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  • Other Sources  (5)
  • NUCLEAR ENGINEERING  (3)
  • SPACE RADIATION  (2)
  • 1
    Publication Date: 2005-11-30
    Description: All mineral detectors exposed on Apollo 16 had high surface track densities probably produced by a solar flare that occurred during the mission. The heavy ions followed a power law spectrum with exponent approximately 3 down to approximately 200 KeV/nucleon. The abundance of low-energy particle tracks observed in this flare may explain the high track densities observed in lunar dust grains. Pristine heavy-particle tracks in feldspar give long tracks. Shallow pits similar to those expected from extremely heavy solar wind ions were observed in about the expected number. Initial results give a low apparent value of neutron albedo relative to theory.
    Keywords: SPACE RADIATION
    Type: NASA. Lyndon B. Johnson Space Center Apollo 16 Prelim. Sci. Rept.; 14 p
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  • 2
    Publication Date: 2006-01-11
    Description: The lunar surface cosmic ray experiment, consisting of sets of mica, glass, plastic, and metal foil detectors, was successfully deployed on the Apollo 17 mission. One set of detectors was exposed directly to sunlight and another set was placed in shade. Preliminary scanning of the mica detectors shows the expected registration of heavy solar wind ions in the sample exposed directly to the sun. The initial results indicate a depletion of very-heavy solar wind ions. The effect is probably not real but is caused by scanning inefficiencies. Despite the lack of any pronounced solar activity, energetic heavy particles with energies extending to 1 MeV/nucleon were observed. Equal track densities of approximately 6000 tracks/cm sq 0.5 microns in length were measured in mica samples exposed in both sunlight and shade.
    Keywords: SPACE RADIATION
    Type: NASA. Johnson Space Center Apollo 17 Prelim. Sci. Rept.; 9 p
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  • 3
    Publication Date: 2019-06-27
    Description: Horn and Von Oertzen (1967) have shown that tracks in mica are produced by an irradiation with 32-MeV O-16 ions. These tracks were attributed to K and Fe recoils produced by elastic scattering of the incident oxygen beam. In the present work an alternate explanation of their observations is provided. The measured characteristics of the tracks are shown to be compatible with theoretical predictions for production of tracks by inelastic (mostly compound nucleus) reactions with silicon and to be inconsistent with the previously proposed elastic scattering process. The possibility that the tracks are produced by contaminant ions in the beam cannot be ruled out.
    Keywords: NUCLEAR ENGINEERING
    Type: Radiation Effects; 19; 1973
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  • 4
    Publication Date: 2019-07-13
    Description: Heavy ion tracks in silicate minerals, using thermal annealing to identify origins
    Keywords: NUCLEAR ENGINEERING
    Type: INTERNATIONAL TOPICAL CONFERENCE ON NUCLEAR TRACK REGISTRATION IN INSULATING SOLIDS AND APPLICATIONS; May 01, 1969; CLERMONT-FERRAND, PUY-DE DOME; FRANCE|; VUE SCIENTIFIQUE ET
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  • 5
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    In:  Other Sources
    Publication Date: 2019-07-13
    Description: Heavy ion track registration in nonconductor minerals, discussing radiation damage and atomic species along trajectory
    Keywords: NUCLEAR ENGINEERING
    Type: INTERNATIONAL TOPICAL CONFERENCE ON NUCLEAR TRACK REGISTRATION IN INSULATING SOLIDS AND APPLICATIONS; May 01, 1969; CLERMONT-FERRAND, PUY-DE DOME; FRANCE|; VUE SCIENTIFIQUE ET
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