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Characterization and evolution of the swift x-ray telescope instrumental background
Author(s) -
C. Pagani,
David C. Morris,
J. L. Racusin,
D. Grupe,
L. Vetere,
M. C. Stroh,
A. Falcone,
J. A. Kennea,
D. N. Burrows,
J. A. Nousek,
A. F. Abbey,
L. Angelini,
A. P. Beardmore,
S. Campana,
M. Capalbi,
G. Chincarini,
O. Citterio,
G. Cusumano,
P. Giommi,
O. Godet,
J. E. Hill,
V. La Parola,
V. Mangano,
T. Mineo,
A. Moretti,
J. P. Osborne,
K. L. Page,
M. Perri,
P. Romano,
G. Tagliaferri,
F. Tamburelli
Publication year - 2007
Publication title -
proceedings of spie, the international society for optical engineering/proceedings of spie
Language(s) - English
Resource type - Conference proceedings
SCImago Journal Rank - 0.192
H-Index - 176
eISSN - 1996-756X
pISSN - 0277-786X
DOI - 10.1117/12.734398
Subject(s) - physics , telescope , vignetting , south atlantic anomaly , x ray telescope , calibration , detector , orbital mechanics , cosmic ray , astrophysics , background radiation , observatory , gamma ray burst , astronomy , radiation , optics , satellite , lens (geology) , van allen radiation belt , nuclear physics , plasma , magnetosphere , quantum mechanics
The X-ray telescope (XRT) on board the Swift Gamma Ray Burst Explorer has successfully operated since the spacecraft launch on 20 November 2004, automatically locating GRB afterglows, measuring their spectra and lightcurves and performing observations of high-energy sources. In this work we investigate the properties of the instrumental background, focusing on its dynamic behavior on both long and short timescales. The operational temperature of the CCD is the main factor that influences the XRT background level. After the failure of the Swift active on-board temperature control system, the XRT detector now operates at a temperature range between -75C and -45C thanks to a passive cooling Heat Rejection System. We report on the long-term effects on the background caused by radiation, consisting mainly of proton irradiation in Swift's low Earth orbit and on the short-term effects of transits through the South Atlantic Anomaly (SAA), which expose the detector to periods of intense proton flux. We have determined the fraction of the detector background that is due to the internal, instrumental background and the part that is due to unresolved astrophysical sources (the cosmic X-ray background) by investigating the degree of vignetting of the measured background and comparing it to the expected value from calibration data.

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