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Vertical distribution and radiological risk assessment of (137)Cs and natural radionuclides in soil samples

The aims of this study were to investigate the vertical distributions of natural radionuclides (232)Th, (226)Ra and (40)K as well as anthropogenic radionuclide (137)Cs in soil samples and to analyze the correlation among the radioactivity of these radionuclides and the physiochemical characteristics...

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Detalles Bibliográficos
Autores principales: Ahmad, Ayesha Y., Al-Ghouti, Mohammad A., AlSadig, Ibrahim, Abu-Dieyeh, Mohammed
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6704082/
https://www.ncbi.nlm.nih.gov/pubmed/31434929
http://dx.doi.org/10.1038/s41598-019-48500-x
Descripción
Sumario:The aims of this study were to investigate the vertical distributions of natural radionuclides (232)Th, (226)Ra and (40)K as well as anthropogenic radionuclide (137)Cs in soil samples and to analyze the correlation among the radioactivity of these radionuclides and the physiochemical characteristics of soil samples namely pH, grain size, carbonate content and organic matter. Risk assessment of the radiological hazard has also been estimated. Forty-four soil samples were collected from eleven locations in Qatar at four depth levels from 0 to 16 cm. The average concentrations of (232)Th, (226)Ra, (40)K and (137)Cs in the soil depth of 16 cm were 10, 17, 201 and 4 Bq/kg, respectively, which were within the reported world mean. The external absorbed gamma dose rate, the annual effective dose, the mean radium equivalent activity, the external hazard index and the lifetime cancer risk were 22 nGy/h, 0.027 mSv/y, 47 Bq/kg, 0.125 and 0.096 × 10(−3), respectively. These values were far below the minimum recommended international values. The level of radioactivity concentrations in the soil was affected by the physiochemical characteristics of the soil. The positive correlation with highest R(2) value was found among the radioactivity concentrations of (232)Th and (40)K and the soil clay content. Total organic carbon was also positively correlated for (226)Ra and (137)Cs activity concentrations, whereas, carbonate content was negatively correlated with the radioactivity concentrations of (232)Th and (40)K. As far as soil moisture content is concerned, the positive correlation with highest R(2) value was obtained for (226)Ra activity concentrations.