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Radiation Assessment Detector (RAD). D.M. Hassler, A. Posner, M. Bullock, S. Rafkin, D. Grinspoon (Southwest Research Institute) R.F. Wimmer-Schweingruber, R. Beaujean, S. Burmeister, R. Muller-Mellin, S. Bottcher (Univ. of Kiel) G. Reitz (DLR/Koln) F. Cucinotta, T. Cleghorn (NASA/JSC).
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Radiation Assessment Detector (RAD) D.M. Hassler, A. Posner, M. Bullock, S. Rafkin, D. Grinspoon (Southwest Research Institute) R.F. Wimmer-Schweingruber, R. Beaujean, S. Burmeister, R. Muller-Mellin, S. Bottcher (Univ. of Kiel) G. Reitz (DLR/Koln) F. Cucinotta, T. Cleghorn (NASA/JSC)
Validating Radiation Transport Codes and Models Penetration Depths for Various Energy Particles. Secondary Particle Production from Galactic Cosmic Rays
Atmospheric Shielding at Mars: Strong dependence on atmospheric column mass
RAD Time Resolution Required to Characterize a Solar Particle Event (SPE)
Astronaut Safety: Determining the Radiation Dose Rate for Humans on Mars GCRs produce near-constant background flux of radiation, modulated by solar cycle. Composed mostly H+ and He2+, but heavy ions contribute disproportionately to the Dose Equivalent due to their high quality factor, Q. (Wilson et al. 1997)
Preparation for Human Exploration of Mars: Astronaut Safety Requires Monitoring Certain Particle Species
RAD Instrument Overview RAD proto-type (top) being tested at Brookhaven National Lab (bottom)
RAD Species Identification Approach:Distinguish Ion Species using dE/dx vs E method Ion kinetic energy deposited per unit length: Bethe-Bloch Equation: Ion Identification: substitute v2 with: Thus: