2019
DOI: 10.1142/s0217751x19500696
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Longitudinal profiles of Extensive Air Showers with inclusion of charm and bottom particles

Abstract: Charm and bottom particles are rare in Extensive Air Showers but the effect of its presence can be radical in the development of the Extensive Air Showers (EAS). If such particles arise with a large fraction of the primary energy, they can reach large atmospheric depths, depositing its energy in deeper layers of the atmosphere. As a consequence, the EAS observables (X max , RM S and N max ) will be modified, as well as the shape of the longitudinal profile of the energy deposited in the atmosphere. In this pap… Show more

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Cited by 3 publications
(6 citation statements)
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“…For X max we have a shift to deeper layers of the atmosphere in relation to the STD CORSIKA, with the relative difference being about 12%. On the other hand, for the RMS, we have a relative difference of about 40% [4]. For the charm production with F E ≥ 0.8 we find the values of 898.8 g/cm 2 and 87.8 g/cm 2 , respectively, for X max and RMS.…”
Section: Pos(icrc2019)361mentioning
confidence: 71%
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“…For X max we have a shift to deeper layers of the atmosphere in relation to the STD CORSIKA, with the relative difference being about 12%. On the other hand, for the RMS, we have a relative difference of about 40% [4]. For the charm production with F E ≥ 0.8 we find the values of 898.8 g/cm 2 and 87.8 g/cm 2 , respectively, for X max and RMS.…”
Section: Pos(icrc2019)361mentioning
confidence: 71%
“…Since charmed particles are able to reach larger depths in the atmosphere, interacting rather than decaying, they delay the EAS development. The resulting longitudinal profiles are wider, have more particles at ground level and larger depths [3,4]. In addition, EASs that transport energy deeper in the atmosphere result in a larger number of electromagnetic component inside the Water-Cherenkov tanks.…”
Section: Discussionmentioning
confidence: 99%
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“…In this contribution we will estimate the prompt muon and neutrino fluxes considering a modified version of the CORSIKA (Cosmic Ray Simulations for Kaskade) Monte Carlo [6], hereafter denoted HQ CORSIKA, which includes the charm and bottom production at the cosmic ray first interaction (For more details see Refs. [7,8]. In order to estimate the impact of the heavy particles in the EAS development, we will compare our predictions with those derived using the standard version of the CORSIKA (STD CORSIKA).…”
Section: Introductionmentioning
confidence: 99%