Abstract
A wide variety of solar system bodies are now known to radiate in the soft x-ray energy (<5 keV) regime. These include planets (Earth, Jupiter, Venus, Saturn, Mars): bodies having thick atmospheres, with or without intrinsic magnetic field; planetary satellites (Moon, Io, Europa, Ganymede): bodies with thin or no atmospheres; and comets and Io plasma torus: bodies having extended tenuous atmospheres. Several different mechanisms have been proposed to explain the generation of soft x-rays from these objects, whereas in the hard x-ray energy range (>10 keV) x-rays mainly result from the electron bremsstrahlung process. In this paper we present a brief review of the x-ray observations on each of the planetary bodies and discuss their characteristics and proposed source mechanisms.
Original language | English (US) |
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Pages (from-to) | 215-226 |
Number of pages | 12 |
Journal | European Space Agency, (Special Publication) ESA SP |
Issue number | 514 |
State | Published - Oct 1 2002 |
Event | Proceedings of the 36th ESLAB Symposium; Earth-Like Planets and Moons - Noordwijk, Netherlands Duration: Jun 3 2002 → Jun 8 2002 |
All Science Journal Classification (ASJC) codes
- Aerospace Engineering
- Space and Planetary Science