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Mission description

The magnetically aligned spacecraft GRS-A, launched into a near-polar orbit on 08 Nov 1969, was a product of a joint effort by NASA-GSFC and the German Bundesministerium für Wissenschaftliche Forschung (BMWF) and had as its primary purpose the acquisition of terrestrial radiation belt data.

The instrument complement included detectors to measure the directional and omnidirectional fluxes of protons and electrons. These instruments and the high quality of the resulting measurements made the AZUR mission particularly well suited for the study of the trapped radiation environment, despite the short duration of the mission. The energetic proton measurements, which were collected during the maximum of Solar Cycle 20, were the basis for the low altitude part of the NASA model AP-8 MAX (Sawyer and Vette, 1976).

The mission goals were the measurements of the following quantities:

  1. directional proton intensities in several energy intervals between 0.25 and 100 MeV;
  2. directional intensity of alpha particles in the energy range 6.5 - 19 MeV;
  3. omnidirectional proton intensities in two energy ranges: 20 - 45 MeV and 40 - 80 MeV;
  4. omnidirectional integral electron intensity above two tresholds: 1.5 and 4.0 MeV;
  5. directional integral intensity of charged particles parallel, antiparallel and perpendicular to magnetic field lines, above 40 keV for electrons and 0.7 MeV for protons;
  6. omnidirectional integral intensity of charged particles above two tresholds: 12 and 30 MeV for protons, 0.7 and 3.2 MeV for electrons;
  7. optical emission by N2+ (lambda = 3914 Å) and OI-N2 (lambda = 2972 Å);
  8. transverse hydromagnetic waves with amplitudes above 5 gamma.

The payload consisted of seven instruments. Descriptions of each instrument package can be found in Achtermann et al. (1970).

After about 24 h in orbit, a command system instability developed and persisted intermittently throughout the flight. The tape recorder failed on 08 Dec 1969. Prior to this failure, the German project office estimated that 85 - 90 % of the expected data had been obtained. All experiments were operating normally until the spacecraft telemetry system malfunctioned on 18 June 1970.

Detector description

The EI-88 experiment consisted of two identical proton-alpha particle telescopes, one oriented perpendicular and one oriented at 45 ° with respect to the local magnetic field vector. In the northern hemisphere, the 45 ° telescope pointed upwards. The telescopes were to detect protons and alpha particles in the Earth's trapping region.

The experiment measures the directional proton flux in the energy range 1.5 - 100 MeV. The aperture opening is constructed with a number of Al and Ta collimators and is continued through a plastic scintillator surrounding the detectors and absorbers. The scintillator is connected to a photomultiplier by means of a plexiglass light conductor. The detectors respond to particle beams through the aperture opening. The energy dependent reach of the incident particle determines the number of detectors and absorbers they penetrate. Through the implementation of seven detectors and a treatment of the detector signal logic the total measurement range is divided into six energy ranges for protons and one channel for alpha particles. The anticoincidence rates are referred to as channel 8.

The lower limit of the detector range is determined by the thickness of the Ni foil placed before the scintillator, the thickness of the first detector and the electronic treshold of the second detector. The Ni foil with thickness 1 µ (8.9 10-4 g cm-2) serves to shield the scintillator and the detectors from incoming light. The upper energy limit of the instrument is given by the absorption thickness of the combined detector cage up to the aft inner wall of the scintillator. In addition to its role as upper energy limit for particles coming in through the aperture, the scintillator also tags particles that penetrate from outside the aperture through the combined shielding. An anticoincidence switch between scintillator and detector prohibits these particles to be measured. In order to limit the impuls rate of the scintillator and, correspondingly, the dead time of the instrument, the electronics is constructed around the scintillator and the photomultiplier to provide additional shielding.

The electronic tresholds of the semiconductor detectors are chosen sufficiently high so that electrons penetrating the aperture without scattering do not produce a signal. This arrangement does not rule out electrons undergoing multiple scattering and pile-up effects. Therefore, the instruments are equipped with a sweeping magnet which ensures that the influence of electrons on the ion count rates is negligible (Achtermann et al., 1970).

The plastic scintillator surrounds an Al cage that contains the seven detectors and the three absorbers. The detector connectors are fed through holes in the scintillator and the closest Ta shield to the amplifiers, which are arranged around the detector cage. The detectors EI-88/1 and EI-88/2 are identical except for a small difference in aperture angle, and thus geometric factor. The integration time for both instruments is fixed at 10 s. Due to the slow spin rate of the satellite, this rather long integration time does not compromise the quality of the directional measurements.

Unfortunately, the data gathered after 5 March 1970 have been lost.

AZUR
Mission
NameAZUR (GRS-A, GRS-A1, German Research Satellite)
Orbit typeNear polar
Perigee: 384 km, Apogee: 3145 km, Inclination: 102.96 °
OperatorDeutsche Forschung- und Versuchanstalt für Luft- und Raumfahrt/NASA
Launch date/time08 Nov 1969 01:55:00 UTC
Instrument
InstrumentEI-88
Data coverage 
Data resolution10 s
PID. K. Hovestadt (Max-Planck Institut für Extra-Terrestrische Physik)
SourceMagnetic tapes from NSSDC
L-coverage  RE
Data set
VariableDescription
AltitudeData set
LatitudeData set
LongitudeData set
Calculated BCalculated at BISA with UNILIB
McIlwain's L parameterCalculated at BISA with UNILIB
Proton fluxesp+: 1.5 - 2.7 MeV
p+: 2.7 - 5.2 MeV
p+: 5.2 - 10.4 MeV
p+: 10.4 - 22 MeV
p+: 22 - 49 MeV
p+: 49 - 104 MeV
Alpha flux (6-19 MeV)Data set

Remarks:

References

Achtermann, E., B. Häusler, D. Hovestadt, and G. Paschmann, Die Experimente EI 88 und EI 93 zur Messung von energiereichen Elektronen, Protonen und Alphateilchen im Satelliten AZUR, Physikalische Eigenschaften und Testmessungen, BMBW-FB W 70-67, 1970.

Häusler, B., Untersuchungen des Verhaltens hochenergetischer Protonen und Elektronen in der inneren Magnetosphäre, MPI-PAE/Extraterr. 66, 1972.

Heynderickx, D., and M. Kruglanski, Flight Data Comparisons, TREND 3, Technical note 5, part 1: The AZUR data, ESTEC Contract No. 10725/94/NL/JG(SC), 1998.

Hovestadt, D., E. Achtermann, B. Ebel, B. Häusler, and G. Pachmann, New Observations of the proton population of the radiation belt between 1.5 and 104 MeV, Earth's Magnetospheric Processes, B. M. McCormac (ed.), D. Reidel Publishing Company, Dordrecht, Holland, 115 - 119, 1972.

Sawyer, D. M., and J. I. Vette, AP-8 Trapped Proton Environment for Solar Maximum and Solar Minimum, NSSDC/WDC-A-R&S 78-06, 1976.


The description is taken from Heynderickx and Kruglanski (1998).

Last update: Mon, 12 Mar 2018