 
 
 
 
 
 
 
  
We obtained 3 240-channel energy spectra for this event of initial and final times with respect to the trigger time as follows: -60-67 s (interval A), 68-195 s (interval B) and 196-323 s (interval C). We fitted to the three spectra the phenomenologically established spectral law for SGRs: an optically thin thermal bremsstrahlung (OTTB). A 10% systematic error has been added to the statistical error in order to take into account the calibration uncertainties at the large off-axis location of the event.
The time integrated spectrum in interval A cannot be fitted 
with a simple OTTB law, showing 
an excess at high energies (also reported for the March 5th event.
This is likely due to the strong spectral evolution as it appears 
from the 1-s ratemeters (see below).
In fact, from the ratemeter data we note that during the first 
seconds the emitted spectrum is very hard and it becomes much
softer soon after the peak.  
Assuming different spectral components for these two fractions
of interval A, we fitted the energy spectrum with the 
sum of an OTTB and of a single power law (PL,  .The best fit parameters are kT=
.The best fit parameters are kT= keV and photon index
 keV and photon index  
 (reduced
 (reduced  =0.705 with 186 d.o.f.).
We note, however, that the spectrum can equally be fit with the sum
of a PL and a blackbody (BB). In this case the photon index is
=0.705 with 186 d.o.f.).
We note, however, that the spectrum can equally be fit with the sum
of a PL and a blackbody (BB). In this case the photon index is
 , the BB temperature is kT=
, the BB temperature is kT= keV,
and reduced
 keV,
and reduced  =0.74.
We have also tried to fit the spectrum two OTTB laws,
two power laws and a broken power law (that usually fits time-averaged 
spectra of classical gamma-ray bursts) but the fits are unacceptable.
=0.74.
We have also tried to fit the spectrum two OTTB laws,
two power laws and a broken power law (that usually fits time-averaged 
spectra of classical gamma-ray bursts) but the fits are unacceptable.
In interval B from the ratemeter data we do not deduce  
strong spectral variation, therefore we first used a simple OTTB law. 
However, 
the best fit to the spectrum for interval B has a kT= keV
and the reduced
 keV
and the reduced  is 1.996 (75 d.o.f.). We note the
existence of a hard excess, that is likely biasing upward
the determination of the effective temperature. Thence we  
added a PL component to the fit, and the best parameters are
kT=
 is 1.996 (75 d.o.f.). We note the
existence of a hard excess, that is likely biasing upward
the determination of the effective temperature. Thence we  
added a PL component to the fit, and the best parameters are
kT= keV and
 keV and  (reduced
 (reduced  =1.360,
73 d.o.f.).
In this case substituting the OTTB with a BB gives a only slightly worse fit
(reduced
=1.360,
73 d.o.f.).
In this case substituting the OTTB with a BB gives a only slightly worse fit
(reduced  =1.424, 73 d.o.f.) 
with kT=
=1.424, 73 d.o.f.) 
with kT= keV and
 keV and  .
.
In the case of interval C we obtain a satisfactory OTTB fit
with kT= keV (reduced
 keV (reduced  1.06 with 71 d.o.f.).
 1.06 with 71 d.o.f.).
Fig. 5.21 shows the energy spectra and best fit models for the time intervals A, B and C. For A and B we reported the OTTB+PL fit and for C the OTTB.
 
 
 
 
 
 
