Vol.:(0123456789)
Journal of Radioanalytical and Nuclear Chemistry
https://doi.org/10.1007/s10967-025-10078-2
Mineralogical investigation and environmental radioactivity risk
of uranium mineralization from altered granites
Mahmoud R. Khattab
1
· Neveen S. Abed
1
· Mohamed H. E. Monged
2
· A. F. Tawfic
3
· Sherif A. Taalab
4
·
Turki Kh. Faraj
5
· Mayeen Uddin Khandaker
6,7,9
· Mohamed Y. Hanfi
8,10
Received: 5 November 2024 / Accepted: 8 March 2025
© Akadémiai Kiadó Zrt 2025
Abstract
The study explores uranium series disequilibrium in altered granites to evaluate uranium mineralization and its radiochro-
nological implications. Disequilibrium occurs due to chemical fractionation and alpha-recoil mechanisms, affecting isotopic
ratios (
238
U,
234
U,
230
Th,
226
Ra) and resource assessment. Gamma-ray spectrometry indicated varied radioactivity ratios
234
U/
238
U close to equilibrium (⁓1) and others deviating (0.85–1.08), revealing uranium mobilization and secondary miner-
alization processes. The ratios of
238
U/
235
U (21.97–26.91) vs. 21.7 imply alteration processes. These findings provide insights
into the geochemical history and uranium migration within granites, aiding uranium resources evaluation and exploration
by interpreting migration history and disequilibrium’s role in deposit accuracy.
Keywords Geochronology · Environmental radioactivity · Uranium · Thorium · Isotopic ratios · Granitic ore · Gamma
spectrometry
Introduction
The fundamental element indispensable to the growth and
development of any nation is energy. Consequently, there
is an imperative for the utilization of renewable energy
sources. Nuclear energy is receiving increased attention
due to the rapid depletion of fossil fuel supplies and the
associated issues with thermal energy emissions [1]. Ura-
nium, a pivotal nuclear fuel, is imperative for the sustained
and future expansion of nuclear energy. To this end, Egypt
is currently undertaking an extensive exploration initiative
across multiple regions, with the objective of identifying
new uranium deposits and reserves. In the majority of cases,
the accurate assessment of resources has been hindered by
* Sherif A. Taalab
sheriftaalab@azhar.edu.eg
* Mohamed Y. Hanfi
mokhamed.khanfi@urfu.ru
1
Department of Geochemical Exploration, Nuclear Materials
Authority (NMA), P.O. Box 530, El-Maadi, Cairo, Egypt
2
Department of Siting and Environment, Nuclear
and Radiological Safety Research Center (NRSRC), Egyptian
Atomic Energy Authority (EAEA), Nasr City, Cairo 11762,
Egypt
3
Nuclear Engineering Department, Military Technical
College, Kobry El Kobbah, Cairo, Egypt
4
Department of Geology, Faculty of Science, Al-Azhar
University, Cairo 11884, Egypt
5
Department of Soil Science, College of Food
and Agricultural Sciences, King Saud University, Riyadh,
Saudi Arabia
6
Centre for Applied Physics and Radiation Technologies,
Faculty of Engineering and Technology, Sunway University,
47500 Bandar Sunway, Selangor, Malaysia
7
Faculty of Graduate Studies, Daffodil International
University, Daffodil Smart City, Birulia, Savar, Dhaka 1216,
Bangladesh
8
Ural Federal University, Ekaterinburg, Russia 620002
9
Department of Physics, College of Science, Korea University,
145 Anam-ro, Seongbuk-gu, Seoul 02841, Republic of Korea
10
Department of Medical and Radiological Research, Nuclear
Materials Authority (NMA), P.O. Box 530, El-Maadi, Cairo,
Egypt