A&A 370, 909-922 (2001)
DOI: 10.1051/0004-6361:20010291
B. L. Jensen 1 - J. U. Fynbo 2,3 - J. Gorosabel 4 - J. Hjorth 1 - S. Holland 2,5 - P. Møller 3 - B. Thomsen 2 - G. Björnsson 6 - H. Pedersen 1 - I. Burud 7 - A. Henden 8 - N. R. Tanvir 9 - C. J. Davis 10 - P. Vreeswijk 11 - E. Rol 11 - K. Hurley 12 - T. Cline 13 - J. Trombka 14 - T. McClanahan 14 - R. Starr 15 - J. Goldsten 16 - A. J. Castro-Tirado 17,18 - J. Greiner 19 - C. A. L. Bailer-Jones 20 - M. Kümmel 20 - R. Mundt 20
1 -
Astronomical Observatory,
University of Copenhagen,
Juliane Maries Vej 30, 2100 Copenhagen Ø, Denmark
2 -
Institute of Physics and Astronomy,
University of Aarhus, 8000 Århus C., Denmark
3 -
European Southern Observatory,
Karl-Schwarzschild-Straße 2,
85748 Garching, Germany
4 -
Danish Space Research Institute,
Juliane Maries Vej 30, 2100 Copenhagen Ø, Denmark,
5 -
Department of Physics, University
of Notre Dame, Notre Dame IN 46556-5670, USA
6 -
Science Institute,
Dunhagi 3, University of Iceland, 107 Reykjavik, Iceland,
7 -
Institut d'Astrophysique et de Géophysique, Université de
Liège, avenue de Cointe 5, 4000 Liège, Belgium
8 -
U.S. Naval Observatory,
Flagstaff Station, Flagstaff, AZ 86002-1149, USA,
9 -
Department of Physical Sciences,
University of Hertfordshire, College Lane, Hatfield,
Herts AL10 9AB, UK
10 -
Joint Astronomy Centre, 660 N. A'ohoku Place, Hilo,
Hawaii 96720, USA
11 -
University of Amsterdam,
Kruislaan 403, 1098 SJ Amsterdam, The Netherlands
12 -
University of California, Berkeley,
Space Sciences Laboratory,
Berkeley, CA 94720-7450 USA
13 -
NASA Goddard Space Flight Center,
Code 661, Greenbelt, MD 20771 USA
14 -
NASA Goddard Space Flight Center,
Code 691, Greenbelt, MD 20771 USA
15 -
The Catholic University of America,
Department of Physics,
Washington, DC 20064 USA
16 -
The Johns Hopkins University,
Applied Physics Laboratory,
Laurel, MD 20723 USA
17 -
Laboratorio de Astrofísica Espacial y Física Fundamental
(LAEFF-INTA), PO Box 50727, 28080, Madrid, Spain,
18 -
Instituto de Astrofísica de Andalucía (IAA-CSIC),
PO Box 03004, 18080 Granada, Spain
19 -
Astrophysikalisches Institut, Potsdam, Germany,
20 -
Max-Planck-Institut für Astronomie,
Königstuhl 17,
69117 Heidelberg,
Germany
Received 6 June 2000 / Accepted 19 February 2001
Abstract
We present Ulysses and NEAR data from the detection of the
short or intermediate duration (2 s) gamma-ray burst
GRB 000301C (2000 March 1.41 UT). The gamma-ray burst (GRB)
was localised by the Inter Planetary Network (IPN) and RXTE to an area
of
50 arcmin2. A fading optical counterpart was subsequently
discovered with the Nordic Optical Telescope (NOT) about 42 h after
the burst. The GRB lies at the border between the long-soft and the
short-hard classes of GRBs. If GRB 000301C belongs to the
latter class, this would be the first detection of an afterglow to a
short-hard burst. We present UBRI photometry from the time of the
discovery until 11 days after the burst. We also present JHK
photometry obtained with UKIRT on 2000 March 4.5 UT (3.1 days after
the burst). Finally, we present spectroscopic observations of the
optical afterglow obtained with the ESO VLT Antu telescope 4 and 5
days after the burst. The optical light curve is consistent with being
achromatic from 2 to 11 days after the burst and exhibits a break. A
broken power-law fit yields a shallow pre-break decay power-law slope
of
,
a break time of
days after the burst, and a post-break slope of
.
These properties of the light curve are best
explained by a sideways expanding jet in an ambient medium of constant
mean density. In the optical spectrum we find absorption features that are
consistent with Fe II, C IV, C II, Si II
and Ly
at a redshift of
.
We find evidence
for a curved shape of the spectral energy distribution of the observed
afterglow. It is best fitted with a power-law spectral distribution
with index
reddened by an SMC-like
extinction law
with
mag. Based on the Ly
absorption line
we estimate the H I column density to be
(N(H I)
.
This is the first direct
indication of a connection between GRB host galaxies and Damped
Ly
Absorbers.
Key words: gamma rays: bursts - cosmology: observations - galaxies: distances and redshifts - ISM: dust, extinction - quasars: absorption lines
The discovery of the first X-ray afterglow (Costa
et al. 1997) and optical counterpart (van Paradijs
et al. 1997) to a long-duration gamma-ray burst (GRB) have
led to a revolution in GRB research. The determination of a redshift
of 0.835 for GRB 970508 (Metzger et al. 1997), and
the subsequent determination of redshifts of 13 bursts with a median
redshift of
1.0, have firmly established their cosmological
origin (Kulkarni et al. 2000a; this work; Bloom et al. 2000).
The intriguing case of an association of the peculiar
supernova SN1998bw with GRB 980425 (Galama
et al. 1998) was the first indication of a possible
connection with supernovae.
Evidence for supernova signatures in the late light curves of
GRB 970228 (Reichart 1999; Galama et al. 1999)
and GRB 980326 (Castro-Tirado & Gorosabel 1999; Bloom et al. 1999) suggests that at least some long-duration GRBs may be related to the collapse of massive (>25
)
stars.
Breaks in the power-law declines of GRB 990123
(Kulkarni et al. 1999) and GRB 990510
(Harrison et al. 1999) are interpreted as evidence for collimated
outflows ("jets'') (see also Holland et al. 2000). Further evidence
for this collapsar + jet model
(e.g., MacFadyen & Woosley 1999) comes from the light curve of
GRB 980519 which is best interpreted as a jet expanding into a
preexisting circumburst stellar wind (Jaunsen et al. 2001).
The high-energy properties of GRBs show a bi-modal distribution of
burst durations (Hurley et al. 1992a; Kouveliotou et al. 1995) which, in the
simplest scenario, may indicate the existence of binary compact mergers
as the progenitors of the short-duration bursts (T90<2 s).
From an analysis of the Third BATSE Catalog, Mukherjee et al. (1998) have shown that, in addition to the short
(T90<2 s) and long (T90>5 s) classes, there may exist a
third, intermediate soft-spectrum class of GRBs with duration 2
s.
In this paper we report the discovery and subsequent observations and analysis of the afterglow of the short-to-intermediate duration GRB 000301C (Fynbo et al. 2000a).
Section 2 reports the detection, IPN localisation and the high-energy data of the GRB obtained from Ulysses and NEAR. Section 3 describes the discovery of the optical counterpart and our subsequent optical and infrared observations. Section 4 details the optical and infrared photometry and Sect. 5 describes the VLT spectroscopy. Section 6 describes the results obtained on the spectroscopy and spectral energy distribution and Sect. 7 is devoted to the discussion and interpretation, with Sect. 8 presenting our conclusions.
Throughout this paper, we adopt a Hubble constant of H0 = 65 km s-1 Mpc-1 and assume
and
.
GRB 000301C was recorded by the Ulysses GRB experiment and by the NEAR X-Ray/Gamma-Ray Spectrometer. Because this burst was relatively weak, it did not trigger the Ulysses Burst Mode, and the only data available from Ulysses is the Observation Mode 1 0.25 s resolution 25-150 keV light curve (Hurley et al. 1992b). NEAR records the light curves of bursts in the 150-1000 keV energy range with 1 s resolution, but takes high-energy spectra only with 40 min resolution.
Analysis of the Ulysses and NEAR relative timing data yields an
annulus centred at
,
with a radius of
degrees (at 3
full-width). This annulus
intersected the error-box of the All-Sky Monitor (ASM) on the RXTE
spacecraft, at near-right angles to create a composite localisation of
a parallelogram of area 50 arcmin2 (see Fig. 2).
Since no high-energy spectra are available, we have estimated the peak fluxes
and fluences for trial power-law spectra with indices between 1 and 4 using
the Ulysses data. For a typical power-law index of 2, we find a 25-100 keV
fluence of
,
and a peak flux over
the same energy range, and over 0.25 s, of
.
The uncertainties in these numbers are partly due to
the lack of a high-energy spectrum.
For example, the fluence estimates range from
1.45 10-6 to
as the
spectral index is varied from 4 to 1. The statistical uncertainty is
approximately 30%. From the NEAR data we estimate the 150-1000 keV fluence
to be approximately
.
![]() |
Figure 1:
A contour plot showing the duration-hardness
(
|
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Figure 1 shows the location of
GRB 000301C in a hardness vs. duration plot. The contour
plot contains 1959 GRBs for which data on fluence and duration were
available in the Fourth BATSE GRB Catalog (revised) (Paciesas et al. 1999) and the BATSE Current GRB Catalog
. The symbols represent the 10 GRBs included in the BATSE catalogs for which an afterglow has been
identified, with GRB 000301C located near the center of the
plot. Triangles are bursts where a break has been found in the
optical light curve. From this sparse set of data there does not
appear to be any marked difference in the distributions of bursts
with, or without, an identified break.
![]() |
Figure 2:
A finding chart with the rectangular IPN-errorbox indicated
along with the two initial ALFOSC pointings (ALFOSC FOV = 6.5 |
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![]() |
Figure 3:
Upper panel: A contour plot showing a
|
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The transient nature of the candidate was subsequently confirmed
at optical and infrared wavelengths (Bernabei et al. 2000;
Stecklum et al. 2000; Garnavich et al. 2000;
Veillet et al. 2000; Fynbo et al. 2000b;
Kobayashi et al. 2000). At the time of discovery the magnitude of
the OT was
(see Sect. 4 for a detailed
discussion of the photometry and Fig. 3 for a finding chart and
UBRI-images of the OT on 2000 March 3 UT).
We obtained subsequent optical observations using the NOT, the Antu telescope (UT1) of ESO's Very Large Telescope (VLT), the USNOFS 1.0-m telescope, the 2.2-m telescope at Calar Alto (CAHA) and the Wide Field Imager (WFI) on the ESO 2.2-m telescope. In addition we obtained near-infrared (NIR) data from the United Kingdom Infra-Red Telescope (UKIRT).
The journal of our optical and NIR observations, including the derived magnitudes, is given in Table 1.
The OT was also observed from several other optical and infrared telescopes,
and the counterpart was subsequently detected in the mm-band at 250 GHz (Bertoldi 2000), and at radio (8.46 GHz) wavelengths
(Berger & Frail 2000)
.
Papers detailing the properties of the counterpart of
GRB 000301C have been presented at radio and mm wavelengths
(Berger et al. 2000) and
in the infrared (Rhoads & Fruchter 2001),
and optical bands (Masetti et al. 2000; Sagar et al. 2000).
| Telescope | date | seeing | filter | exp. time | mag |
| (2000, UT) | arcsec | (sec) | |||
| NOT | Mar 3.14 | 2.3 | R | 900 |
|
| NOT | Mar 3.17 | 2.2 | R | 900 |
|
| NOT | Mar 3.19 | 2.1 | R | 900 |
|
| NOT | Mar 3.20 | 2.2 | B | 900 |
|
| NOT | Mar 3.21 | 2.3 | R | 900 |
|
| NOT | Mar 3.22 | 2.3 | B | 900 |
|
| NOT | Mar 3.24 | 2.3 | U | 900 |
|
| NOT | Mar 3.25 | 2.2 | R | 900 |
|
| NOT | Mar 3.26 | 2.0 | I | 900 |
|
| NOT | Mar 3.27 | 2.3 | I | 300 |
|
| CAHA 2.2m | Mar 4.14 | 1.4 | I | 1440 |
|
| USNO | Mar 4.39 | 2.0 | I | 480 |
|
| USNO | Mar 4.40 | 2.1 | V | 720 |
|
| USNO | Mar 4.41 | 2.0 | B | 1200 |
|
| USNO | Mar 4.42 | 1.8 | R | 600 |
|
| USNO | Mar 4.48 | 1.6 | R | 1200 |
|
| USNO | Mar 4.49 | 1.6 | R | 1200 |
|
| USNO | Mar 4.50 | 1.6 | R | 1200 |
|
| USNO | Mar 4.52 | 1.6 | B | 1200 |
|
| USNO | Mar 4.53 | 1.6 | V | 1200 |
|
| USNO | Mar 4.43 | 2.0 | U | 1200 |
|
| UKIRT | Mar 4.51 | 0.7 | J | 810 |
|
| UKIRT | Mar 4.53 | 0.6 | H | 810 |
|
| UKIRT | Mar 4.55 | 0.5 | K | 810 |
|
| CAHA 2.2m | Mar 5.23 | 1.5 | I | 960 |
|
| ESO VLT | Mar 5.39 | 0.9 | R | 10 |
|
| ESO VLT | Mar 6.39 | 1.1 | R | ... |
|
| NOT | Mar 7.22 | 1.4 | R | 300 |
|
| NOT | Mar 7.24 | 1.4 | U | 3600 |
|
| CAHA 2.2m | Mar 7.23 | 1.1 | I | 960 |
|
| NOT | Mar 8.18 | 1.4 | R | 1200 |
|
| NOT | Mar 8.20 | 1.5 | I | 900 |
|
| NOT | Mar 8.21 | 1.6 | B | 1100 |
|
| NOT | Mar 8.25 | 1.9 | U | 3700 |
|
| NOT | Mar 9.15 | 1.4 | R | 2000 |
|
| NOT | Mar 9.20 | 1.6 | U | 5400 |
|
| NOT | Mar 9.24 | 1.4 | B | 1200 |
|
| NOT | Mar 9.26 | 1.2 | I | 900 |
|
| CAHA 2.2m | Mar 10.05 | 1.3 | I | 960 |
|
| USNO | Mar 10.40 | 3.0 | B | 1800 |
|
| CAHA 2.2m | Mar 11.21 | 1.2 | I | 1440 |
|
| ESO 2.2m | Mar 11.39 | 2.4 | R | 3200 |
|
| USNO | Mar 12.44 | 1.9 | R | 4800 |
|
To avoid contamination from the nearby star A (located at a separation
of
west and
south of the OT in
Fig. 3), we measured the magnitude of the OT relative to
stars in the field by performing Point Spread Function (PSF)
photometry, using DAOPHOT II (Stetson 1987, 1997).
There are several bright and
unsaturated stars in the field from which a good PSF could be
determined.
For the data presented here, there is no indication of a contribution from a host galaxy to the emission at the position of the OT (see Sect. 7.2 for a discussion of the host galaxy). Hence, extended emission from a faint galaxy at the position of the OT will not affect the PSF photometry appreciably (much less than observational errors). The quality of the PSF photometry was checked by subtracting the PSFs from the images of star A and the OT. In all frames the residuals are consistent with being shot-noise.
To avoid errors due to colour terms or colour differences in our photometry (the conditions during most of the observations at the NOT were possibly non-photometric due to increasing amounts of Saharan dust in the atmosphere over the telescope at the time of observations), the magnitudes of the OT for all our optical photometry were calibrated relative to stars of similar colours in the field.
The photometric standard
calibration
of the field was performed at the USNOFS 1.0-m telescope and is
available in Henden (2000). This calibration has an
estimated zero-point uncertainty of 2 percent, which is well below the
errors in the relative magnitudes. The results of the PSF photometry
are presented in Table 1. The 2000 March 6.39
VLT R-data point has been derived from the March 6 combined
VLT-spectrum (Table 2).
Based on this photometric calibration we conclude that star A showed no sign
of variability within observational errors throughout our observations, and
that it had the following magnitudes:
,
,
,
,
and
.
The UKIRT images were processed using the ORAC imaging data
reduction routines developed for UKIRT (Bridger et al. 2000).
The J, H and K magnitudes of the OT were then measured from the UKIRT
data as follows. First we measured the magnitude of the OT relative to
star A using DAOPHOT II PSF photometry as described above. Then, in order to
transform this magnitude to the standard UKIRT system, we performed
aperture photometry in an aperture with a diameter of
on
calibration images obtained of the standard stars
S868-G and p389-d
from the list of UKIRT faint standards
and on star A. The estimated error
in the zero-point is about 0.05 in each of J, H and K. We have
assumed negligible extinction difference between standard and program
field. The results of these measurements are presented in
Table 1.
Spectroscopic observations were carried out on 2000 March 5 and 6 UT with VLT-Antu equipped with FORS1 (for details see the observing log in Table 2). We used the GRIS_300V+10 grism and the GG375 order separation filter, which provide a spectral coverage from 3600 Å to 8220 Å and a dispersion of 2.64 Å/pixel. The effective exposure time was 800 s on March 5.39 UT and 1200 s on March 6.38 UT. Standard procedures were used for bias and flat field correction, and the optimal extraction procedure for faint spectra (described in Møller 2000) was used to extract one dimensional spectra.
| Date | Exposure time | Airmass | Slit width |
| (2000 UT) | (s) | (
|
|
| Mar 5.39 | 400 | 1.732-1.745 | 1.3 |
| Mar 5.40 | 400 | 1.719-1.729 | 1.3 |
| Mar 6.38 | 600 | 1.772-1.801 | 1.0 |
| Mar 6.39 | 600 | 1.745-1.767 | 1.0 |
The position angle of the long slit was chosen such that both the OT and
star A were centred onto the slit. From the magnitude of star A we calibrated the flux of the trace of the optical counterpart.
The spectral flux calibration derived for the OT on March 5 is consistent with the optical photometry displayed in Table 1.
We derive a value for the spectral index of
on
March 5 and
on March 6, corrected for interstellar
extinction of
,
using the
dust maps of Schlegel et al. (1998).
![]() |
Figure 4: Combined VLT+FORS1 spectrum of GRB 000301C from 2000 March 5+6 UT. The spectrum is normalized to 1 in the continuum. The atmospheric absorption bands and residuals from strong sky-lines are marked, as well as the 4 absorption lines listed in Table 3. The spectrum is binned to 7 Å pixels, and the lower curve shows the noise (per pixel) |
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The combined spectrum, reproduced in Fig. 3, has a resolution of 14 Å FWHM, and signal-to-noise (S/N) in the range 15-30 per resolution element redwards of 4000 Å. From 4000 Å to 3600 Å the S/N drops rapidly.
Due to the poor resolution, only very strong absorption lines can be detected individually. In Table 3 we list the only four absorption features which were detected at a S/N in excess of 4.5. Two of the features were found bluewards of 4000 Å, and were initially ignored. The line at 4712 Å is broader than the resolution profile, and we tentatively identified it as a possible C IV absorption complex with redshifts in the range 2.038 to 2.042. With this identification, the other three features would fit the proposed identifications given in Table 3. Note, however, that the Si II 1260 line is far too strong and wide to be a single line, and we hence assume that it is a blended feature. The Fe II 2600 line is strong and narrow, but also this line seems excessively strong given the lack of other strong Fe II lines.
| Line | Identification |
|
|
|
| (Å) | (Å) | |||
| 1 | Ly |
3693.56 | 67.07 | 12.09 |
| 2 | Si II 1260 | 3843.09 | 18.99 | 2.03 |
| 3 | C IV 1549 | 4712.23 | 3.76 | 0.82 |
| 4 | Fe II 2600 | 7909.03 | 6.29 | 1.21 |
In order to provide a more strict test of our proposed identification, and to obtain an accurate value for the redshift, we proceeded as follows. First we shifted and stacked pieces of the spectra where we would expect common low ionization lines. We selected the singly ionized species of Si, C and Fe, all of which are known as strong absorbers in quasar absorption line systems. In total our spectrum covers positions of the lines Fe II 1608, Fe II 2344, Fe II 2374, Fe II 2382, Fe II 2586, Fe II 2600, Si II 1260, Si II 1304, Si II 1526, and C II 1334. Si II 1260 (at 3832 Å) was in the very low S/N part of spectrum, and almost certainly blended, so it was not included. Treating each ion separately, a weighted mean absorption feature was calculated using the oscillator strength of each line as statistical weight.
![]() |
Figure 5: Left: Upper panel: Oscillator strength weighted mean absorption lines of Fe II, Si II and C II, lined up in redshift space for easy comparison (see text for details). Lower panel: The combined "Low Ionization'' absorption feature (weighted mean of the three sections of spectrum shown above). Right: Upper panel: The combined "Low Ionization'' absorption feature lined up with the C IV trough. Lower panel: Combined "Metal Absorption Feature''. All the sections of spectra have been normalized to 1 in the continuum, but shifted along the abscissa by suitable off-sets. Note that none of the figures start at 0, instead the scale on the abscissa provides the proper reference |
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The regions of the co-added spectra for each of the ions Fe II, Si II and C II, transformed into redshift space, is shown in the left panel of Fig. 5. A combined "Low Ionization'' absorption feature (bottom of left panel of Fig. 5) was obtained by co-addition of the three sets of features, but using the number of lines as statistical weights. The redshift range searched for low ionization absorption systems by this method was 1.95-2.14 and no other candidate systems were found in this range. For comparison of the redshifts, we plot in the right panel of Fig. 5 again the combined "Low Ionization'' absorption feature together with the C IV absorption trough. The bottom panel here shows the combination of all the lines. Given the significance of this combined "Metal Absorption Feature'', we conclude that the tentative identification of this system is confirmed.
| |
Figure 6:
Upper panel: The "Combined Metals'' absorption
feature from Fig. 5 is shown here for comparison.
Lower panel: Spectral region
around Ly |
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The oscillator strength weighted mean observed equivalent width of the
Fe II lines is 2.56 Å, which is strong enough that by
comparison to known quasar absorbers one would expect this to likely
have a column density of neutral Hydrogen in excess of
.
Such absorbers are known as Damped
Ly
Absorbers (DLAs), and hold a special interest because of
the large amounts of cold gas locked up in those objects (Wolfe et al. 1995; Storrie-Lombardi et al. 1997). It is
commonly assumed that the DLAs are the progenitors of present day disk
galaxies, but they have proven extremely difficult to identify (see
e.g. Møller & Warren 1993; Kulkarni et al. 2000b).
Observational evidence has been accumulating (Møller & Warren
1998; Fynbo et al. 1999) which suggests that a likely reason
why DLA galaxies are so hard to identify is their small gas
cross-sections and faint magnitudes, causing them to stay hidden
under the point spread functions of the bright quasars. A GRB selected
DLA galaxy sample would not be hampered by this problem once the OT
has faded sufficiently, and could as such help greatly in
understanding the nature of DLA galaxies. We shall therefore now
briefly consider the low S/N part of the GRB spectrum below
4000 Å, to investigate if any information concerning the
H I column density can be extracted.
In Fig. 6 (lower panel) we have plotted the
spectral region around Ly
,
and for comparison of redshifts,
the "Combined Metals'' feature (upper panel). Also plotted on the
lower panel is the noise per bin (for redshift binsize = 0.003).
It is clearly seen that the spectrum drops steeply before the
expected central position of the Ly
line,
and well before the S/N drops below detection. One likely explanation
for this is the presence of a very broad Ly
absorption
line. To quantify this we have modelled several Ly
absorption
lines, all at redshift 2.0404, and calculated the
of their
fit to the data in the range 3700 Å to 3750 Å.
For
the
per degree-of-freedom DOF is 6.46 which
confirms that an absorption feature is indeed present.
The formal
minimum is found at
(
per DOF = 0.86),
but any value within a factor 3 of this is acceptable.
It should be recalled that the above estimate, in a strict
sense, only applies in the case the OT lies "behind'' the absorbing
cloud. In case the OT is in fact embedded "inside'' a DLA cloud,
resonant scattering of Ly
photons may alter the
profile of the absorption line somewhat. In the present case this
is a detail which the quality of our data will not allow us to
discern.
The wide wavelength coverage obtained around 2000 March 4.5 UT allows us to
construct the multi-wavelength spectrum of the afterglow, by using our USNO
and UKIRT data. Most fireball models (e.g. Sari et al. 1998;
Piran 1999; Mészáros 1999 and references therein)
and observations of previous afterglows suggest a power-law Spectral Energy
Distribution (SED). However, a global fit to the broadband SED of
GRB 000301C by
Berger et al. (2000) demonstrates that the mm-optical
range cannot be described by a single power-law. Thus, we have only
considered wavelengths shorter than IR when fitting the SEDs presented in this
section. This gives eight measurements in the period March 4.39-4.55 UT,
namely UBVRIJHK. The eight measurements, plotted against
together with the VLT spectrum in Fig. 7, allow us to
constrain the SED of the OT at this epoch.
![]() |
Figure 7:
Spectral energy distribution of the OT on 2000 March
4.39-4.55 UT (
|
| Open with DEXTER | |
As extinction is highly wavelength dependent, a progressive deviation
from a pure power-law fit can be explained as being due to dust extinction
in the GRB host galaxy. In order to test this possibility, we first fit a
power-law to the data in the NIR-optical range with the addition of an
intrinsic extinction law, i.e., using the expression
,
where
is the rest frame
extinction in magnitudes at the rest frame frequency
.
Four extinction
laws have been applied in order to establish a relationship between
and
.
Following Rhoads & Fruchter (2001), we have fitted
the extinction curves for the Galaxy and Magellanic Clouds published by Pei
(1992). Pei (1992) provides extinction laws for the
Milky Way (MW), the Large Magellanic Cloud
(LMC), and the Small Magellanic Cloud (SMC)
based on their different proportions in the dust-to-gas ratio (1:1/5:1/10)
and in the abundance of heavy elements (1:1/3:1/8). The most significant
difference is the sequential change in the strength of the 2175 Å
extinction feature, prominent for the MW, moderate in the
LMC, and nonexistent for the SMC extinction curve. It
is important to note that for the redshift of GRB 000301C this
extinction feature falls in the observed R-band. So, the presence of this
feature would result in a clear decrease in the R-band flux compared
to the I and
V-bands. The MW extinction curve requires an equal amount of
graphite and silicate grains, while the SMC extinction curve can
be explained by silicate grains only, with the LMC extinction law
as an intermediate stage.
We have applied these four extinction laws to our data in order to infer
qualitative information about the dust-to-gas ratio, the abundance of heavy
elements and the composition of the dust in the host galaxy of
GRB 000301C. We leave
as a free parameter, so fitting a
function like
allows us to determine
and
simultaneously. The values of
are displayed in Table 4 for each case.
| AV | |||
| mag | |||
| No extinction | 1.69 |
|
0 |
| MW, Pei (1992) | <0 | ||
| LMC, Pei (1992) | <0 | ||
| SMC, Pei (1992) | 0.91 |
|
|
As expected by the lack of the absorption bump in the R-band, the
MW and the LMC extinction laws are completely inconsistent
with our data. In fact, both fits imply an unphysical negative extinction
(see Table 4). This is because the R-band flux is slightly
over the linear interpolation between the I-band and V-band fluxes (in a
Log-Log space), and both of these two extinction laws fit
the 2175 Å bump as an
emission feature instead of an absorption bump. To illustrate the problem
with the MW and LMC extinction curves, we have, in the
lower panel of Fig. 7, plotted the effect of having the
MW and LMC extinction laws with the parameters derived
for the SMC extinction law (
,
AV=0.09). As seen,
the shapes of both SEDs are incompatible with our UBVRIJHK measurements.
The quality of the MW, LMC and SMC and
unextincted SEDs can also be compared checking the flux predicted at
GHz (rest-frame), where Berger et al. (2000) reports a flux of
mJy at 250 GHz
on March 4.29 UT.
Extrapolating the four extinction curves, we
obtain the following fluxes in increasing order; 5.0 mJy (SMC),
18.1 mJy (No extinction), 33.9 mJy (MW) and 51.6 mJy
(LMC). As with the NIR-optical range, the SMC extinction
provides the most reasonable results. The actual measured flux in mm is
below the value predicted by the mm-optical extrapolation, because the
pure power-law assumption is not correct in the mm-NIR spectral
range and an additional curvature effect is present in the SED, as
demonstrated by Berger
et al. (2000) (see their Fig. 1). Thus, the
value of
for the SMC-fit given in
Table 4 should be taken as a good indication of the
real extinction, although strictly
speaking it is just an upper limit.
In conclusion, the featureless SMC extinction law provides the best fit to our data, improving the quality of the fit obtained for an unextincted afterglow (see Table 4). It is interesting to note the dramatic dependence of the quality of fit on the existence of the 2175 Å absorption bump. Extinction laws with high moderate dust-to-gas ratios that produce such an absorption feature do not provide good fits to our data points. Therefore, the spectral energy distribution of GRB 000301C supports a scenario where the host is in the early stages of chemical enrichment.
The power-law + extinction fits to the SED in the NIR-optical range
allow us to predict the UV flux at the spectral range of MAMA-HST when the UV
spectrum was obtained at 2000 March 6.375 UT (Smette et al. 2000)
assuming that the shape of the SED has not changed between the two
epochs. This assumption is supported by the imaging data (Sect. 6.3).
First, we consider the best fit to the SED at 2000 March 4.39-4.55 UT
and calculate the flux at March 4.39-4.55 UT at 3000 Å. Then,
making use of the light curve models (presented in Table 6),
we estimate the value of the flux at 3000 Å for March 6.375 UT.
The predicted flux ranges from 5.9 10-18 erg
cm
s-1 Å-1 to 7.9 10-18 erg
cm
s-1 Å-1,
depending on the light curve model.
A final analysis (Smette et al. 2001) of the MAMA-HST
data revealed a flux of
7.3
+0.8-1.8 10-18 erg cm-1 consistent with our extrapolation.
From our UBRI photometric data (presented in Table 1) we have multi-band optical coverage from 2 to 10 days after the burst-trigger (on March 1.41 UT). When analysing the colours, we find that the simplest reliable fit is for constant colours. Thus we find no evidence for optical chromatic evolution for the afterglow during the period of observations (see Fig. 8). For these constant fits, we obtain the values presented in Table 5. These values are not corrected for Galactic or intrinsic extinction.
![]() |
Figure 8: Fitting the colours from the optical photometry from 2000 March 3 to March 11 UT, assuming achromatic evolution. The solid line indicates the best fit, with the dashed lines representing the error-range. The photometry is from Table 1. The results of the fitting is presented in Table 5 |
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According to the simple fireball model the optical afterglow
should follow a power-law decay,
(Sari et al. 1998). However, a single power-law
is excluded at more than the 99.9% confidence level. The
parameters for this power-law are given in Table 6.
The photometry suggests that the optical afterglow follows a shallow
power-law decay for the first few days and then steepens. This
behaviour has been seen previously in GRB 980519 (Jaunsen
et al. 2001), GRB 990123 (Kulkarni
et al. 1999), GRB 990510 (Harrison
et al. 1999), GRB 991208
(Castro-Tirado et al. 2001) and GRB 000926
(Fynbo et al. 2001b and is
predicted by many models for gamma-ray bursts (see below). Sagar
et al. (2000) report that there are seven components to the
R-band light curve. Here we are primarily interested in the
overall structure of the light curve, not the structure at small time
scales. Therefore, we fit a broken power-law of the form,
| Colour | Value | |||
| U-B | -0.49 | 0.06 | 0.41 | 0.26 |
| B-R | 0.91 | 0.03 | 1.67 | 0.83 |
| R-I | 0.49 | 0.04 | 0.51 | 0.20 |
| B-I | 1.43 | 0.05 | 0.33 | 0.14 |
| U-I | 0.92 | 0.07 | 0.64 | 0.36 |
| U-R | 0.40 | 0.05 | 1.35 | 0.75 |
| V-R | 0.44 | 0.05 | - | - |
| Single Power Law | Broken Power Law | Smooth Function | |
|
|
|
|
|
| |
|
|
|
| |
|
|
|
| 0 |
|
|
|
|
|
|
|
|
|
|
|
|
|
| 4.499 | 1.023 | 1.090 | |
| DOF | 33 | 31 | 31 |
The data was corrected for Galactic reddening and extinction
before the fits were made. No corrections were made for reddening or
extinction in the host galaxy. The photometry was transformed to the
R band using the colours given in Table 5 and
then converted to units of flux using a photometric zero point of
erg cm-1 s-1 Hz-1(Fukugita et al. 1995).
The best fit to the combined UBRI photometry is listed in
Table 6, and shown in Fig. 9.
To test the sensitivity of the results to the fitting function, we also
fit our data with the smooth function used by Stanek et al. (1999,
their Eq. (1)) on GRB 990510. The results are
given in Table 6. The broken power-law gives the
smallest chi-square value, and the errors in the individual parameters
are smaller for the broken power-law fit than they are for the smooth function.
The correlation coefficient between
and
is
-0.39 and the coefficient between
and
is -0.84.
The broken power-law fit is consistent with the data at the 43%
confidence level.
Even though we, from the theory of fireballs, would expect that the light-curve
evolution is a smooth function, we find in the case
of GRB 000301C, in agreement with Berger et al. (2000),
that the broken power-law provides the most reliable fit.
Additionally, a broken power-law provides the most reliable metod
of determining the time when the decay of the light has steepened,
and thus is a useful way of parameterising the data.
![]() |
Figure 9:
The upper panel shows the UBRI photometry from
Table 1 and the best-fitting broken power-law fit
to the data. The photometry was offset to the R band using the
colours given in Sect. 6.3 (see the text). The
horizontal line at the location of the break shows the 1- |
| Open with DEXTER | |
We combined all our UBRI-data (Table 1) with those from the literature. Figure 10 shows the best-fitting broken
power-law for all of the UBRI data in the literature
(Sagar et al. 2000 and references therein)
and Table 1. This data was
shifted to the R band in the manner described above. The parameters
of the fit are shown in Fig. 10 and are not
significantly different from the parameters of the broken power-law
that was fit to our data (see Table 6).
The conspicuous short-term behaviour of the light-curve has been detailed
by Masetti et al. (2000), Sagar et al. (2000)
and Berger et al. (2000). Garnavich et al.
(2000) find that the variation of the lightcurve can be
interpreted as a microlensing event, peaking about 3.5 days after the burst,
superposed on a power-law broken at
days.
This superposed event peaks at a more sparsely sampled period in our data,
coinciding partly with where we identify the break. Thus it is not
possible, from our data, to further constrain the existence of such an event.
We choose here to work only with the data presented in
Table 1 as it represents a consistently derived set.
![]() |
Figure 10: This Figure is analogous to Fig. 9, but instead shows the data from Table 1 (filled circles) together with all the UBRI photometry presented in the literature (Rhoads & Fruchter 2001 and references therein) (open circles) and with the best-fitting broken power-law fit to this data |
| Open with DEXTER | |
The fit to the multi-colour light curves shows a break at
days, with the light curve steepening from
to
,
i.e., by
.
A broken light curve can arise in a
number of circumstances: i) If the frequency separating fast
cooling electrons from slow cooling ones moves through the optical at
,
the resulting light curve would steepen by
(Sari et al. 1998). ii) The light curve may
also steepen if a spherical fireball slows down to a non-relativistic
expansion (Dai & Lu 1999), resulting in
for our value of
.
iii) If the outflow is
collimated with a fixed opening angle, the break in the light curve
occurs when the relativistic beaming of the synchrotron radiation
becomes wider than the jet opening angle (Mészáros & Rees
1999). In this case the break is a geometrical effect and the
steepening is
.
iv) If the afterglow
arises in a sideways expanding jet, the steepening will be
(Rhoads 1999) for our value of
.
The above estimates all assume a constant mean density distribution
of the ambient medium. We note that collimated outflows in general
result in faster decaying light curves than the spherically
symmetric ones. If the mean density distribution is not constant,
e.g. it has a stellar wind density profile, the light curves also
decay faster, but the break will be less pronounced
(Panaitescu et al. 1998).
Based on the light-curve properties alone, the model that best fits the
observations is that of a sideways expanding jet in an ambient medium with a
constant mean density distribution. In that interpretation, the observed light
curve indices imply an electron energy distribution index of
that results in a theoretical spectral index of
.
This is in agreement with the spectral
index of
inferred from our spectroscopic
observations when correcting for
extinction in the host galaxy (Sect. 6.2),
independently strengthening the described model for the afterglow.
With a combined fluence in the 25-1000 KeV range of
4 10-6 erg cm-2, and a redshift of
z=2.0404, the isotropic energy release of GRB 000301C is
E = 4.6
1052 erg. Following Rhoads (1999),
the energy estimate and the light curve break
time,
days, implies a jet opening angle, at that
time, of
,
where n is the number
density of the ambient medium (in units of cm-3), and the break is assumed to occur when the opening angle equals the bulk Lorentz factor,
.
This interpretation is similar to that of GRB 990510 which was
almost 5 times more energetic, but had a jet opening angle of
approximately
,
leading to an earlier break in the light
curve. The best fit to GRB 990510 was a smooth function (e.g. Stanek
et al. 1999; Harrison et al. 1999; Holland et al. 2000), as compared to a broken power-law in the case of
GRB 000301C.
The host galaxy appears to be very faint. There is no evidence
for any extended emission from a host galaxy in any of the data
presented in this paper. Deep images obtained with
HST+STIS about 1 month after the GRB indicate that any host galaxy
must be
(Fruchter et al. 2000).
Hence, we can safely conclude that the host galaxy of GRB 000301C is
very faint compared to other known populations of galaxies at high redshifts.
From fitting extinction curves to our photometry, we have found
evidence for some extinction (
)
in the
host galaxy. The AV derived from the best fit corresponds to an
absorption at rest-frame 1500 Å of about 0.4 magnitudes.
For comparison, Lyman Break Galaxies (LBGs) at slightly higher redshifts
(
-3.5) on average have values of extinction at
rest frame wavelength
1500 Å of approximately 1.7 magnitudes, and, in rare cases up to 5 magnitudes (Steidel et al. 1999). Hence, the faint optical
appearance of the host galaxy relative to the star-forming LBGs at
high redshift is most likely not imposed by massive extinction, but is
rather due to a lower overall star formation rate of the host galaxy.
As the host galaxy furthermore has a very high H I column
density, log(NH I
as derived from the Ly
absorption feature and supported by the strong Lyman break
(Smette et al. 2000), it is interesting to compare
with the population of galaxies identified as
Damped Ly
Absorbers (Wolfe et al. 1986) in the
spectra of background QSOs. These galaxies have H I
column densities higher than log(NH I)=20.3. Based on
the luminosity function of LBGs and the typical impact parameters of
DLAs, Fynbo et al. (1999) show that the majority
of DLAs at z=3 must be
fainter than the current flux limit for LBGs of R=25.5 and that there
hence is a very abundant population of galaxies fainter than the LBG
flux limit. A similar conclusion has been reached by Haehnelt et al.
(2000).
The dust-to-gas ratio towards the line-of-sight of GRB 000301C gives
a value of
cm
2
= 0.6 10-22 cm-2. This upper limit is, within errors,
consistent with the expected
for DLAs. The corresponding value for the Milky Way is
2
10-22 cm-2 (Allen 2000).
It is still uncertain what fraction of the integrated star formation rate at high redshift is accounted for by the LBGs and what fraction has to be accounted for by galaxies further down the luminosity function. The relative occurrence of GRBs in a given population of galaxies is expected to be proportional to its relative contribution to the total star formation rate (Totani et al. 1997; Wijers et al. 1998; Mao & Mo 1999; Blain & Natarajan 2000). However, so far only one GRB (GRB 971214 at z=3.418) is confirmed to have occurred in a galaxy similar to the faint members of the LBGs selected in ground based surveys (Odewahn et al. 1998). The fact that GRB 000301C occurred in an intrinsically very faint galaxy and that most GRBs with identified OTs have occurred in L* or sub-L* galaxies, suggest that a large fraction of total star formation at high redshift occurs in a population of galaxies that is further down the luminosity function than the bright LBGs found in ground based surveys and that is likely to have a large overlap with the DLAs.
GRB 000301C is so far the GRB of shortest duration, for which a
counterpart has been detected.
The high-energy properties of the burst are consistent
with membership of the short-duration class
of GRBs, though GRB 000301C could belong
to the proposed intermediate class of GRBs or the extreme short
end of the distribution of long-duration GRBs.
Our VLT-spectra show that GRB 000301C occurred at a redshift
of
.
The light curve of the optical transient is
well-fitted by a broken power-law and it is consistent with being
achromatic. From the light-curve properties we find that the best model
for GRB 000301C is that of a sideways expanding jet in an ambient
medium of constant density.
This interpretation is further supported by the achromatic
light-curve evolution, and by the agreement between the theoretically
predicted and observationally derived spectral indices. The spectral energy
distribution at March 4.5
reveals SMC-like extinction in the host galaxy at a level of
AV < 0.10, which is significantly lower than for
the strongly star-forming LBGs. Hence, the extreme faintness of the
host galaxy indicates a low overall star-formation rate in the
host galaxy, raising the possibility that the host may be a chemically
less evolved, relatively low-luminosity galaxy containing SMC-type
dust. We argue that there may be a connection between the host galaxy of
GRB 000301C and DLAs, suggesting
that substantial star-forming activity at high redshift takes place in
relatively faint galaxies. Future studies of high redshift GRBs will further
help explore this connection.
Acknowledgements
We wish to thank our anonymous referee for providing many helpful comments and suggestions. Support for this programme by the director of the Nordic Optical Telescope, professor Piirola, is much appreciated. We also acknowledge the assistance given by the ESO service observing team. J. Gorosabel acknowledges the receipt of a Marie Curie Research Grant from the European Commission. J. Hjorth acknowledges support from the Danish Natural Science Research Council (SNF). B. Thomsen acknowledges support from the Danish Natural Science Research Council for funding the Danish Centre for Astrophysics with the HST. G. Björnsson acknowledges support from the Icelandic Research Council and the University of Iceland Research Fund. I. Burud is supported by Pôle d'Attraction Interuniversitaire, P4/05 (SSTC, Belgium). K. Hurley acknowledges support for Ulysses operations under JPL Contract 958056, for IPN operations under NASA LTSA grant NAG5-3500, and for NEAR operations under the NEAR Participating Scientist program (NAG 5-9503). We are grateful to R. Gold and R. McNutt for their assistance with the NEAR spacecraft. R. Starr is supported by NASA grant NCC5-380. We are indebted to T. Sheets for her excellent work on NEAR data reduction. Special thanks also go to the NEAR project office for its support of post-launch changes to XGRS software that made these measurements possible. In particular, we are grateful to John R. Hayes and Susan E. Schneider for writing the GRB software for the XGRS instrument and to Stanley B. Cooper and David S. Tillman for making it possible to get accurate universal time for the NEAR GRB detections. The data presented here have been taken using ALFOSC, which is owned by the Instituto de Astrofísica de Andalucia (IAA) and operated at the Nordic Optical Telescope under agreement between IAA and the NBIfAFG of the Astronomical Observatory of Copenhagen. Additionally, the availability of the GRB Coordinates Network (GCN) and BACODINE services, maintained by Scott Barthelmy, is greatly acknowledged. We acknowledge the availability of POSS-II exposures, used in this work; The Second Palomar Observatory Sky Survey (POSS-II) was made by the California Institute of Technology with funds from the National Science Foundation, the National Aeronautics and Space Administration, the National Geographic Society, the Sloan Foundation, the Samuel Oschin Foundation, and the Eastman Kodak Corporation.