Gamma spectrometric measurements to determine the isotopic composition and total uranium mass in UO pellets (D = 7.5 mm; H = 3.5 mm, ρ = 10 g/cm) were carried out. The required efficiency curve was obtained by applying the efficiency transfer method from a calibration standard (D = 65 mm; H = 20 mm) of a slightly acidified water solution. The average isotopic composition of ten UO pellets was consistent with values of natural uranium given by IUPAC. The average relative bias for the U/U amount ratio was -0.73% using the 1001 keV gamma line for U and 0.50% using the 63 keV gamma line (186 keV was always used for U). For the total uranium mass, the mean deviation as compared to mass determinations using a balance was 5.5% using the 1001 keV gamma line for U and 4.3% using the 63 keV gamma line.
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http://dx.doi.org/10.1016/j.apradiso.2022.110607 | DOI Listing |
Proc Natl Acad Sci U S A
January 2025
Cosmochemistry and Isotope Signatures Group Nuclear and Chemical Sciences Division Lawrence Livermore National Laboratory, Livermore, CA 94550.
The radiogenic isotopic compositions of basaltic Martian meteorites (shergottites) and clinopyroxene/olivine cumulate meteorites (nakhlite/chassignites) are used to define the global evolution of Mars. However, the two main groups of meteorites demonstrate that their sources underwent divergent styles of magmatic evolution. The shergottites portray a planet that differentiated ~4.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
January 2025
School of Physical Sciences, The Open University, Milton Keynes MK7 6AA, United Kingdom.
Much has been learned about Mars through data returned from space missions and analyses of martian meteorites. There are, however, many questions still outstanding which cannot currently be answered-including the issue of whether there is, or was, life on Mars. The return of a cache of samples-including of the atmosphere-from separate locations in Jezero Crater and with differing petrogeneses will provide the international community with the opportunity to explore part of the evolutionary history of Mars in great detail.
View Article and Find Full Text PDFDalton Trans
January 2025
Key Laboratory of Nonferrous Metal Chemistry and Resources Utilization of Gansu Province and State Key Laboratory of Applied Organic Chemistry, Frontiers Science Center for Rare Isotopes, College of Chemistry and Chemical Engineering, Lanzhou University, 73000 Lanzhou, China.
Curr Res Food Sci
December 2024
Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, via G. Campi, 103, 41125 Modena, Italy.
Stable isotope analysis has become a valuable tool for studying food chain processes and verifying the authenticity and geographical origin of typical products. The analysis is particularly important for those foods with geographical indications, such as Aceto Balsamico Tradizionale di Modena labelled with the protected designation of origin mark (ABTM PDO) and Aceto Balsamico di Modena with the protected geographical indication (ABM PGI). Understanding how the aging process affects the isotopic composition of specific compounds in ABTM is important for distinguishing between traditional and non-traditional products, as well as for verifying their authenticity.
View Article and Find Full Text PDFiScience
December 2024
Department of Molecular Environmental Biotechnology, Helmholtz-Centre for Environmental Research - UFZ, 04318 Leipzig, Saxony, Germany.
Protein-based stable isotope probing (protein-SIP) can link microbial taxa to substrate assimilation. Traditionally, protein-SIP requires a sample-specific metagenome-derived database for samples with unknown composition. Here, we describe GroEL-prototyping-based stable isotope probing (GroEL-SIP), that uses GroEL as a taxonomic marker protein to identify bacterial taxa (GroEL-proteotyping) coupled to SIP directly linking identified taxa to substrate consumption.
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