Cosmic-ray muon flux at Canfranc Underground Laboratory
/ Authors
W. Trzaska, M. Slupecki, I. Bandac, A. Bayo, A. Bettini, L. Bezrukov, T. Enqvist, A. Fazliakhmetov, A. Ianni, L. Inzhechik
and 7 more authors
J. Joutsenvaara, P. Kuusiniemi, K. Loo, B. Lubsandorzhiev, A. Nozik, C. Peña Garay, M. Poliakova
/ Abstract
Residual flux and angular distribution of high-energy cosmic muons have been measured in two underground locations at the Canfranc Underground Laboratory (LSC) using a dedicated Muon Monitor. The instrument consists of three layers of fast scintillation detector modules operating as 352 independent pixels. The monitor has a flux-defining area of 1m2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$1~\hbox {m}^{2}$$\end{document} and covers all azimuth angles, and zenith angles up to 80∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$80^{\circ }$$\end{document}. The measured integrated muon flux is (5.26±0.21)×10-3m-2s-1\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$(5.26 \pm 0.21) \times 10^{-3}~\hbox {m}^{-2}\hbox {s}^{-1}$$\end{document} in the Hall A of the LAB2400 and (4.29±0.17)×10-3m-2s-1\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$(4.29 \,\pm \, 0.17) \times 10^{-3}~\hbox {m}^{-2}\hbox {s}^{-1}$$\end{document} in LAB2500. The angular dependence is consistent with the known profile and rock density of the surrounding mountains. In particular, there is a clear maximum in the flux coming from the direction of the Rioseta valley.
Journal: The European Physical Journal C