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Gamma activity concentrations of 226Ra, 232Th, 40K, and health hazard assessments of granites from Wadi El-Nabi’ mining area, Egyptian Nubian Shield
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  • Published: 14 February 2026

Gamma activity concentrations of 226Ra, 232Th, 40K, and health hazard assessments of granites from Wadi El-Nabi’ mining area, Egyptian Nubian Shield

  • Aya S. Shereif1,2,
  • Mohamed Th. S. Heikal1,
  • Abdel Salam Abu El Ela1,
  • Ahmed El Shabasy3,
  • Ahmed E. Masoud1 &
  • …
  • Árpád Csámer2,4 

Scientific Reports , Article number:  (2026) Cite this article

  • 698 Accesses

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We are providing an unedited version of this manuscript to give early access to its findings. Before final publication, the manuscript will undergo further editing. Please note there may be errors present which affect the content, and all legal disclaimers apply.

Subjects

  • Environmental sciences
  • Natural hazards
  • Solid Earth sciences

Abstract

Granitic rocks constitute one of the most prevalent and economically significant lithologies, owing to their abundance, mechanical durability, and aesthetic appeal, which render them highly suitable as ornamental stones in architectural and construction applications. In recent years, extensive research efforts have been directed toward quantifying the radiological hazards posed by naturally occurring radioactive materials within these rocks, concerning their potential implications for human health and environmental safety when utilized in building materials. In the present study, a comprehensive radiometric investigation was conducted on 35 granitic rock samples of Wadi El-Nabi’ mining area, specifically El-Igl El-Ahmer monzo-syenogranites, to quantify the activity concentrations of principal radionuclides, including 226Ra, 232Th, and 40K, utilizing gamma spectrometry with a high-purity germanium (HPGe) detector. Furthermore, an array of radiological hazard indices was systematically calculated to evaluate the potential radiological risks associated with these granitoid specimens. Our findings indicate that the mean activity concentrations of 226Ra, 232Th, and 40K in the monzogranite samples were 29 (± 6), 34 (± 6), and 883 (± 49) Bq/kg, respectively. In comparison, the syenogranite samples exhibited slightly elevated average values, measured at 31 (± 5), 35 (± 4), and 890 (± 9) Bq/kg for the corresponding radionuclides, reflecting a modest enrichment in radioactivity within the syenogranitic lithology. With respect to the radiological parameters, the results indicate that Dout, Din, AEDEin, ELCRout, ELCRin, Iγ, and AGDE for both monzogranite and syenogranite samples exceed the internationally recommended reference levels. Conversely, Raeq, AEDEout, Hex, and Hin remain within acceptable global thresholds. 232Th/226Ra (238U) ratios for the monzogranite and syenogranite samples range from 0.88 to 1.39 (mean 1.15 ± 0.14) and 0.88 to 1.41 (mean 1.14 ± 0.16), respectively. These values are markedly lower than the canonical crustal Th/Ra ratio of ~ 3.5, indicating post-magmatic hydrothermal alteration and selective uranium enrichment within the host granitoids. This radiological evidence is reinforced by remote sensing observations, which reveal characteristic alteration patterns, including kaolinization, sericitization, fluoritization, and silicification zones, that are spatially associated with the monzo-syenogranitic units, especially in the buffer location. Consequently, the granitic rocks in certain localized areas, particularly where radionuclide concentrations or radiological hazard indices exceed typical thresholds, may be considered unsuitable for use as construction materials.

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Data availability

All data generated and analysed during this study are included in this published article and its supplementary information files.

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Acknowledgements

The authors thank (in depth) to Dr. Gulcan Top. Independent Researcher, Turkey for her constructive help in statistical analysis of the radioactivity concentrations and their risk parameters. Great thanks to NASA and USGS for providing the data, and for the University of Debrecen for their support.

Funding

Open access funding provided by University of Debrecen. This work was supported by the University of Debrecen Program for Scientific Publication. Aya S. Shereif received funding from the Stipendium Hungaricum Scholarship, a joint executive program between Hungary and Egypt.

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Authors and Affiliations

  1. Geology Department, Faculty of Science, Tanta University, Tanta, 31527, Egypt

    Aya S. Shereif, Mohamed Th. S. Heikal, Abdel Salam Abu El Ela & Ahmed E. Masoud

  2. Department of Mineralogy and Geology, University of Debrecen, Debrecen, 4032, Hungary

    Aya S. Shereif & Árpád Csámer

  3. The Radiation Protection Department, Nuclear and Radiological Regulatory Authority (ENRRA), Cairo, Egypt

    Ahmed El Shabasy

  4. Cosmochemistry and Cosmic Methods Research Group, University of Debrecen, Debrecen, 4032, Hungary

    Árpád Csámer

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Contributions

Conceptualization, Aya S. Shereif and Mohamed Heikal; Methodology, Aya S. Shereif; Software, Aya S. Shereif; Validation, Aya S. Shereif, Árpád Csámer, Ahmed El Shabasy and Ahmed Masoud; Formal analysis, Ahmed El Shabasy; Investigation, Árpád Csámer; Resources, Aya S. Shereif and Ahmed El Shabasy; Data curation, Aya S. Shereif, Árpád Csámer, Mohamed Heikal and Abdel Salam Abu El Ela; Writing the original draft preparation, Aya S. Shereif, Mohamed Heikal, Abdel Salam Abu El Ela and Ahmed Masoud; Writing—review and editing, Árpád Csámer, Aya S. Shereif and Mohamed Heikal; Visualization, Aya S. Shereif, Ahmed El Shabasy and Ahmed Masoud; Supervision, Mohamed Heikal, Abdel Salam Abu El Ela and Árpád Csámer; Project administration, Árpád Csámer; Funding acquisition, Árpád Csámer. All authors have read and agreed to the published version of the manuscript.

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Correspondence to Árpád Csámer.

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Shereif, A.S., Heikal, M.T.S., El Ela, A.S.A. et al. Gamma activity concentrations of 226Ra, 232Th, 40K, and health hazard assessments of granites from Wadi El-Nabi’ mining area, Egyptian Nubian Shield. Sci Rep (2026). https://doi.org/10.1038/s41598-026-39664-4

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  • Received: 28 July 2025

  • Accepted: 06 February 2026

  • Published: 14 February 2026

  • DOI: https://doi.org/10.1038/s41598-026-39664-4

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Keywords

  • Gamma index
  • HPGe detector
  • Health hazard indices
  • Wadi El-Nabi’ mining area
  • Egyptian Nubian Shield
  • And hydrothermal alteration
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