Cosmogenic Muon Background Characterization for the Colorado Underground Research Institute (CURIE)

TL;DR

This study characterizes cosmogenic muon backgrounds at the CURIE underground facility, measuring muon flux and validating simulation models, demonstrating the site's suitability for low-background physics experiments.

Contribution

First successful application of GEANT4 and PROPOSAL simulations for muon flux modeling at depths less than 1 km.w.e., with a new depth-intensity relationship for shallow underground sites.

Findings

Measured muon flux at two sites with uncertainties.

Good agreement between measurements and simulations.

Established the facility's potential for low-background experiments.

Abstract

We present the characterization of cosmogenic muon backgrounds for the Colorado Underground Research Institute (CURIE), located in the Edgar Experimental Mine (EEM) in Idaho Springs, Colorado. The CURIE facility at the EEM offers a versatile shallow underground environment, with accessible horizontal tunnel access and stable rock formations ideal for low-background physics experiments. We have measured the total underground muon flux in two locations, Site 0 and Site 1, yielding values of $\phi$ = 0.246 $\pm$ 0.020$_{sys.}$ $\pm$ 0.012$_{stat.}$ and 0.239 $\pm$ 0.025$_{sys.}$ $\pm$ 0.010$_{stat.}$ $\mu\text{/}m^{2}\text{/}s$, respectively. We have utilized GEANT4 and PROPOSAL Monte Carlo simulations with Daemonflux and MUTE to model the muon flux at both sites, as well as an additional future location. We find good agreement between measurement and simulations, demonstrating the first instance of this computational framework being successfully used for depths $<$ 1 km.w.e. The measured underground flux corresponds to a factor of 700 reduction compared to the sea level flux. Additionally, we present a new depth-intensity relationship to normalize the mountain overburden to an equivalent flat depth, enabling direct comparison with other underground facilities. We report an average equivalent vertical depth of 0.415 $\pm$ 0.027 km.w.e. Based on our measurements, this work highlights the facility's capability for hosting low-background experiments, addressing the demand for shallow underground research spaces.