor of
3 (Mannucci et al. 2007). This effect is due to galaxy-galaxy interactions in clusters (Boselli & Gavazzi 2006) either producing a small amount of young stars or affecting the evolution and properties of binary systems. In the latter case, there should also be an increase in the merger rate of white dwarfs or a white dwarf with a neutron star or black hole. A merger involving a white dwarf (Levan et al. 2006; Fryer et al. 1999; King et al. 2007; Middleditch 2004) should produce a long GRB that is likely to be fainter than the formation of a black hole in cosmological GRBs. There will be no supernova in the merger of a white dwarf with a neutron star or black hole, and probably a faint afterglow. In addition, the merger could take place in the intercluster region without a host galaxy if the binary is ripped from its host in the merger interaction involving the cluster galaxies (Niino & Totani 2008).
INTEGRAL observations of gamma-ray bursts have
yielded many interesting results and offer significant insight
into the prompt -ray emission. IBAS successfully
provides accurate, fast localisations of GRBs to the community
at a rate of
0.8 GRBs per month, enabling
multi-wavelength afterglow observations to be carried out by
other space-based missions and ground-based telescopes.
We have presented the spectral, spatial, and temporal lag analysis of the 47 INTEGRAL GRBs up to July 2007. Most weak INTEGRAL GRBs are well fit with a power law, while bright GRBs can be fit by both the Band and quasithermal models. Approximately 40% of the GRBs for which a lag was measured have long spectral lags (>0.75 s between 25-50 and 50-300 keV). The long-lag GRBs are characterised by low peak flux, long slow pulses and are concentrated towards the supergalactic plane, reflecting the nearby large-scale structure of the Universe.
INTEGRAL therefore detects a large proportion of faint, long-lag GRBs that are inferred to be local. The sensitivity of IBIS is such that it can detect very faint GRBs, allowing INTEGRAL to probe the population of low-luminosity GRBs with long lags. This population appears to be distinct from that of high-luminosity GRBs and dominates the local GRB population.
Acknowledgements
The authors thank Darach Watson and Rob Preece for useful discussions and comments, Andreas von Kienlin for providing the GRB 060901 data and Erik Kuulkers for the INTEGRAL exposure map data. S.M.B. acknowledges the support of the European Union through a Marie Curie Intra-European Fellowship within the Sixth Framework Program.
The lightcurves of 43 of the 47 INTEGRAL GRBs are presented in the 25-50 keV (dark lines) and 50-300 keV (light lines) energy bands. Exceptions are the XRFs which were not detected above 50 keV and for which the lightcurves are plotted in the 15-25 keV (dark lines) and 25-50 keV (light lines) and the very weak GRBs and GRBs with telemetry gaps for which a lag could not be determined which are given over the full energy range of 25-300 keV. The regions which were used in the spectral lag analysis are denoted by solid vertical lines and the temporal resolution is that at which the lag was determined. All lightcurve data is from the IBIS instrument on board INTEGRAL with the exceptions of GRB 041219a and GRB 050525a for which data is taken from the BAT instrument on Swift due to IBIS telemetry saturation. A satellite slew occurred during GRB 030131 and the lightcurve is not presented here but is available in Götz et al. (2003). GRB 060428c was discovered in the INTEGRAL archival data and the lightcurve is available in Grebenev & Chelovekov (2007). IBIS data is currently unavailable for GRB 060930 and GRB 070311.
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Figure A.1: Lightcurves of GRBS observed with INTEGRAL. |
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Figure A.1: continued. |
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Figure A.1: continued. |
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Figure A.1: continued. |
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