For each configuration obtained by combining each energy
step with a single direction an MNCP simulation has been
produced, using a monochromatic parallel beam of 5x photons;
each single run has given the number of counts
detected by the
th GRBM unit
(
), in the 40-700 keV (GRBM) band, with input photon energy
(
) and incoming direction
(
;
).
The energy grid has been refined to 1 keV steps by interpolating
the measured
by means of cubic splines.
When considering a GRB coming from the local direction
,
with a power law photon spectrum
,
where
is the power law photon index
(which is a good description of real burst spectra at zero order
approximation), the 40-700 keV counts in the
th GRBM unit are
expected to be the following:
The power law photon index is assumed to take the following values:
1.0, 1.5, 2.0 (when
, respectively): these values have been
chosen in order to account for the range of typical photon indices of
measured bursts.
The best estimate of the burst incoming direction is assumed to minimize
the following
statistics:
where expresses the GRB total counts in the
th GRBM
unit in the 40-700 keV (GRBM) channel;
is
the variance of
plus
;
; and
.
In order to refine the
angular grid, for any
the expected counts
(eq.
) have been
interpolated with bicubic splines down to
cells.
The best estimate
for the GRB direction is given,
according to the following procedure: once the
(eq.
) is computed, the solutions that
are likely to be the burst direction are found in correspondence
of the relative minima.
The fact that there are often more than one candidate position
is mainly connected with two factors: first, the geometrical symmetry
of the GRBM configuration, only partially modified by the
surrounding material; second, possible albedo effects due to the
Earth atmosphere, that have not been taken into account yet.
Finally, another similar technique aimed to reconstruct the burst
directions from the total counts left in each GRBM detector unit
was developed by [Preger et al., 1999]: while the minimization
technique was on principle the same, in that case,
the GRBM response matrix was derived from the results of the
on-ground calibration tests ([Amati, 1998]),
performed with different radioactive
sources at different directions with respect to the satellite frame
of reference. In the majority of cases, the two methods have given
consistent results in localizing the same bursts.
For a complete review of the Monte Carlo model see [Calura et al., 2000b],
while for the reconstruction method based on the on-ground
calibrations, see [Preger et al., 1999b].