EXPERIMENTAL AND NUMERICAL-SIMULATION OF MARTIAN NEUTRON DISTRIBUTIONS

Citation
Dm. Drake et al., EXPERIMENTAL AND NUMERICAL-SIMULATION OF MARTIAN NEUTRON DISTRIBUTIONS, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 84(3), 1994, pp. 337-356
Citations number
46
Categorie Soggetti
Physics, Nuclear","Nuclear Sciences & Tecnology","Instument & Instrumentation
ISSN journal
0168583X
Volume
84
Issue
3
Year of publication
1994
Pages
337 - 356
Database
ISI
SICI code
0168-583X(1994)84:3<337:EANOMN>2.0.ZU;2-8
Abstract
Measurements of the gamma-ray and neutron distributions produced by co smic-ray bombardment of planetary surfaces can provide important infor mation about water content and near-surface elemental compositions. Ac curate interpretation of such measurements depends heavily on comparis ons with radiation-transport calculations, which involve not only the soil composition but also assumptions about (1) particle types and ene rgy distributions of cosmic rays, (2) interaction mechanisms for high- energy protons and neutrons, (3) neutron transport at low energies, an d (4) production of prompt gamma rays and radionuclides in proton- and neutron-induced reactions. The present experiment simulates the plane tary situation by directing a beam of 800 MeV protons onto a large con tainer of Martian-like sand. Measurements were made of (1) the spatial distributions for protons and neutrons inside the container via activ ation foils and (2) the energy spectrum for neutron leakage out of the container via time of flight. Several configurations of the target we re used to represent different Martian surfaces. The measured neutron- energy spectra are in good agreement with calculations made using a co mputer code that couples medium-energy neutron production to low-energ y neutron transport, and the measured spatial distributions match thos e predicted using calculated fluxes and known cross sections for radio nuclide production. The analyses include discussions of soil water con tent, finite-size effects, and the implications for data from possible planetary missions.