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#12b.     The Outer Radiation Belt

  (Files in red–history)


10. Trapped Motion

    10H. Einstein, 1910

10a. Particle Drift

11. Explorers 1/3

  11a. Geiger Counter

12. Rad. Belts

    12H. Argus 1958

12a. Inner Belt

12. Outer Belt

13. Fast Particles

14. Synch. Orbit

15. Energy

16. The Sun

  16H. Schwabe, 1843

        The space probes Pioneer 3 and 4 detected a wide belt of trapped particles beyond the inner belt. The intensity contours drawn here (together with the trajectories of the probes through space) were derived from their observations and are banana-shaped, because they follow magnetic field lines to which the particles are attached. We now know that outer-belt ions and electrons probably come from the long "magnetic tail" of stretched field lines on the night side of the magnetosphere.

    The Two Radiation Belts
        Now and then a violent outburst, known as a magnetic storm, drives tail plasma earthward, into the near-Earth magnetosphere. Electric fields (voltage differences) are essential to this process, to help tail particles break into trapped orbits and to drive them to higher energies. When the outburst ends and the electric field dies away, the particles find themselves locked in trapped orbits of the ring current and the outer radiation belt. Lesser outbursts, known as magnetospheric substorms, occur quite frequently.

        Whereas the inner belt is marked by great stability, the ring current and outer belt constantly change. Sooner or later the particles are lost, e.g. by collision with the rarefied gas of the outermost atmosphere, and on the other hand, new ones are frequently injected from the tail. The electric fields which inject the new particles can also draw oxygen ions upwards from the ionosphere, and the ring current contains such ions, typically a few percent of the total, more during magnetic storms.

Questions from Users:
      ***     Effects of Radiation beyond the Van Allen Belts

Last updated 25 November 2001
Re-formatted 9-28-2004

Above is background material for archival reference only.

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