Study of cosmic ray events with high muon multiplicity using the ALICE detector at the CERN Large Hadron Collider
ALICE Collaboration

TL;DR
This study analyzes atmospheric muon multiplicity from cosmic rays using ALICE at CERN, revealing high multiplicity events originate from ultra-high-energy cosmic rays and are best explained by a heavy primary cosmic ray composition.
Contribution
It provides the first detailed comparison of high muon multiplicity events with Monte Carlo simulations at the LHC, highlighting the importance of heavy primary cosmic rays.
Findings
High multiplicity muon events are linked to cosmic rays above 10^16 eV.
Simulations with heavy primary composition match observed high multiplicity event frequency.
Results constrain models of cosmic ray composition and hadronic interactions at ultra-high energies.
Abstract
ALICE is one of four large experiments at the CERN Large Hadron Collider near Geneva, specially designed to study particle production in ultra-relativistic heavy-ion collisions. Located 52 meters underground with 28 meters of overburden rock, it has also been used to detect muons produced by cosmic ray interactions in the upper atmosphere. In this paper, we present the multiplicity distribution of these atmospheric muons and its comparison with Monte Carlo simulations. This analysis exploits the large size and excellent tracking capability of the ALICE Time Projection Chamber. A special emphasis is given to the study of high multiplicity events containing more than 100 reconstructed muons and corresponding to a muon areal density m. Similar events have been studied in previous underground experiments such as ALEPH and DELPHI at LEP. While these experiments were…
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