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Radiological Hazards Assessment Associated with Granitoid Rocks in Egypt

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dc.contributor.author Gawad, Ahmed E. Abdel
dc.contributor.author Masoud, Masoud S.
dc.contributor.author Khandaker, Mayeen Uddin
dc.contributor.author Hanf, Mohamed Y.
dc.date.accessioned 2024-12-19T03:32:33Z
dc.date.available 2024-12-19T03:32:33Z
dc.date.issued 2024-02-23
dc.identifier.uri http://dspace.daffodilvarsity.edu.bd:8080/handle/123456789/13653
dc.description.abstract The present study aimed to assess the radioactive hazards associated with the application of granitoid rocks in building materials. An HPGe spectrometer was used to detect the levels of the radioactive elements uranium-238, thorium-232, and potassium-40 in the granitoid rocks. The results showed that the levels of these elements were lower (38.32 < 33 Bq kg−1), comparable (47.19–45 Bq kg-1) and higher (992.26 ≫> 412 Bq kg−1) than the worldwide limits for 238U, 232Th, and 40K concentration, respectively. The exposure to gamma radiation of granitoid rocks was studied by various radiological hazard variables like the absorbed dose rate (Dair), the outdoor and indoor annual effective dose (AEDout and AEDin), and excess lifetime cancer risk (ELCR). A variety of statistical methods, including Pearson correlation, principal component analysis (PCA), and hierarchical cluster analysis (HCA) was used, to study the relationship between the radioactive elements and the radiological hazards. According to statistical analysis, the main radioactive risk of granitoid rocks is contributed to by the elements uranium-238, thorium-232, and potassium-40. Granitoid rocks can be applied in building materials, but under control to prevent risk to the public. en_US
dc.language.iso en_US en_US
dc.publisher Elsevier en_US
dc.subject Radiology en_US
dc.subject Egypt en_US
dc.subject Hazards assessment en_US
dc.title Radiological Hazards Assessment Associated with Granitoid Rocks in Egypt en_US
dc.type Article en_US


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