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Since the end of 1996 the GRBM detected two giant flares from SGR1900+14
and 22 short typical SGR bursts from the followig sources: 11 from
SGR1900+14, 9 from SGR1627-41, and 2 from SGR1806-20.
Out of this 22 short bursts, only 4 have triggered the off-line GRB quest
(table
);
the remaining 18 have not been discovered automatically, owing to the
spectral softness of SGR bursts, below the HR threshold (eq.
);
on the other side, this proves the effectiveness of the GRB search algorithms
in distinguishing the classical GRBs from SGRs (only 4 out of 22 bursts + 2
giant flares have been mistaken for GRBs by the automatic off-line quest).
The other 18 SGR bursts show no AC (
100 keV) significant signal in any
of the four GRBM units; as their duration is
1 s, except for
some of them, it has been possible to recognize them only through the analysis
of HTR data. Due to this, the search for SGR events was limited to the set of
GRBM on-board triggered events: 15 out of the remaining 18 SGR bursts detected with
the GRBM resulted from a cross-check between the list of
GRBM on-board triggers and a recent list of SGR events detected by Konus/WIND
([Aptekar, et al., 2001]); the remaining 3, all from SGR1900+14, show HTR light
curves that are typical of SGRs, so we classified them as true SGR1900+14 bursts;
all occurred when the source was extremely active.
Finally, in addition to these 22 bursts, other two SGR burst candidates
have been detected: 980831, UT 22:52:40.71, attributed to SGR1900+14,
and 980618, UT 03:44:00.04, attributed to SGR1627-41; since they have
not been detected by Konus/WIND, they need confirmation.
Table
reports all these SGR events as seen with the
GRBM; the two SGR burst candidates have been classified as ``uncertain''.
Table:
SGR Events detected with GRBM.
SGR |
Date |
U.T. |
 |
 |
 |
Comments |
name |
|
|
( ) |
( ) |
(s) |
|
1900+14 |
30 May 1998 |
23:27:35.28 |
216.5 |
-3.8 |
 |
|
1900+14 |
27 Aug 1998 |
10:22:15.69 |
240.8 |
+47.5 |
 |
Giant Flare |
1900+14 |
27 Aug 1998 |
11:06:57.39 |
240.8 |
+47.5 |
 |
No Konus det. |
1900+14 |
29 Aug 1998 |
10:16:32.30 |
152.9 |
-24.5 |
 |
Intermediate Fl. |
1900+14 |
29 Aug 1998 |
18:18:43.52 |
152.9 |
-24.5 |
 |
|
1900+14 |
31 Aug 1998 |
16:34:40.36 |
260.6 |
+41.8 |
 |
No Konus det. |
1900+14 |
31 Aug 1998 |
22:52:40.71 |
260.6 |
+41.8 |
 |
Uncertain |
1900+14 |
01 Sep 1998 |
17:06:27.06 |
114.7 |
+36.4 |
 |
Unusual |
1900+14 |
02 Sep 1998 |
07:23:50.13 |
114.7 |
+36.4 |
 |
No Konus det. |
1900+14 |
15 Sep 1998 |
18:17:40.98 |
355.6 |
+89.8 |
 |
NFI Observation |
1900+14 |
10 Jan 1999 |
08:39:01.51 |
11.1 |
-8.1 |
 |
|
1900+14 |
05 Apr 1999 |
08:21:00.70 |
65.2 |
+40.2 |
 |
Ulysses det.; hard |
1900+14 |
18 Apr 2001 |
07:55:11.50 |
276.7 |
+9.0 |
 |
Giant Flare; WFC1 det.! |
1900+14 |
02 Jul 2001 |
03:34:07.16 |
207.8 |
+19.1 |
 |
HETE-II det. |
|
|
|
|
|
|
|
1627-41 |
17 Jun 1998 |
19:58:29.95 |
221.6 |
+6.8 |
 |
|
1627-41 |
17 Jun 1998 |
20:06:28.39 |
221.6 |
+6.8 |
 |
|
1627-41 |
17 Jun 1998 |
21:04:38.75 |
221.6 |
+6.8 |
 |
|
1627-41 |
17 Jun 1998 |
21:37:18.67 |
221.6 |
+6.8 |
 |
|
1627-41 |
17 Jun 1998 |
21:57:08.42 |
221.6 |
+6.8 |
 |
|
1627-41 |
18 Jun 1998 |
03:28:28.03 |
221.6 |
+6.8 |
 |
|
1627-41 |
18 Jun 1998 |
03:44:00.04 |
221.6 |
+6.8 |
 |
Uncertain |
1627-41 |
22 Jun 1998 |
13:29:54.94 |
140.8 |
-18.0 |
 |
|
1627-41 |
22 Jun 1998 |
14:11:24.42 |
140.8 |
-18.0 |
 |
|
1627-41 |
25 Jun 1998 |
10:56:18.79 |
133.8 |
+21.0 |
 |
|
|
|
|
|
|
|
|
1806-20 |
22 Nov 1996 |
02:17:39.61 |
9.1 |
+36.7 |
 |
|
1806-20 |
01 Jun 1999 |
10:00:05.29 |
173.6 |
+34.4 |
 |
|
The BeppoSAX local direction of the SGR sources is expressed by the local
angles
and
; both fluence (counts) and duration (
)
have been estimated from the 40-700 keV data, owing to the spectral
softness of SGR bursts. The last column reports a comment for some bursts,
e.g. when the burst has not been detected by Konus, when other experiments
detected it in addition to Konus; in particular, the SGR1900+14 burst
occurred on April 05, 1999 was detected by Ulysses as well: the Ulysses-BeppoSAX
annulus indeed included the SGR1900+14 position, making it the best candidate
([Preger et al., 1999b]). This burst has the peculiarity of an unusual spectral
hardness: actually, it triggered the off-line trigger conditions, thanks to
its average
, which is very high for usual SGR bursts
(
), but, on the other side, too low for short duration GRBs, whose
average HR has been found to be
(sec.
).
However, other bursts from SGR1900+14 look particularly hard, like in the
case of the burst occurred on January 10, 1999, (
,
confirmed by BATSE and Ulysses data ([Woods et al., 1999b]).
Other bursts from SGR1900+14 have been detected by other experiments as well:
this is the case of the burst occurred on July 2, 2001, first detected by
HETE-II (Ricker et al., GCN 1078), and then confirmed by the GRBM detection
(Montanari et al. , GCN 1081).
The SGR1900+14 burst occurred on August 29, 1998, i.e. two days after the
impressive giant flare of August 27, has been classified as ``intermediate''
burst in table
, owing to its unusual properties;
this burst was also detected by BATSE and RXTE ([Ibrahim et al., 2001]).
One SGR1900+14 burst, occurred on September 15, 1998, was in the field of view
of the NFI/BeppoSAX, while the April 2001 giant flare ([Guidorzi et al., 2001c],
Guidorzi et al. , GCN 1041) was in the WFC1 field of view; the extraordinary
brightness of this flare switched off the WFC by rate protection.
Figure:
GRBM Light Curves of some SGR1900+14 bursts (40-700 keV).
 |
Figure:
GRBM Light Curves of other SGR1900+14 bursts (40-700 keV).
 |
In figg.
,
the time profiles of the short SGR1900+14
bursts are shown; the two giant flares are treated later on.
The energy band is 40-700 keV in all figures, since only in this range
HTR profiles are acquired; the numbers among brackets refer to the GRBM unit
numbers used for the light curves: e.g., ``(1+2+3+4)'' means that the
light curve shown is the sum of all GRBM units curves, and so on.
Figure:
GRBM Light Curves of some SGR1627-41 bursts (40-700 keV).
 |
Figure:
GRBM Light Curves of other SGR1627-41 bursts (40-700 keV).
 |
Similarly, figg.
,
show the time histories
of the bursts from SGR1627-41. In the case of SGR1806-20, fig.
shows both bursts detected with the GRBM; the light curve of 961122 belongs to the
GRBM unit 1, instead of unit 4, that is the brightest, because only the
HTR data of unit 1 are available within the current GRBM archive.
Figure:
GRBM Light Curves of two bursts from SGR1806-20 (40-700 keV).
 |
Next: SGR1900+14: The interesting Case
Up: Soft-Gamma-ray Repeaters
Previous: SGR Main Properties
  Contents
Cristiano Guidorzi
2003-07-31