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Author: search.filters.author.Jhonny RojasSubject: search.filters.subject.Radon

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    An approach to the measurement of radon permeability and transmission factor using Cr-39 detectors inside a diffusion chambers exposed in a new-build radon chamber
    (RELX Group (Netherlands), 2022-01-01)
    Many CR-39 (poly allyl glycol carbonate) detectors inside two different diffusion chambers were used to study the radon permeability and the radon transmission factor. This factor represents the percentage of radon concentration that truly enters a diffusion chamber, since there is a loss of radon concentration inside the chamber compared to the outside radon concentration, due to the radioactive nature of radon gas. Here, a theoretical discussion is presented, followed by an experimental study that was carried out in a new-build radon chamber. These initial results are presented in order to check the reliability of the radon chamber. The most remarkable observation is that research consistently shows that the obtained value of radon permeability constant for a commercial membrane is 4.404×10 − 8±0.012×10 − 8cm2/s, which is in a good agreement with literature data.
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    Environmental Alpha Radiation from the Soil at a Prehispanic Ancient Sacred Site in Lima, Perú
    (Polskie Towarzystwo Inzynierii Ekologicznej (PTIE), 2023-01-01)
    In the present work, we investigate the concentration of radon and its alpha-emitting progeny at the archaeological site of Huaca 20 in Lima, Peru. The site holds significant cultural and historical importance as an ancient pre-Inca ruin, providing valuable insights into the lives and rituals of its former inhabitants. We quantified the radon levels accurately with passive CR-39™ detectors deployed within specially designed chambers at the site for 28 days. In a controlled laboratory environment, we processed the detectors afterward, examining and analyzing the resulting tracks using advanced microscopy and the ImageJ analysis software. The ground-level concentration of radon and its alpha-emitting progeny was determined, revealing elevated levels ranging from 2.4 ± 0.6 to 8.9 ± 0.9 (kBq/m3). These findings underscore the unique presence of radon at Huaca 20 and highlight the potential impact on microorganisms at ground level. Likewise, these results can contribute to studies on the radiological risks faced by visitors, excavators and archaeologists. Finally, we show the spatial distribution of radon concentrations within the site by creating an iso-concentra-tion map. The iso-concentration map reveals a relation between areas with elevated radon levels and the good preservation of funerary contexts.