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Identification of gamma ultra high energy cosmic rays by simulating extensive air showers

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dc.contributor.author Geranios, A en
dc.contributor.author Fokitis, E en
dc.contributor.author Maltezos, S en
dc.contributor.author Mastichiadis, A en
dc.contributor.author Malandraki, OE en
dc.contributor.author Antoniadou, I en
dc.date.accessioned 2014-03-01T02:50:24Z
dc.date.available 2014-03-01T02:50:24Z
dc.date.issued 2006 en
dc.identifier.issn 0094243X en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/35110
dc.title Identification of gamma ultra high energy cosmic rays by simulating extensive air showers en
heal.type conferenceItem en
heal.identifier.primary 10.1063/1.2348033 en
heal.identifier.secondary http://dx.doi.org/10.1063/1.2348033 en
heal.publicationDate 2006 en
heal.abstract Among the most interesting tasks for the identification of Ultra High Energy Cosmic Rays (origin, mechanisms of acceleration, top down model, direction, and maximum energy) is their isotopic composition. For example, if they are protons, heavier nuclei, gammas or even exotic. Air Shower Extended Simulation code (AIRES) is used to simulate the Extended Atmospheric Showers. This code gives, among others, the maximum number of secondary particles within the atmosphere along the longitudinal direction of the showers. From the distribution of the depths of maximum number of shower particles and their content in muons, we can distinguish between proton and gamma primary cosmic rays, both of energy of 100 EeV. The results show a maximum at lower atmospheric depths for protons and at higher for gammas, respectively. Due to the bremsstrahlung and pair production effects, the muon content of gamma showers is much poorer than of protons. Both facts enable the distinction between proton and gamma cosmic rays. For the simulation of the atmospheric EAS due to the passage of an Ultra High Energy Cosmic Ray, the Linsley standard atmospheric model is used. © 2006 American Institute of Physics. en
heal.journalName AIP Conference Proceedings en
dc.identifier.doi 10.1063/1.2348033 en
dc.identifier.volume 848 en
dc.identifier.spage 580 en
dc.identifier.epage 586 en


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