Elemental Abundances in the Cosmic Rays 26$\le $Z$\le $34 -- Evidence For Cosmic-Ray Origin in OB Associations

ORAL

Abstract

The TIGER instrument flew on high-altitude balloons over Antarctica for 50 days. The observed elemental abundances with 26$\le $Z$\le $34, when corrected for fragmentation during propagation in the Galaxy and in the atmosphere, show cosmic-ray source abundances that differ from the standard Solar System (SS) abundances. Preferential acceleration of refractory elements does not fully explain these differences. They can be accounted for by a source mixture of $\sim $80{\%} SS and $\sim $20{\%} representative of the ejecta from massive stars, which mixture is then affected by elemental volatility in the acceleration process. This 80/20 mixture has also been shown to account for the isotopic composition of lighter cosmic rays and can be understood as the result of cosmic-ray acceleration in OB associations.

Authors

  • M.H. Israel

    Washington U., Washington U., St. Louis

  • B.F. Rauch

    WU

  • K. Lodders

    WU

  • W.R. Binns

    Washington University, St. Louis, WU

  • E.R. Christian

    NASA/GSFC

  • G.A. de Nolfo

    NASA/GSFC, GSFC

  • S. Geier

    Calif. Inst. of Technology

  • J.T. Link

    GSFC

  • R.A. Mewaldt

    Caltech

  • L.M. Scott

    WU

  • R.E. Streitmatter

    GSFC

  • E.C. Stone

    Caltech

  • C.J. Waddington

    U. of Minnesota

  • M.E. Wiedenbeck

    Jet Propulsion Lab