https://doi.org/10.1140/epjp/s13360-022-02407-1
Regular Article
Gamma-ray flux measurement and geotechnical studies at the selected site for the LABChico underground laboratory
1
Instituto de Ciencias Nucleares, Universidad Nacional Autónoma de México, Ciudad de México, México
2
Centro Atómico Bariloche, CNEA/CONICET/IB, Bariloche, Argentina
3
Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, 04510, Ciudad de México, México
4
Royal Holloway, University of London, Egham Hill, United Kingdom
5
Instituto de Física, Universidad Nacional Autónoma de México, 01000, Ciudad de México, México
6
Facultad de Ingeniería, Universidad Nacional Autónoma de México, Ciudad de México, México
7
Boulby Underground Laboratory, Boulby Mine, Saltburn-by-the-Sea, United Kingdom
8
Department of Physics and Astronomy, University of Sussex, Brighton, United Kingdom
9
Departamento de Física, FES-Cuautitlán, Universidad Nacional Autónoma de México, C.P. 54770, Estado de México, México
Received:
26
May
2021
Accepted:
10
January
2022
Published online:
8
February
2022
The -ray flux inside La Guadalupe mine, the selected site for the construction of the underground laboratory LABChico in Mexico, is reported for energies below 3 MeV. Data were recorded with a 0.669 kg thallium-activated sodium iodide (NaI) crystal detector deployed for 3.6 hr. The detector response was calculated via Monte Carlo simulations with GEANT4 and validated against point-like calibration sources, and the
-ray spectrum was extracted using an unfolding technique. The
-ray flux above 250 keV and below 3 MeV is 0.1768
/cm
/s. The two most intense
-rays in the natural radioactive background,
K and
Tl, were identified. The flux measured for these isotopes is 0.0363 ± 0.0020
/cm
/s and 0.0016 ± 0.0005
/cm
/s, respectively. A
-ray spectrometry analysis of rock samples showed 674.0 ± 2.0 Bq/kg, 24.0 ± 0.1 Bq/kg, and 17.7 ± 0.2 Bq/kg, of
K,
Th, and
U, respectively. These results are compared with deep underground facilities such as SURF, SNOLAB, Boulby, Modane, and Gran Sasso, with differences observed mainly due to the rock composition. Geotechnical studies of the mine and its rock composition are also reported.
The original online version of this article was revised to correct affiliations 3 and 5.
A correction to this article is available online at https://doi.org/10.1140/epjp/s13360-022-02482-4.
Copyright comment corrected publication 2022
© The Author(s), under exclusive licence to Società Italiana di Fisica and Springer-Verlag GmbH Germany, part of Springer Nature 2022. corrected publication 2022