Characterization of the Antarctic soil of King George Island/25 May by gamma spectrometry
DOI:
https://doi.org/10.35954/SM2018.37.1.4Keywords:
Diagnostic Techniques, Radioisotope; Isotope Labeling; Radioisotopes, Gamma Spectrometry; Isotopic Labeling; Radioisotope Diagnostic Techniques; Radioisotope Diagnostics TechniquesAbstract
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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