Semones, E.; Rutledge, R.; Flanders, J.
13th Workshop on Radiation Monitoring for the International Space Station - Final Program2008
13th Workshop on Radiation Monitoring for the International Space Station - Final Program2008
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Institute of Nuclear Physics, Polish Academy of Sciences, Cracow (Poland). Funding organisation: Institute of Nuclear Physics, Cracow (Poland); RadPro International, Wermelskirchen (Germany); 54 p; 2008; p. 15; 13. Workshop on Radiation Monitoring for the International Space Station; Cracow (Poland); 8-10 Sep 2008; Also available from http://www.ifj.edu.pl/conf/wrmiss/
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Saganti, P.; Cucinotta, F.A.; Cleghorn, T.F.; Flanders, J.; Riman, F.; Hu, X.; Zeitlin, C.J.; Pinsky, L.; Lee, K.T.; Anderson, V.; Atwell, W.; Turner, R.
12th Quadrennial Congress of the International Association for Radiation Research incorporating the 50th Annual Meeting of Radiation Research Society, RANZCR Radiation Oncology Annual Scientific Meeting and AINSE Radiation Science Conference2003
12th Quadrennial Congress of the International Association for Radiation Research incorporating the 50th Annual Meeting of Radiation Research Society, RANZCR Radiation Oncology Annual Scientific Meeting and AINSE Radiation Science Conference2003
AbstractAbstract
[en] Full text: For a given GCR (Galactic Cosmic Ray) environment at Mars, particle flux of protons, alpha particles, and heavy ions, are also needed on the surface of Mars for future human exploration missions. For the past twelve months, the MARIE (Martian Radiation Environment Experiment) instrument onboard the 2001 Mars Odyssey has been providing the radiation measurements from the Martian orbit. These measurements are well correlated with the HZETRN (High Z and Energy Transport) and QMSFRG (Quantum Multiple-Scattering theory of nuclear Fragmentation) model calculations. These model calculations during these specific GCR environment conditions are now extended and transported through the CO2 atmosphere onto the Martian surface. These calculated particle flux distributions are presented as a function of the Martian topography making use of the MOLA (Mars Orbiter Laser Altimeter) data from the MGS (Mars Global Surveyor). Also, particle flux calculations are presented with visualization in the human body from skin depth to the internal organs including the blood-forming organs
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International Association for Radiation Research (International Organisation without Location); Australian Institute of Nuclear Science and Engineering (AINSE), Lucas Heights, NSW (Australia); 414 p; 2003; p. 394; ICRR 2003: 12. Quadrennial Congress of the International Association for Radiation Research; Brisbane, QLD (Australia); 17-22 Aug 2003; Available in abstract form only, full text entered in this record
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Saganti, P.; Cucinotta, F.A.; Cleghorn, T.F.; Flanders, J.; Riman, F.; Hu, X.; Zeitlin, C.J.; Pinsky, L.; Lee, K.T.; Anderson, V.; Atwell, W.; Turner, R.
12th Quadrennial Congress of the International Association for Radiation Research incorporating the 50th Annual Meeting of Radiation Research Society, RANZCR Radiation Oncology Annual Scientific Meeting and AINSE Radiation Science Conference2003
12th Quadrennial Congress of the International Association for Radiation Research incorporating the 50th Annual Meeting of Radiation Research Society, RANZCR Radiation Oncology Annual Scientific Meeting and AINSE Radiation Science Conference2003
AbstractAbstract
[en] Full text: The Galactic Cosmic Ray spectra in Mars orbit were generated with the HZETRN (High Z and Energy Transport) and QMSFRG (Quantum Multiple-Scattering theory of nuclear Fragmentation) model calculations, and compared with the first twelve months of measured data from the MARIE (Martian Radiation Environment Experiment) instrument onboard the 2001 Mars Odyssey spacecraft that is currently in Martian orbit. The dose rates observed by the MARIE instrument are within 10% of the model calculations. Model calculations are compared with the MARIE measurements of dose, dose-equivalent values, along with particle flux distributions. Model calculation particle fluxes also includes GCR elemental composition of atomic number, Z = 1-28 and mass number, A = 1-58. Particle flux calculations specific for the current mapping period are presented
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International Association for Radiation Research (International Organisation without Location); Australian Institute of Nuclear Science and Engineering (AINSE), Lucas Heights, NSW (Australia); 414 p; 2003; p. 394; ICRR 2003: 12. Quadrennial Congress of the International Association for Radiation Research; Brisbane, QLD (Australia); 17-22 Aug 2003; Available in abstract form only, full text entered in this record
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