Hydrogen and helium isotope inner radiation belts in the Earth's magnetosphere

G. I. Pugacheva (1) , W. N. Spjeldvik (2) , A. A. Gusev (1) , I. M. Martin (1) , N. M. Sobolevsky (3)

1 UNICAMP - Universidade Estadual de Campinas = University of Campinas
2 Department of Physics
3 Institute of Nuclear Research of Russian Academy of Science

Radial transport theory for inner radiation zone MeV ions has been extended by combining radial diffusive transport and losses due to Coulomb friction with local generation of D, T and ³He ions from nuclear reactions taking place on the inner edge of the inner radiation zone. Based on interactions between high energy trapped protons and upper atmospheric constituents we have included a nuclear reaction yield D, T and ³He flux source that was numerically derived from a nuclear reaction model code originally developed at the Institute of Nuclear Researches in Moscow, Russia. Magnetospheric transport computations have been made covering the L-shell range L=1.0?1.6. The resulting MeV energy D, T and ³He ion flux distributions show a strong influence of the local nuclear source mechanism on the inner zone energetic D, T and ³He ion content.

Domaines: Océan, Atmosphère; Sciences de la Terre

G. I. Pugacheva, W. N. Spjeldvik, A. A. Gusev, I. M. Martin, N. M. Sobolevsky. Hydrogen and helium isotope inner radiation belts in the Earth's magnetosphere. Annales Geophysicae, 1998, 16 (8), pp.931-939. ⟨hal-00316425⟩