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The potential use of thorium (Th) and uranium (U) as nuclear fuels underscores the importance of developing materials for their sustainable recovery. The production of Th and U requires the separation of these elements from rare-earth elements (REEs) as they often coexist in various feedstocks. Equally crucial is efficiently isolating scandium (Sc) from REEs, considering its high-value status and pivotal role in advanced alloy technologies. This study introduces a new selective ligand-functionalized silica sorbent for extracting Sc, other REEs, Th, and U from solutions with varying pH and elemental compositions. The functionalized sorbent exhibits exceptional selectivity for Sc ions at pH 4 across solutions containing 3-20 elements. It also shows excellent selectivity for Th at pH 2 in 18- and 20-element solutions and substantial selectivity for U in 18- and 20-element solutions at pH 4. Additionally, it efficiently adsorbs neodymium (Nd), dysprosium (Dy), and lanthanum (La) in Sc-free solutions with a given preference for Nd. The ligand-functionalized sorbent successfully undergoes ten cycles of reuse which along with its enhanced recovery performance toward targeted elements highlights its industrial application potential.
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http://dx.doi.org/10.1002/smsc.202400171 | DOI Listing |
F1000Res
September 2025
Department of Biotechnology, Faculty of Life and Allied Health Sciences, M.S. Ramaiah University of Applied Sciences, Bengaluru, Karnataka, 560054, India.
Background: Chintamani village, Chikkaballapura district, Karnataka, India was found to possess high aquifer uranium concentrations. Geologically, Chintamani village is located on bedrock that is rich in elements like potassium (K) that naturally contain high levels of radioactive elements, such as uranium and thorium, due to the presence of alkali-feldspar granites and gneisses. Aquifer depletion has caused the concentration of these elements in groundwater to increase over time, posing a potential health hazard to the residents of Chintamani village.
View Article and Find Full Text PDFSci Rep
September 2025
Federal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, 30655, Hannover, Germany.
The strategic importance of metals found in deep-sea polymetallic nodules has spurred a surge in interest for their exploitation. However, nodules are known to incorporate radionuclides during their growth, so that any industrial processing would involve classifying them as naturally occurring radioactive materials (NORM). As the start of deep-sea mining gets closer, concerns about elevated exposure to radiation that could result from the handling of nodules has recently been raised.
View Article and Find Full Text PDFAppl Radiat Isot
August 2025
Department of Radiochemistry and Radioecology, University of Pannonia, Veszprém, Hungary. Electronic address:
The natural background radiation to humans comes both from outside the Earth (cosmic radiation) and from radioactive isotopes found on Earth (terrestrial radiation). Radionuclides of terrestrial origin are partly external exposure and partly internal exposure via ingestion and inhalation. One of the most important sources of external terrestrial radiation is soil, where the most significant isotopes found are uranium-238, uranium-235 and thorium-232, members of the decay series, and potassium-40.
View Article and Find Full Text PDFAn Acad Bras Cienc
August 2025
Observatório Nacional - ON, Rua General José Cristino, 77, Vasco da Gama, 20921-400 Rio de Janeiro, RJ, Brazil.
Heat loss from Earth's interior, driven by conduction and convection, influences lithospheric thermal regimes. This heat originates from mantle convection, primordial planetary accretion, and the decay of radioactive heat-producing elements (RHPE: U-238, U-235, Th-232 and K-40), which contribute around 98% of Earth's radiogenic heat production, crucial for surface radioactive heat flux (SRHF). Understanding RHPE is key to studying geothermal dynamics, especially in volcanic regions like Trindade Island, Brazil.
View Article and Find Full Text PDFEnviron Geochem Health
August 2025
Departamento de Geologia, Universidade Estadual Paulista (UNESP), Av. 24- No. 1515, Rio Claro, SP, CEP 13506-900, Brasil.
Historically, in the past years, the Pardo River watershed in the Brazilian State of São Paulo has provided enough water resources for people living there. However, with an increasing population, growing urbanization, industrialization, and higher living standards, groundwater became extensively exploited from bores that reached various aquifer systems occurring in that hydrographic basin. Hydrogeochemical surveys involve the acquisition of mandatory parameters to evaluate the water quality and to understand some processes taking place in the aquifers.
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