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The recovery of cosmic‐ray emulsions from rocket and space probes

OCT 01, 1960

DOI: 10.1063/1.3062764

Herman Yagoda

The atmosphere presents a barrier between the cosmic‐ray physicist and the object of his study. In its absorptive capacity for cosmic radiation the tenuous mantel of air adds up at sea level to 1040 grams per cm2 equivalent to a shielding of about one meter of lead. To identify and to measure the relative proportions of the diverse components present in the primary cosmic‐ray beam arriving from space the instrumentation must be sent above the atmosphere. Unlike the astronomer who can wait patiently for a night of “good seeing” in order to resolve planetary detail no such natural opportunity awaits those who are curious about the charge spectrum of the heavy primary component. Owing to the large collision cross sections of these massive charged particles an appreciable alteration of the beam takes place even at elevations readily accessible to high‐altitude balloons, particularly for particles which arrive at large zenith angles.

References

  1. 1. For technical details of mountings see H. Yagoda, “Cassettes d’emulsions pour l’étude des rayons cosmiques dans les fusées a haute altitude”, Proc. 1st Inter. Cong. Corpuscular Photography, Centre National de la Recherche Scientific, France, 1958.

  2. 2. H.Yagoda, H. G.de Carvalho, and N.Kaplan, “Stars and heavy primaries recorded during a V‐2 rocket flight”, Phys. Rev. 78, 765 (1950).https://doi.org/PHRVAO

  3. 3. H.Yagoda, “Observations on stars and heavy primaries recorded in emulsions flown in Viking Rocket No. 9”. Canadian J. Phys. 34, 122 (1956).https://doi.org/CJPHAD

  4. 4. Milton Rosen, The Viking Rocket Story (Harper Bros., New York, 1955).

  5. 5. H. L.Bradt and B.Peters, “Abundance of light nuclei in the primary cosmic radiation”, Phys. Rev. 80, 943 (1950).https://doi.org/PHRVAO

  6. 6. H. Yagoda, “Observations on heavy primary cosmic ray nuclei above the atmosphere”, Geophysical Research Paper No. 60, July 1958, AFCRC, Bedford, Mass.

  7. 7. C. J.Waddington, Phil. Mag. 2, 1059 (1957).https://doi.org/PHMAA4

  8. 8. S. H.Yagoda, Bull. Amer. Phys. Soc. ser. II, 1, 64 (1956);
    S. H.Yagoda, Nuovo cimento 10, 559 (1957); https://doi.org/NUCIAD
    Proc. 6th Rochester Conf. High Energy Nuclear Physics, IX‐30 (Interscience Publishers, Inc., New York, April 1956).

  9. 9. S. C.Freden and R. S.White, “Protons in the Earth’s magnetic field”, Phys. Rev. Letters 3, 9 (1959).https://doi.org/PRLTAO

  10. 10. H.Yagoda, “Star production by trapped protons in the inner radiation belt”, Bull. Amer. Phys. Soc., ser. II, 5, 260 (1960);
    H.Yagoda, Phys. Rev. Letters 5, 17 (1960).https://doi.org/PRLTAO

  11. 11. A. H.Armstrong, F. B.Harrison, and L.Rosen, Bull. Amer. Phys. Soc., ser. II, 4, 360 (1959).

More about the Authors

Herman Yagoda. Ionospheric Physics Laboratory, Geophyiscs Research Directorate Bedford, Massachusetts.

This Content Appeared In
pt-cover_1960_10.jpeg

Volume 13, Number 10

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