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OSO-3


photo of OSO

The Third Orbiting Solar Observatory (OSO-3), was launched on 8 March 1967, into a nearly circular orbit of mean altitude 550 km, inclined at 33 degrees with respect to the equatorial plane. The satellite had two principle components, a continuously spinning wheel in which the hard X-ray experiment is mounted with a radial view, and a sail component which was served to acquire the sun during the orbit day. The attitude control system maintained the scan plane orientation to within a few degrees of the sun. The spin-period of the satellite of roughly 1.7 s allowed about 1 cm2/s exposure per revolution to sources on the scan plane. Celestial sources near the ecliptic plane such as Sco X-1 transited the instrument scan plane twice a year. Only real-time data were received from the satellite after the last tape recorder failure on 27 June 1968. The last data transmission occurred 10 November 1969. OSO-3 descended into the atmosphere on 4 April 1982.

Mission Characteristics

Lifetime
Mar 1967–10 Nov 1969

Payload

USCD X-ray Telescope

Energy Range
7.7–210 keV
Effective Area
10 cm2
Field of View
23°
Energy Resolution
45% at 30 keV (6 channel resolution)
The UCSD X-ray telescope consisted of a single thin NaI(Tl) scintillation crystal plus phototube assembly enclosed in a howitzer-shaped CsI(Tl) anti-coincidence shield. It scanned the entire sky over the course of the mission.

MIT Gamma Ray Instrument

Energy Range
> 50 MeV
The MIT Gamma Ray Instrument operated continuously for about 16 months, at which time the last spacecraft tape recorded failed. The detector was a counter telescope. The multi-layer scintillation detector consisted of layers of CsI and plastic. The directional Cerenkov counter was a 3 × 3 in cylinder of lucite. The energy detector contained several layers of NaI, sandwiched by layers of tungsten. The entire detector was enclosed by plastic scintillator detectors.

Science Highlights

  • The instrument flown on OSO-3 obtained extensive observations of solar flares, the diffuse component of cosmic X-rays, and the observation of a single flare episode from Sco X-1.
  • The gamma-ray instrument registered 621 events attributed to cosmic gamma rays above 50 MeV. A complete sky survey showed that the celestial distribution of gamma rays is highly anisotropic, being concentrated along the galactic equator. In addition, an extended region around the galactic center showed a higher measured intensity.

Publications