Solar wind composition

Details Solar wind composition Solar wind composition

Jan 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995gsfc.rept.....o&link_type=abstract

Progress Report National Aeronautics and Space Administration. Goddard Space Flight Center, Greenbelt, MD.

Astronomy and Astrophysics

Astrophysics

Abundance, Astrophysics, Coronas, Energetic Particles, Fractionation, Galactic Cosmic Rays, Ionization, Mathematical Models, Photosphere, Solar Radiation, Solar Wind, Stellar Models, Charge Exchange, Interplanetary Medium, Ionization Potentials, Ions, Neutral Atoms, Spectroscopy, Topology

Scientific paper

Advances in instrumentation have resulted in the determination of the average abundances of He, C, N, O, Ne, Mg, Si, S, and Fe in the solar wind to approximately 10%. Comparisons with solar energetic particle (SEP) abundances and galactic cosmic ray abundances have revealed many similarities, especially when compared with solar photospheric abundances. It is now well established that fractionation in the corona results in an overabundance (with respect to the photosphere) of elements with first ionization potentials less than 10 eV. These observations have in turn led to the development of fractionation models that are reasonably successful in reproducing the first ionization (FIP) effect. Under some circumstances it has been possible to relate solar wind observations to particular source regions in the corona. The magnetic topologies of the source regions appear to have a strong influence on the fractionation of elements. Comparisons with spectroscopic data are particularly useful in classifying the different topologies. Ions produced from interstellar neutral atoms are also found in the solar wind. These ions are picked up by the solar wind after ionization by solar radiation or charge exchange and can be identified by their velocity in the solar wind. The pick-up ions provide most of the pressure in the interplanetary medium at large distances. Interstellar abundances can be derived from the observed fluxes of solar wind pick-up ions.

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