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Название: The radiation shielding competence and imaging spectroscopic based studies of Iron ore region of Kozhikode district, Kerala
Авторы: Arivazhagan, S.
Naseer, K. A.
Mahmoud, K. A.
Bassam, S. A.
Naseef, Mohammed, P. N.
Libeesh, N. K.
Sachana, A. S.
Sayyed, M. I.
Alqahtani, M. S.
El, Shiekh, E.
Khandaker, M. U.
Дата публикации: 2023
Издатель: Korean Nuclear Society
Библиографическое описание: Arivazhagan, S, Naseer, KA, Mahmoud, KA, Bassam, SA, Naseef Mohammed, PN, Libeesh, NK, Sachana, AS, Sayyed, MI, Alqahtani, MS, El Shiekh, E & Khandaker, MU 2023, 'The radiation shielding competence and imaging spectroscopic based studies of Iron ore region of Kozhikode district, Kerala', Nuclear Engineering and Technology, Том. 55, № 7, стр. 2380-2387. https://doi.org/10.1016/j.net.2023.03.038
Arivazhagan, S., Naseer, K. A., Mahmoud, K. A., Bassam, S. A., Naseef Mohammed, P. N., Libeesh, N. K., Sachana, A. S., Sayyed, M. I., Alqahtani, M. S., El Shiekh, E., & Khandaker, M. U. (2023). The radiation shielding competence and imaging spectroscopic based studies of Iron ore region of Kozhikode district, Kerala. Nuclear Engineering and Technology, 55(7), 2380-2387. https://doi.org/10.1016/j.net.2023.03.038
Аннотация: Hyperspectral data and its ability to explore the minerals and their associated rocks have a remarkable application in mineral exploration and lithological characterization. The present study aims to explore the radiation shielding aspects of the iron ore in Kerala with the aid of the Hyperion hyperspectral dataset. The reflectance-spectra obtained from the laboratory conditions as well as from the image show various absorptions. The results from the spectra are validated with geochemical data and GPS points. The Monte Carlo simulation employed to evaluate the radiation shielding ability. Raising the oxygen ions caused a noteworthy decrease in the μ values of the studied rocks which is accompanied by an increase in Δ0.5 and Δeq values. The Δ0.5 and Δeq values increased by factors of approximately 77 % with raising the oxygen ions between 44.32 and 47.57 wt.%. The μ values varies with the oxygen concentrations, where the μ values decreased from 2.531 to 0.925 cm−1 (at 0.059 MeV), from 0.381to 0.215 cm−1 (at 0.662 MeV), and from 0.279 to 0.158 cm−1 (at 1.25 MeV) with raising the oxygen ions from 44.32 to 47.43 wt.%. © 2023 Korean Nuclear Society
Ключевые слова: BUILDING MATERIALS
HVL
IRON ORE AND ITS ASSOCIATED ROCKS
MAC
RADIATION SHIELDING
URI: http://elar.urfu.ru/handle/10995/130538
Условия доступа: info:eu-repo/semantics/openAccess
cc-by-nc-nd
Текст лицензии: https://creativecommons.org/licenses/by-nc-nd/4.0/
Идентификатор SCOPUS: 85160757484
Идентификатор WOS: 001015354900001
Идентификатор PURE: 40103701
ISSN: 1738-5733
DOI: 10.1016/j.net.2023.03.038
Сведения о поддержке: King Khalid University, KKU: RCAMS/KKU/03-22
This work was supported by the King Khalid University through a grant RCAMS/KKU/03-22 under the Research Center for Advance Materials (RCAMS) at King Khalid University , Saudi Arabia.
Располагается в коллекциях:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

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