The Time-of-Flight Energy, Angle, Mass Spectrograph (Teams) Experiment for Fast

AbstractThe Time-of-flight Energy Angle Mass Spectrograph (TEAMS) is being flown on the FAST Small Explorer mission to measure the 3-dimensional distribution function of the major ion species present in the lower magnetosphere. The instrument is similar to time-of-flight plasma analyzer systems that have been designed and planned for flight as CODIF (COmposition and DIstribution Function analyzer) on the four European Space Agency Cluster-II spacecraft and, as ESIC (Equator-S Ion Composition instrument) on Equator-S. This instrument allows the 3-dimensional distribution functions of individual ion species to be determined within $$\frac{1}{2}$$ spin period (2.5 s). Two-dimensional distributions are measured in 80 ms. These capabilities are crucial for the study of selective energization processes in the auroral regions of the magnetosphere. The design, operational characteristics, and test and calibration results for this instrument are presented. The sensor consists of a toroidal top-hat electrostatic analyzer with instantaneous acceptance of ions over 360° in polar angle. After post-acceleration of the incoming ions by up to 25 kV, a time-of-flight mass spectrograph discriminates the individual species. It has been demonstrated through calibration that the instrument can easily separate H+, He2+, He+, O+ and, for energies after post-acceleration of > 20 keV, even O2+ molecules. On-board mass discrimination and the internal accumulation of several distinct data quantities combined with the spacecraft's flexible telemetry formatting allow for instrument data rates from 7.8 kb s−1 to 315 kb s−1 to be telemetered to ground through the FAST centralized Instrument Data Processor.

[1]  G. Gloeckler,et al.  New high-resolution electrostatic ion mass analyzer using time of flight , 1990 .

[2]  E. Shelley,et al.  SATELLITE OBSERVATIONS OF ENERGETIC HEAVY IONS DURING A GEOMAGNETIC STORM. , 1972 .

[3]  R. Elphic,et al.  Species dependent energies in upward directed ion beams over auroral arcs as observed with FAST TEAMS , 1998 .

[4]  S. Krimigis,et al.  The Medium-Energy Particle Analyzer (MEPA) on the AMPTE CCE Spacecraft , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[5]  H. Rosenbauer,et al.  Discovery of He2+ and O2+ ions of terrestrial origin in the outer magnetosphere , 1977 .

[6]  J. Nordholt,et al.  New approach to 3-D, high sensitivity, high mass resolution space plasma composition measurements , 1990 .

[7]  G. Gloeckler,et al.  The Charge-Energy-Mass Spectrometer for 0.3-300 keV/e Ions on the AMPTE CCE , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[8]  D. Curtis,et al.  The Plasma Instrument for AMPTE IRM , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[9]  Y. Jiang,et al.  The 3-D plasma distribution function analyzers with time-of-flight mass discrimination for Cluster, FAST, and Equator-S , 2013 .

[10]  E. Shelley,et al.  Satellite observations of an ionospheric acceleration mechanism , 1976 .

[11]  B. Klecker,et al.  The Time-of-Flight Spectrometer SULEICA for Ions of the Energy Range 5-270 keV/Charge on AMPTE IRM , 1985, IEEE Transactions on Geoscience and Remote Sensing.

[12]  E. Möbius,et al.  High mass resolution isochronous time-of-flight spectrograph for three-dimensional space plasma measurements , 1990 .

[13]  Fritz Gliem,et al.  CELIAS: Charge, element and isotope analysis system for SOHO , 1988 .

[14]  B. A. Whalen,et al.  The Toroidal Imaging Mass-Angle Spectrograph (TIMAS) for the polar mission , 1995 .

[15]  David T. Young,et al.  2π-Radian field-of-view toroidal electrostatic analyzer , 1988 .

[16]  D. Klumpar Transversely accelerated ions - An ionospheric source of hot magnetospheric ions , 1979 .

[17]  G. Paschmann,et al.  An instrument for rapidly measuring plasma distribution functions with high resolution , 1982 .

[18]  J. P. McFadden,et al.  The Electron and ion Plasma Experiment for Fast , 2001 .

[19]  E. Shelley,et al.  Observation of an ionospheric acceleration mechanism producing energetic (keV) ions primarily normal to the geomagnetic field direction , 1977 .