Radon Dose Determination and Radiological Risk in Some Mexican Caves with CR-39 Detectors

Authors

  • A. Chavarria Sciences Faculty, National Autonomous University of Mexico https://orcid.org/0000-0002-0159-3712
  • J. I. Golzarri Instituto de Física, Universidad Nacional Autónoma de México, Cd. de México 04520 México; Condensed Matter Department, Physics Institute, National Autonomous University of Mexico
  • G. Espinosa Instituto de Física, Universidad Nacional Autónoma de México, Cd. de México 04520 México; Condensed Matter Department, Physics Institute, National Autonomous University of Mexico

DOI:

https://doi.org/10.15415/jnp.2021.82022

Keywords:

Caves, Radon, Doses, CR-39, Radiological risk

Abstract

Radon (222Rn) is a radioactive gas, from the 238U decay chain, that contributes in large part of the natural radiation dose to which humans are exposed. Radon is the second cause of lung cancer after tobacco. The US-EPA considers a concentration of 148 Bq/m3 for homes and 400 Bq/m3 for workplaces as the reference level. Caves are closed spaces where 222Rn, which emanates from the surrounding minerals and rocks, can accumulate and reaches large concentrations that can represent a health risk for the guides, speleologists and visitors who spend time in these spaces. This work uses the previously recorded radon concentrations in 8 caves in Mexico and calculates the average dose range and the average annual dose for each of them with the “Wise” public domain program (http://www.wise-uranium.org/rdcrn.html) to determine the level of radiological risk with 2,000 1,000 and 500 working hours per year. Karmidas cave had the highest average 222Rn concentration with 27,633.3 Bq/m3 and for 2,000 working hours per year an average annual dose rate of 347.1 mSv/y. Los Riscos cave had the lowest average concentration with 384.7 Bq/m3 and for 2,000 working hours per year an average annual dose rate of 4.832 mSv/y. These results show that all the caves studied present values,
with 2,000 working hours per year, that exceed 3 mSv/y for workplaces and must be considered by the people who work in these places. A casual tourist visiting the caves does not present any radiological risk, while guides and speleologists should consider it.

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References

S. Alberigi, B.R.S. Pecequilo, H.A.S. Lobo and M.P. Campos, Radiation Protection Dosimetry 145, 252 (2011). https://doi.org/10.1093/rpd/ncr054

J. Borau, A. Gonzales, G. Espinosa and J.I. Golzarri, Nuclear Tracks and Radiation Measurements 22, 287 (1993). https://doi.org/10.1016/0969-8078(93)90069-G

A.A Cigna, International Journal of Speleology 34, 1 (2005). https://doi.org/10.5038/1827-806X.34.1.1

J.T. Duffy, J.S. Madden, G.M. Mackin, A.T. McGarry and P.A. Colgan, Environment International 22, 415 (1996). https://doi.org/10.1016/S0160-4120(96)00140-7

G. Espinosa, Radon gas in caves (Original: Gas Radón en Cuevas). (Physics Institute, National Autonomous University of Mexico, Mexico, 2016).

G. Espinosa, J.I. Golzarri, R.E. Gammage, L. Sajo-Bohus, J. Viccon-Pale and M. Signoret-Poillon, Radiation Measurements 43, S364 (2008). https://doi.org/10.1016/j.radmeas.2008.04.033

G. Espinosa, J.I.Golzarri, E. Vega-Orihuela and J.B. Morales-Malacara, Journal of Radioanalytical and Nuclear Chemistry 296, 43 (2013). https://doi.org/10.1007/s10967-012-1975-8

A. Hoffman, J.G. Palacios-Vargas and J.B. Morales-Malacara, Manual of Biospeleology (Original: Manual de Bioespeliología). (National Autonomous University of Mexico, Mexico, 1986).

C.N. Grant, G.C. Lalor and M. Balcazar, Applied Radiation and Isotopes 71, 96 (2012). https://doi.org/10.1016/j.apradiso.2012.07.007

C. Lazcano, Gaceta UNAM. No. 41, 21 (1983).

P. Jovanovič, Environment International 22, 429 (1996). https://doi.org/10.1016/S0160-4120(96)00142-0

W.W. Nazaroff, Reviews of Geophysics 30, 137 (1992). https://doi.org/10.1029/92RG00055

P. Szervin, Environment International 22, 389 (1996). https://doi.org/10.1016/S0160-4120(96)00137-7

F.A.G. Paz, Y.A.G. Romero and R. Zalakeviciute, Journal of Radiation Research 60, 759 (2019). https://doi.org/10.1093/jrr/rrz064

UNSCEAR, Sources and effects of ionizing radiation. (United Nations, New York, 2000).

US-EPA Environments Division (6609 J). US-EPA, Washington, DC (2004).

WISE. http://www.wise-uranium.org/rdcrnh.html. (2009). Accessed 10 Aug 2020.

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Published

2021-02-10

How to Cite

(1)
Chavarria, A.; Golzarri, J. I. .; Espinosa, G. Radon Dose Determination and Radiological Risk in Some Mexican Caves With CR-39 Detectors. J. Nucl. Phy. Mat. Sci. Rad. A. 2021, 8, 169-175.

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