Evaluation of cosmogenic production of $^{39}Ar$ and $^{42}Ar$ for rare-event physics using underground argon
Chao Zhang, Dongming Mei

TL;DR
This study simulates cosmogenic isotope production in underground argon to determine safe handling durations for dark matter and neutrinoless double beta decay experiments, ensuring minimal background interference.
Contribution
It provides detailed simulated production rates of $^{39}Ar$ and $^{42}Ar$ in underground argon, establishing time limits for surface exposure to maintain experimental sensitivity.
Findings
Production rates of $^{39}Ar$ and $^{42}Ar$ are quantified through simulation.
Maximum surface exposure durations are set at 954 days for $^{39}Ar$ and 1702 days for $^{42}Ar$.
Results inform handling and storage protocols for underground argon in rare-event physics.
Abstract
Underground argon (UAr) with lower cosmogenic activities of and has been planned as a detector in detecting scintillation light and charge collection using time projection chambers for dark matter searches and as a veto detector in suppressing backgrounds for neutrinoless double beta decay (0) experiments. Long-lived radioactive isotopes, and , can also be produced on the surface when UAr is pumped out from a deep well. Understanding the production of long-lived isotopes in Ar is important for utilizing UAr for dark matter and 0 experiments in terms of its production, transportation, and storage. Ar exposure to cosmic rays at sea-level is simulated using Geant4 for a given cosmic ray muon, neutron, and proton energy spectrum. We report the simulated cosmogenic production rates of , , and other…
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