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.
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Authors
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M.H. Israel
Washington U., Washington U., St. Louis
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B.F. Rauch
WU
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K. Lodders
WU
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W.R. Binns
Washington University, St. Louis, WU
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E.R. Christian
NASA/GSFC
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G.A. de Nolfo
NASA/GSFC, GSFC
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S. Geier
Calif. Inst. of Technology
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J.T. Link
GSFC
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R.A. Mewaldt
Caltech
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L.M. Scott
WU
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R.E. Streitmatter
GSFC
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E.C. Stone
Caltech
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C.J. Waddington
U. of Minnesota
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M.E. Wiedenbeck
Jet Propulsion Lab