AMPTE-IRM

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AMPTE-IRM
NamesAMPTE-Ion Release Module
Mission type Magnetosphere research
Operator NASA / Germany
COSPAR ID 1984-088B OOjs UI icon edit-ltr-progressive.svg
SATCAT no. 15200
Mission duration2 years (achieved)
Spacecraft properties
SpacecraftAMPTE-IRM
Spacecraft typeActive Magnetospheric Particle Tracer Explorers (AMPTE)
Bus AMPTE-Ion Release Module
Manufacturer Max Planck Institute for Extraterrestrial Physics
Launch mass705 kg (1,554 lb)
Power60 watts
Start of mission
Launch date16 August 1984, 14:48 UTC [1]
Rocket Delta 3924 (Delta 175)
Launch site Cape Canaveral, LC-17A
Contractor Douglas Aircraft Company
Entered service16 August 1984
End of mission
Last contact14 August 1986
Orbital parameters
Reference system Geocentric orbit [2]
Regime Highly elliptical orbit
Perigee altitude 1.09 RE
Apogee altitude 18.83 RE
Inclination 28.60°
Period 44.30 hours
Instruments
3-D Plasma Analyzer
Ion Release Experiment
Mass Separation Ion Spectrometer (MSIS)
Plasma Wave Spectrometer
Suprathermal Energy Ionic Charge Analyzer
Triaxial Fluxgate Magnetometer
Explorer program
←  AMPTE-CCE (Explorer 65)
AMPTE-UKS  →
 

AMPTE-IRM, also called as AMPTE-Ion Release Module, was a Germany satellite designed and tasked to study the magnetosphere of Earth, being launched as part of the Explorer program. The AMPTE (Active Magnetospheric Particle Tracer Explorers) mission was designed to study the access of solar wind ions to the magnetosphere, the convective-diffusive transport and energization of magnetospheric particles, and the interactions of plasmas in space. [3]

Contents

Mission

The AMPTE-IRM is one of the three components of the international space mission AMPTE, which also included AMPTE-CCE (Charge Composition Explorer), designed by NASA, and AMPTE-UKS (United Kingsom Subsatellite), provided by the United Kingdom. [3]

Spacecraft

The program consisted of three spacecraft: the AMPTE-CCE, which measured in the magnetosphere the ions released by the AMPTE-IRM; and the AMPTE-UKS, which used thrusters to keep station near the AMPTE-IRM to provide two-point local measurements. The AMPTE-IRM provided multiple ion releases in the solar wind, the magnetosheath, and the magnetotail, with in situ diagnostics of each. The AMPTE-IRM spacecraft was spin-stabilized at 15 rpm. Its spin axis was initially in the ecliptic plane, but later it was adjusted with magnetic torqueing to be at right angles to the ecliptic. The power system was a 60 watts solar array with redundant batteries. There was a redundant S-band telemetry and telecommand system. Telemetry rates could be chosen between 1 and 8 kbps. For injection into the final orbit, the AMPTE-IRM carried its own kick stage. In addition to the ion releases, the instruments on board the spacecraft monitored the ambient, magnetosphere, but with the data acquisition confined to the passes that could be tracked in real time from Germany. [3]

Launch

AMPTE-IRM was launched with the two other satellites of the AMPTE program on 16 August 1984, at 16:48 UTC, from a Cape Canaveral launch pad by a Delta 3924 launch vehicle. [1] [2]

Experiments

3-D Plasma Analyzer (30-channel, Electrons: 15 eV-30 keV; Ions: 20 eV/q-40 keV/q)

The main instrument consisted of two symmetrical quadrispherical electrostatic analyzers to measure the three-dimensional distributions of electrons and ions, respectively, over 4-pi-sr during every satellite spin period (4 seconds). The energy range covered was 15 eV/Q to 30 keV/Q in 30 channels. The angular resolution was 22.5°. Moments of the measured distributions were directly computed on board. An additional retarding-potential analyzer measured the flux of electrons between approximately 0 and 25 eV. [4]

Ion Release Experiment

The experiment consisted of eight lithium and eight barium canisters, which were injected from the AMPTE-IRM in pairs by ground command and ignited 10 minutes after separation from the spacecraft. Each of these was either totally lithium or totally barium. A pair of Li/Ba canisters produced a total of 2.E25/7.E24 Li/Ba atoms, respectively, which were subsequently ionized by solar radiation. Li releases in the solar wind, which were carried out in August/September 1984, were to be followed by an artificial comet release of Ba ions in the dawnside magnetosheath and a number of Ba and Li releases in the geomagnetic tail. In situ diagnostics by AMPTE-IRM and AMPTE-UKS and optical observations of the clouds from the ground were followed by tracing of the ions in the inner magnetosphere by AMPTE-CCE. [5]

Mass Separation Ion Spectrometer (MSIS) (H through Ba: 0.5 eV/q-14 keV/q)

The instrument consisted of a retarding-potential analyzer entrance section and a toroidal electrostatic energy-per-charge analyzer, followed by a quadrispherical electrostatic analyzer with superimposed radial magnetic field for mass-per-charge analysis. The energy range covered was approximately 0 to 12 (or 24) keV/Q, with adequate mass resolution to separate the Li and Ba tracer ions. Up to eight different ion species could be analyzed simultaneously. [6]

Plasma Wave Spectrometer (64 channel, E- and B-field, E-: 0.0-5.6 MHz; B-: 30 Hz-1.5 MHz)

The instrument used a 42 m (138 ft) tip-to-tip antenna to measure electric fields from DC to 5 MHz and two boom-mounted search coil magnetometers to measure magnetic fields from 30 Hz to 1 MHz. The signals were analyzed by a very low frequency VLF/MF 16-channel spectrum analyzer, three VLF narrow-band swept-frequency receivers, a 60-channel high frequency HF stepped-frequency receiver, and an analog wide-band receiver. [7]

Suprathermal Energy Ionic Charge Analyzer (H through Fe: 5-270 keV/q; electrons: 35-207 keV)

The main instrument consisted of a curved plate electrostatic energy-per-charge analyzer followed by a 12 cm (4.7 in) time-of-flight telescope with a thin carbon foil at the front and a solid-state detector at the rear, which measured ion velocity and residual energy. The energy-per-charge range was 10 to 300 keV/Q. The mass resolution, delta M/M, ranged from 0.25 to 0.12. The instrument package also contained an electron sensor for the energy range 35 to 220 keV, provided by University of California, Berkeley. [8]

Triaxial Fluxgate Magnetometer

The instrument was a three-axis fluxgate magnetometer mounted on a 2 m (6 ft 7 in) boom. It had two switchable ranges (± 4 microtesla, and ± 60 microtesla) with resolutions of 0.12 and 1.8 nT, respectively and was read out at 32, 16, 8, or 4 vector samples per second, depending on the T/M rate. Signals from each sensor were also fed into four band pass filters with 5.5, 11, 22, and 44-Hz center frequencies and were read out up to two times per second. [9]

End of mission

The spacecraft became inoperational on 14 August 1986. [3] [2]

See also

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References

  1. 1 2 "Launch Log". Jonathan's Space Report. 21 July 2021. Retrieved 26 November 2021.
  2. 1 2 3 "Trajectory: AMPTE-IRM (1984-088B)". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  3. 1 2 3 4 "Display: AMPTE-IRM (1984-088B)". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  4. ↑ "Experiment: 3-D Plasma Analyzer". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  5. ↑ "Experiment: Ion Release Experiment". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  6. ↑ "Experiment: Mass Separation Ion Spectrometer (MSIS)". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  7. ↑ "Experiment: Plasma Wave Spectrometer". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  8. ↑ "Experiment: Suprathermal Energy Ionic Charge Analyzer". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
  9. ↑ "Experiment: Triaxial Fluxgate Magnetometer". NASA. 28 October 2021. Retrieved 26 November 2021.PD-icon.svg This article incorporates text from this source, which is in the public domain .
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