2022
DOI: 10.48550/arxiv.2205.09359
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In-orbit background for X-ray detectors

Abstract: In-orbit background is an unavoidable feature of all space-borne X-ray detectors, and arises both from cosmic sources (diffuse or point-like) and from the interaction of the detectors themselves with the space environment (primary or secondary cosmic rays, geomagnetically trapped particles, activation of spacecraft structures). In this chapter the main background sources are discussed, with their principal effects on the various detector types, and simulation and mitigation strategies are described.

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Cited by 2 publications
(3 citation statements)
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“…Because of the interaction of charged particles with the spacecraft and the payload structure during the SAA passages, the background increases and decreases immediately upon the entrance and exit of the SAA (Campana 2022), which leads to short-term temporal variation in data. This can be seen in the individual orbital segments of the 1-s light curve (shown in the solid blue line in the top plot of Fig.…”
Section: Data Cleaning For Short-term Variation In Datamentioning
confidence: 99%
See 1 more Smart Citation
“…Because of the interaction of charged particles with the spacecraft and the payload structure during the SAA passages, the background increases and decreases immediately upon the entrance and exit of the SAA (Campana 2022), which leads to short-term temporal variation in data. This can be seen in the individual orbital segments of the 1-s light curve (shown in the solid blue line in the top plot of Fig.…”
Section: Data Cleaning For Short-term Variation In Datamentioning
confidence: 99%
“…X-ray background consists of multiple sources such as cosmic background radiation, induced radioactivity, trapped particles near the SAA, Earth Albedo, etc. (Campana 2022). A careful selection of blank sky observations is necessary to estimate the background due to all these sources correctly.…”
Section: Introductionmentioning
confidence: 99%
“…cosmic X-ray background (CXB), cosmic ray particles, geomagnetically trapped particles and albedo (secondary) emission produced in the Earth's atmosphere. [20][21][22] The scintillator based gamma-ray detector is also sensitive to the energetic protons and electrons present in the Van Allen radiation belts (SAA and polar regions). 23 The advantage of our detector design, which employs MPPC sensors is that it operates at relatively low bias voltage and it can also safely measure inside the extreme radiation conditions of the SAA and polar regions.…”
Section: Low Earth Orbit Background Monitoringmentioning
confidence: 99%