Given that BATSE gives for each detected GRB a 'rough' direction, peak fluxes values and fluences in 4 bands (from which some spectral information can be derived) and that it is expected to be a well calibrated experiment, we can use the GRBM+BATSE detected GRB sample to perform an in-flight verification of the calibration of the GRBM.
We performed a power-law fit to the BATSE fluences in the 25-50, 50-100 and 100-300 energy bands, to obtain a spectral model for each event. Then, given the source direction reported by BATSE or the high
accuracy position given by the WFC for the BATSE/GRBM/WFC detected events, we
calculated the expected counts in the GRBM and AC ratemeters bands by convolving the photon spectrum derived from BATSE fluences with LS1 or LS3 efficiency at
the source direction.
We find that for those events with directions at an angular distance from LS1 or LS3 axis of 30 the agreement between expected and measured counts
is good. The consistency between expected and measured data increases with
the brightness of the event, indicating that for weak events there can be
differences in BATSE and GRBM fluences estimations due to the different sensitivity of the two experiments.
In Tab. 4.11.2 we report results of this analysis for some of the GRBs also detected in the WFC. The expected count fluences refer to the GRBM band. The expected count fluences error computation accounts for errors of the power-law parameters and GRBM response systematics.
GRB | LS | Expected | Measured | ||
960720 | LS1 | 11.2 | 0.4 | 3700500 | 3250 200 |
970111 | LS3 | 12.4 | 7.6 | 6600015000 | 77200 1500 |
970228 | LS1 | 7.6 | 15 | 150002000 | 13500 800 |
971214 | LS1 | -15.3 | 6.3 | 140001700 | 12200 1700 |
980109 | LS3 | 12.0 | -0.4 | 54001200 | 4800 500 |
980329 | LS3 | 11.0 | 0.4 | 8500012000 | 82100 3200 |