Environmental Alpha Radiation from the Soil at a Prehispanic Ancient Sacred Site in Lima, Perú

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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...

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Detalles Bibliográficos
Autores: Díaz, Félix, Liza, Rafael, Rojas, Jhonny, Pereyra, Patrizia, Lopez, Maria Elena, Palacios, Daniel, Sajo-Bohus, Laszlo, Benites, Santiago
Formato: artículo
Fecha de Publicación:2023
Institución:Universidad Autónoma del Perú
Repositorio:AUTONOMA-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.autonoma.edu.pe:20.500.13067/2909
Enlace del recurso:https://hdl.handle.net/20.500.13067/2909
https://doi.org/10.12912/27197050/174034
Nivel de acceso:acceso abierto
Materia:Alpha particles
Radon
Natural radioactivity
https://purl.org/pe-repo/ocde/ford#2.07.00
Descripción
Sumario: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-39TM 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/m^3). 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-concentration map. The iso-concentration map reveals a relation between areas with elevated radon levels and the good preservation of funerary contexts.
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