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dc.contributor.authorFathy, D.en
dc.contributor.authorZakaly, H. M. H.en
dc.contributor.authorLasheen, E. S. R.en
dc.contributor.authorElsaman, R.en
dc.contributor.authorAlarifi, S. S.en
dc.contributor.authorSami, M.en
dc.contributor.authorAwad, H. A.en
dc.contributor.authorEne, A.en
dc.date.accessioned2024-04-05T16:30:30Z-
dc.date.available2024-04-05T16:30:30Z-
dc.date.issued2023-
dc.identifier.citationFathy, D, Zakaly, HMH, Lasheen, ESR, Elsaman, R, Alarifi, SS, Sami, M, Awad, HA & Ene, A 2023, 'Assessing geochemical and natural radioactivity impacts of Hamadat phosphatic mine through radiological indices', PLoS ONE, Том. 18, № 8, e0287422. https://doi.org/10.1371/journal.pone.0287422harvard_pure
dc.identifier.citationFathy, D., Zakaly, H. M. H., Lasheen, E. S. R., Elsaman, R., Alarifi, S. S., Sami, M., Awad, H. A., & Ene, A. (2023). Assessing geochemical and natural radioactivity impacts of Hamadat phosphatic mine through radiological indices. PLoS ONE, 18(8), [e0287422]. https://doi.org/10.1371/journal.pone.0287422apa_pure
dc.identifier.issn1932-6203-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Gold, Green3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85166518303&doi=10.1371%2fjournal.pone.0287422&partnerID=40&md5=574226b00568f98f15a27c7074d025a61
dc.identifier.otherhttps://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0287422&type=printablepdf
dc.identifier.urihttp://elar.urfu.ru/handle/10995/130689-
dc.description.abstractThe utilization of phosphorite deposits as an industrial resource is of paramount importance, and its sustainability largely depends on ensuring safe and responsible practices. This study aims to evaluate the suitability of phosphorite deposits for industrial applications such as the production of phosphoric acid and phosphatic fertilizers. To achieve this goal, the study meticulously examines the geochemical characteristics of the deposits, investigates the distribution of natural Radioactivity within them, and assesses the potential radiological risk associated with their use. The phosphorites are massive and collected from different beds within the Duwi Formation at the Hamadat mining area. They are grain-supported and composed of phosphatic pellets, bioclasts (bones), non-phosphatic minerals, and cement. Geochemically, phosphorites contain high concentrations of P2O5 (23.59-28.36 wt.%) and CaO (40.85-44.35 wt.%), with low amounts of Al2O3 (0.23-0.51 wt.%), TiO2 (0.01-0.03 wt.%), Fe2O3 (1.14-2.28 wt.%), Na2O (0.37-1.19 wt.%), K2O (0.03-0.12 wt.%), and MnO (0.08- 0.18 wt.%), suggesting the low contribution of the detrital material during their deposition. Moreover, they belong to contain enhanced U concentration (55-128 ppm). They are also enriched with Sr, Ba, Cr, V, and Zn and depleted in Th, Zr, and Rb, which strongly supports the low detrital input during the formation of the Hamadat phosphorites. The high Radioactivity of the studied phosphorites is probably due to the widespread occurrence of phosphatic components (e.g., apatite) that accommodate U in high concentrations. Gamma spectrometry based on NaI (Tl) crystal 3×3 has been used to measure occurring radionuclides in the phosphorite samples. The results indicate that the radioactive concentrations' average values of 226Ra, 232Th, and 40K are 184.18±9.19, 125.82±6.29, and 63.82±3.19 Bq Kg-1 , respectively. Additionally, evaluations have been made of the radiological hazards. The calculated risk indicators exceeded the recommended national and world averages. The data obtained will serve as a reference for follow-up studies to evaluate the effectiveness of the Radioactivity of phosphatic materials collected from the Hamdat mine area. © 2023 Fathy et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherPublic Library of Scienceen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.rightscc-byother
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/unpaywall
dc.sourcePLOS ONE2
dc.sourcePLoS ONEen
dc.subjectAPATITEen
dc.subjectPHOSPHATEen
dc.subjectPOTASSIUM 40en
dc.subjectRADIUM 226en
dc.subjectTHORIUM 232en
dc.subjectURANIUMen
dc.subjectFERRIC IONen
dc.subjectPHOSPHORITEen
dc.subjectPOTASSIUMen
dc.subjectRADIUMen
dc.subjectRADIUM-226en
dc.subjectTHORIUMen
dc.subjectTHORIUM-232en
dc.subjectARTICLEen
dc.subjectEGYPTen
dc.subjectGAMMA SPECTROMETRYen
dc.subjectGEOCHEMICAL ANALYSISen
dc.subjectMININGen
dc.subjectNATURAL RADIOACTIVITYen
dc.subjectRADIATION HAZARDen
dc.subjectPROCEDURESen
dc.subjectRADIOACTIVITYen
dc.subjectFERRIC COMPOUNDSen
dc.subjectPOTASSIUM RADIOISOTOPESen
dc.subjectRADIATION MONITORINGen
dc.subjectRADIOACTIVITYen
dc.subjectRADIUMen
dc.subjectTHORIUMen
dc.titleAssessing geochemical and natural radioactivity impacts of Hamadat phosphatic mine through radiological indicesen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.type|info:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1371/journal.pone.0287422-
dc.identifier.scopus85166518303-
local.contributor.employeeFathy, D., Faculty of Science, Geology Department, Minia University, El-Minia, Egypten
local.contributor.employeeZakaly, H.M.H., Faculty of Science, Physics Department, Al-Azhar University, Assiut Branch, Cairo, Egypt, Faculty of Engineering and Natural Sciences, Computer Engineering Department, Istinye University, Istanbul, Turkey, Institute of Physics and Technology, Ural Federal University, Yekaterinburg, Russian Federationen
local.contributor.employeeLasheen, E.S.R., Faculty of Science, Geology Department, Al-Azhar University, Cairo, Egypten
local.contributor.employeeElsaman, R., Faculty of Science, Physics Department, Al-Azhar University, Assiut Branch, Cairo, Egypten
local.contributor.employeeAlarifi, S.S., Department of Geology and Geophysics, College of Science, King Saud University, Riyadh, Saudi Arabiaen
local.contributor.employeeSami, M., Faculty of Science, Geology Department, Minia University, El-Minia, Egypten
local.contributor.employeeAwad, H.A., Faculty of Science, Geology Department, Al-Azhar University, Assiut Branch, Cairo, Egypten
local.contributor.employeeEne, A., Faculty of Sciences and Environment, Department of Chemistry, Dunarea de Jos University of Galati, INPOLDE Research Center, Physics and Environment, Galati, Romaniaen
local.issue8 August-
local.volume18-
dc.identifier.wos001043333000054-
local.contributor.departmentFaculty of Science, Geology Department, Minia University, El-Minia, Egypten
local.contributor.departmentFaculty of Science, Physics Department, Al-Azhar University, Assiut Branch, Cairo, Egypten
local.contributor.departmentFaculty of Engineering and Natural Sciences, Computer Engineering Department, Istinye University, Istanbul, Turkeyen
local.contributor.departmentInstitute of Physics and Technology, Ural Federal University, Yekaterinburg, Russian Federationen
local.contributor.departmentFaculty of Science, Geology Department, Al-Azhar University, Cairo, Egypten
local.contributor.departmentDepartment of Geology and Geophysics, College of Science, King Saud University, Riyadh, Saudi Arabiaen
local.contributor.departmentFaculty of Science, Geology Department, Al-Azhar University, Assiut Branch, Cairo, Egypten
local.contributor.departmentFaculty of Sciences and Environment, Department of Chemistry, Dunarea de Jos University of Galati, INPOLDE Research Center, Physics and Environment, Galati, Romaniaen
local.identifier.pure43268072-
local.description.ordere0287422-
local.identifier.eid2-s2.0-85166518303-
local.identifier.wosWOS:001043333000054-
local.identifier.pmid37535632-
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