Characterization of the Antarctic soil of King George Island/25 May by gamma spectrometry

Authors

  • Marcos Tassano Laboratorio de Radioquímica, Centro de Investigaciones Nucleares, Facultad de Ciencias, Universidad de la República, Uruguay. https://orcid.org/0000-0001-6685-4656
  • Joaquín Irigoyen Unidad de Radioprotección, Centro de Investigaciones Nucleares, Facultad de Ciencias, Universidad de la República, Uruguay
  • Joan González Laboratorio de Radioquímica, Centro de Investigaciones Nucleares, Facultad de Ciencias, Universidad de la República, Uruguay. https://orcid.org/0000-0003-3313-3021
  • Mirel Cabrera Laboratorio de Radioquímica, Centro de Investigaciones Nucleares, Facultad de Ciencias, Universidad de la República, Uruguay. https://orcid.org/0000-0002-5225-1106

DOI:

https://doi.org/10.35954/SM2018.37.1.4

Keywords:

Diagnostic Techniques, Radioisotope; Isotope Labeling; Radioisotopes, Gamma Spectrometry; Isotopic Labeling; Radioisotope Diagnostic Techniques; Radioisotope Diagnostics Techniques

Abstract

Ice-free areas are the most biologically active places on the Antarctic continent. Only a few plants and animals have managed to colonize and survive in ice-free regions and are mainly limited to the few areas of exposed rocks, mostly around the coast, and especially associated with the Fildes Peninsula, King George Island / May 25 (near the Artigas Antarctic Scientific Base - Uruguay). The 137Cs is an artificial radioactive isotope byproduct of nuclear tests of the years 1950-1970, which has a global distribution and can be used as a tracer of the soil. In order to measure it, high-resolution gamma spectrometry technique (with hyperpure germanium crystals) is used, which can, together with the 137C measurements, determine the amounts of uranium, thorium and potassium of the tested samples, allowing a general radioisotope characterization of the superficial soil. Ranges of values obtained for 238U, 232Th and 40K were similar to previous studies King George Island / May 25th. But the relatively important values (between 98.47 to 670.64 Bq / m2) of 137Cs, support future work in the use of this element for studies of the Antarctic soil.

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References

(1) Bockheim JG, editor. The Soils of Antarctica (World Soils Book Series). 2015th. Springer, 2015. 322 p.

(2) Nie X, Zhang J, Gao H. Soil Enzyme Activities on Eroded Slopes in the Sichuan Basin, China. Pedosphere 2015; 25(4):489-500.

(3) Sanders CJ, Santos IR, Patchineelam SR, Schaefer C, Silva-Filho EV. Recent 137Cs deposi-tion in sediments of Admiralty Bay, Antarctica. J Environ Radioact 2010; 101(5):421-4.

(4) Ferreira PA, Ribeiro AP, do Nascimento MG, Martins C, de Mahiques MM, Montone RC, et al. 137Cs in marine sediments of Admiralty Bay, King George Island, Antarctica. Sci Total Environ 2013; 443:505-10.

(5) Kuzmann E, Schuch L, Garg V, de Souza Junior PA, Guimarães EM, de Oliveira AC, et al. Maritime Antarctica soils studied by Mössbauer spectrosco-py and other methods. Braz. J. Phys. [online]. 1998, vol.28, n.4, pp.00-00. Disponible en: http://www.scielo.br/pdf/bjp/v28n4/garg.pdf [Consulta 16/01/2018].

Published

2018-06-30

How to Cite

1.
Tassano M, Irigoyen J, González J, Cabrera M. Characterization of the Antarctic soil of King George Island/25 May by gamma spectrometry. Salud mil [Internet]. 2018 Jun. 30 [cited 2026 Jun. 11];37(1):30-3. Available from: https://revistasaludmilitar.uy/ojs/index.php/Rsm/article/view/95

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