A&A 404, 815-818 (2003)
DOI: 10.1051/0004-6361:20030121
A. Klotz1 - M. Boër1 - J. L. Atteia2
1 - Centre d'Étude Spatiale des Rayonnements,
Observatoire Midi-Pyrénées (CNRS-UPS), BP 4346, 31028
Toulouse Cedex 04, France
2 - Laboratoire d'Astrophysique,
Observatoire Midi-Pyrénées (CNRS-UPS), 14 avenue E. Belin,
31400 Toulouse, France
Received 20 November 2002 / Accepted 17 January 2003
Abstract
We present the data acquired by the TAROT automated
observatory on the afterglow of GRB 020531.
Up to now, no convincing
afterglow emission has been reported for this short/hard GRB at
any wavelength, including X-ray and optical. The combination of
our early limits, with other published data allows us to
put severe constraints on the afterglow magnitude and light curve.
The limiting magnitude is 18.5 in R band, 88 min after the GRB, and the decay slope power
law index could be larger than 2.2.
Key words: gamma-ray : bursts
Since their first detection by van Paradijs
et al. (1997), gamma-ray burst (GRB)
optical afterglows have been
detected in about 40% of the sources displaying an X-ray
afterglow. The fireball model (Rees & Mészáros
1992; Mészáros & Rees 1997; Panaitescu
et al. 1998) has been established as a
standard tool to
interpret these observations. In this framework the afterglow
emission is described as synchrotron and inverse Compton emission
of high energy electrons accelerated during the shock of an
ultra-relativistic shell with the external medium, while the
prompt emission is due to the internal shocks produced by shells
of different Lorentz factors
within the relativistic blast wave (see Piran
1999 for a review). Both the prompt radiation and early
afterglow phases provide critical information to establish the
physical processes at work during the burst itself, as well as the
physical conditions of the surrounding environment (Kumar &
Panaitescu 2000; Kumar & Piran 2000). There
is a general consensus that the fireball plasma is constituted by
pairs and
-ray photons, however the ultimate energy
reservoir and the detailed radiation
mechanisms are still a challenge
to theoretical models.
The situation of 60% of the GRB afterglows which are not observed at optical wavelengths (called dark GRBs) is not clear. As it has been shown in Boër & Gendre (2000), the optical flux is not correlated with the intensity of the X-ray afterglow, nor with the distance. Generally speaking the absence of an optical transient associated with a GRB can be attributed to four, non exclusive, reasons, namely 1) the distance of the source, though this is obviously not the general case, 2) the absorption of the visible light by a dense medium (i.e. dust), 3) the rapid decay of the optical afterglow, and 4) the intrinsic faintness of the source at long wavelengths (i.e. optical, NIR...). However, a few reports of near IR and optical non-detection of GRB afterglows show that hypothesis 2 is not the main reason (see e.g. GRB 010214, Piro 2001 and subsequent GCN circular available at the URL http://gcn.gsfc.nasa.gov/gcn/other/010214.gcn3). In the absence of rapid simultaneous X-ray and optical measurements, hypotheses 3 and 4 are difficult to evaluate.
It should be noted that for the sub-class of GRBs that exhibit a short duration and a hard spectrum, usually called short/hard GRB (Dezalay et al. 1996; Kouveliotou et al. 1993), no optical counterpart has been detected yet (Hurley et al. 2002a; Gorosabel et al. 2002) excepted in the case of GRB 000313 (Castro-Tirado et al. 2002a published R=9.4 at 4 min after GRB). However the reality of the afterglow candidate for GRB 000313 is questionable because it is seen in only one image. The usual no optical counterpart detection is largely due to the scarcity of the observations. If this appears a "general" law, it can be the indication of a different geometry (as viewed from the observer) or of another mechanism for the emission of the afterglow (e.g. Shanthi et al. 1999). Hence, it is important to get rapid and deep measures (or upper limits) on the afterglow emission for GRB sources of all classes, and in particular for the short GRBs.
In this Paper we report on the early observations of GRB 020531 performed with the automatic TAROT observatory (Bringer et al. 1999). Our data, combined with the data from other telescopes strongly constrain both the magnitude and the decay slope index of the optical counterpart, if any.
The High Energy Transient Explorer satellite
(HETE, Ricker et al. 2000) detected GRB 020531 with the FREGATE and WXM instruments on
May 31, 2002 at 0h26min18.73 UTC (Ricker et al.
2002). This event is a short/hard GRB:
t90=0.94 s,
t50=0.45 s, and fluence is
erg cm-2 in the FREGATE
50-300 keV band. The absolute localization was not performed by the
flight software and the preliminary coordinates were computed by a
ground analysis. The GRB Coordinates Network (GCN - Barthelmy
1997) broadcasted the position at 1h54min22s UT.
Additional information about the GRB localization
can be found in Lamb et al. 2002. Twenty-five GCN circulars (GCNC) were published on this event between May 31 and July 25, 2002. In the first very early reports, it appears that no
unambiguous optical counterpart was recorded.
The final error box given by the Inter Planetary Network (IPN) published
on the July 10th 2002 (Hurley et al.
2002b). In this area, four faint sources were detected
by the Chandra satellite ACIS-I array (Butler et al. 2002)
five days after GRB.
The connection of one of these X-ray sources
with the gamma-ray transient remains to be confirmed.
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Figure 1: A sub-image of the TAROT composite image (11 frames of duration 30 s each). The parallelogram is the last IPN error box (from GCNC 1461, Hurley et al. 2002b). The limiting magnitude is 18.5 (R band). |
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Figure 2:
A synthetic Cousins R image of the same field as the
TAROT image in Fig. 1. Magnitude values are taken from the
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Up to now, none of the suggested optical counterparts of GRB 020531 has been confirmed. In this study we present the data acquired with the TAROT observatory. Our limits are compared with the limiting magnitudes obtained by other observers at different times after the GRB. Given that our data were obtained only 88 min after the burst itself, we can infer strong limits both on the optical counterpart magnitude and decay slope.
The first image was taken by TAROT less than 6 s after the position of GRB 020531 was provided by the GCN. A series of 11 unfiltered images of 30 s was then taken. An automatic preprocessing software gave scientific images in the following minutes. We compared them to the Digital Sky Survey (DSS) images. We concluded quickly that no bright new source was present. The limiting magnitude of the individual images, in the Cousins R band, is about 16.7.
Then we coadded the 11 images to improve the signal to noise
ratio (see Fig. 1). A limiting magnitude of 18.5 (compared
to the R Cousins
band) is reached. This limiting magnitude is estimated from
comparison with a set of synthetic images computed from the
USNOFS all-sky photometry of field (Henden 2002). In
Fig. 2, only stars brighter than
are plotted.
Three TAROT sources, afterglow candidates, were published in the GCN circulars: sources A and B (Boër et al. 2002) and C (Klotz et al. 2002).
Table 1: Log of the published values of the limiting magnitudes, presented in the chronological order. The first column is the date from GRB (in days). The second is the limiting R magnitude of the image. The third is the GCN circular index of the publication.
Source A,
(J2000.0), R=17.4,
cannot be the asteroid number 2 mentioned by Li et al.
(2002) in the GCNC 1405, as it was supposed by
Boër et al. (2002) in the GCNC 1408. The reason is that it lies
in the opposite side of the apparent motion published by Li et al.
(2002). Source B,
(J2000.0), R=17.1, is a known star visible in DSS and various
other images. Anyway, A and B sources lie outside the IPN error
box.
Source C,
(J2000.0),
,
is considered as the best TAROT image candidate in the IPN error box. We reprocessed the raw images using the calibration
frames taken both before and after the night of May 30-31, 2002,
and we obtained a fainter source at the position of the source C
on the new refined co-added
images. This meant that source C could be a group of "hot pixel"
badly corrected by the automatic preprocessing which uses only the
calibration frame taken during the preceding day, to produce
synthetic calibration data.
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Figure 3: Reported upper limits of the magnitude (from Table 1) of the optical afterglow of GRB 020531 (arrows, with the GCN circular number). Limiting magnitudes of the two other early observations from GCN 1430 (R>8) lie far outside upper the panel. For comparison, we added some data, labeled 010119 and 000313, respectively for the upper limits of the short/hard GRB 010119 (Gorosabel et al. 2002) and GRB 000313 (Castro-Tirado et al. 2002a). We plotted, as a solid line, the light curve of the dim afterglow of the long burst GRB 020124 (Berger et al. 2002). The dotted line represents the upper limit for the brightness of the afterglow, assuming a constant decay slope. |
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Other fuzzy patches are also seen in the image of
TAROT presented in Fig. 1. All of these patches
can be related to known stars fainter than
.
However, as the TAROT image is unfiltered, it is not
surprising to find these stars (color effects).
Up to now, no afterglow of a short/hard GRB was detected. However, it is possible to get some constraints on the optical light curve. The best limits to constrain the light curve for the afterglow of GRB 020531 comes from TAROT, KAIT, and INT data. If GRB 020531 was followed by an optical afterglow, its light curve must lie in the left part of Fig. 3, below the dashed line.
Before GRB 020531, the earliest optical observations of a short/hard GRB were obtained on GRB 000313 (Castro-Tirado et al. 2002a) and on GRB 010119 (Gorosabel et al. 2002).
The decay slope index
for an afterglow of a short/hard
GRB (assuming flux
proportional to
)
is now more constrained
by GRB 020531 observations. Typical long GRBs afterglow decays are
between 0.7 and 1.8, marginally higher than 2
(i.e. GRB 980519, Vrba et al. 2000).
Concerning GRB 020531, if
the flux of the afterglow was about the limiting magnitude of TAROT (R =
18.5 at 1.47 hour after the burst), then its decay slope
must be >2.2. This slope value is in accordance with the GRB 000313 results
(Castro-Tirado et al. 2002a).
If the afterglow of GRB 020531 was
fainter at 1.47 hour after the burst, the decay slope should have a lower value.
If the afterglow of GRB 020531
was R=9.4 at 4 min after GRB (the same as the detection of GRB 000331),
the TAROT observation constrains the slope to be higher than 2.6.
Comparing to the dimmest long GRBs, e.g. GRB 020124 (Berger et al. 2002, see Fig. 3), it implies that the afterglow of GRB 020531 must be fainter. The TAROT upper limit measurement constrains the afterglow to be very dim. This result is correlated to the 50-300 keV fluence which is one decade fainter than those of typical long GRBs.
If the afterglow exists and decays with a
law,
and if the source flux was about the limiting magnitude
of late observations, one can calculate R=22.0at 1.47 hour after the GRB (TAROT observations) assuming
(the typical case). Obviously, the afterglow can
be even fainter if it is dimer than the limiting magnitude
of late observations. As a consequence, plans for future searches
of afterglows of short/hard GRBs can be adressed: large aperture
telescopes, equiped by wide field cameras, should observe
early stages (until 1 hour after GRB).
Small aperture telescopes could also
contribute if they shoot until 15 min after GRB with a
limiting magnitude R > 18.
The afterglow of GRB 020531, if it exists, is very dim,
compared to the observed optical counterparts
of long GRBs.
If the optical counterpart of GRB 020531 is typical of short/hard GRBs,
it means that these kinds of GRBs are associated
to very dim afterglows or no afterglow at all.
The observations suggest that the decay
slope
could be larger than 2.
It must be mentioned that dim afterglows can be localized only by early optical observations (case of GRB 020124 afterglow, found at 1.67 hour after the GRB).
Of course the possibility that GRB 020531 had no afterglow cannot be excluded. This proves the need to get more sensitive observations of the afterglow, as early as possible after the main event. The TAROT observatory demonstrated that this is possible, provided that the alert is sent quickly by the instrument. The increase in the HETE performances, the recent successful launch of the Curie-INTEGRAL satellite, as well as the perspective of the SWIFT GRB dedicated satellite gives hope that rapid observations of GRB optical counterparts willbe soon possible, as it was the case with BATSE (Akerlof et al. 1999; Boër et al. 2001; Castro-Tirado et al. 1999; Park et al. 1999).
Acknowledgements
The Télescope à Action Rapide pour les Objets Transitoires (TAROT) has been funded by the Centre National de la Recherche Scientifique (CNRS), Institut National des Sciences de l'Univers (INSU) and the Carlsberg Fundation. It has been built with the support of the Division Technique of INSU (INSU/DT). The TAROT CCD camera was built by a collaboration between the CESR and the CEMES. We thank the technical staff associated with the TAROT project: G. Bucholtz, J. Esseric, A. Mayet, A. M. Moly, F. Morand, M. Nexon, H. Pinna, and C. Pollas. We thank Holger Pedersen and the referee for their remarks.