A monitoring program was undertaken to determine the levels of airborne radioactive 14CO2 in an operating waste management area, and it its vicinity. As a part of this program, alkaline microporous pellets, recently developed, were used to sample the 14CO2 in air near waste storage structures and near the waste management area. These pellets were never fully characterized for their ability to capture high levels of 14CO2, and the processing and analysis needed to be improved to provide data on recoveries and consistencies, for an eventual method validation, with independent calibrations and standards. The sample analysis scheme also had to accommodate 14CO2 levels varying from near the natural background (250 Bq kg-1 C), to potentially three to four orders of magnitude above this value, near the wastes. The porous alkaline solid pellets were used for the passive capture of airborne 14CO2 over a period of weeks, to a few months. The pellets were processed to release the captured CO2 (14CO2 and 12CO2) into a NaOH solution, which was subsequently analyzed by liquid scintillation. Processing of the pellets yielded a 14C recovery of 96.0 +/- 4.2% and a lower, but consistent total carbon recovery, i.e., 85.9 +/- 2.7 and 86.9 +/- 2.6%, for procedural blanks and standards, respectively. The detection limits for the pellet sampling and processing was sufficient to reach environmental levels. For the higher levels of 14CO2 and for 'spot' sampling, we also used air samples, pumped into a NaOH solution to trap the 14CO2. These NaOH solutions were counted directly for 14C, also by liquid scintillation. The method limits of this latter technique, although much higher than for pellet samples, also achieved the performance objective for detecting airborne 14CO2. Both sampling and processing techniques, when used together, provided sufficient flexibility to be used for low (environmental) levels and high levels, near the wastes.
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http://dx.doi.org/10.1039/b111579k | DOI Listing |
J Environ Radioact
January 2025
Department of Chemistry, Biochemistry and Pharmaceutical Sciences, University of Bern, Freiestrasse 3, 3012, Bern, Switzerland; Oeschger Centre for Climate Change Research, University of Bern, Hochschulstrasse 4, 3012, Bern, Switzerland. Electronic address:
Since the 1980s, radiocarbon (C) has gained attention as a valuable tool to quantify the amount of fossil and non-fossil emissions of CO and CH in the atmosphere. Since the 1970s, however, important C emissions in the atmosphere also occur through the operation of nuclear power plants. The limited knowledge about these emissions challenges the use of C as a universal source apportionment tool.
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Departamento de Bioquímica, Facultad de Química-Universidad Nacional Autónoma de México, CDMX, México.
Seed development requires substantial metabolic resources and is influenced by adverse environmental conditions. However, the ability of plants to produce viable seeds under restrictive conditions suggests the existence of mechanisms that make this process less sensitive to environmental stress. Uncovering their regulation could lead to the development of genotypes better adapted to stressful conditions.
View Article and Find Full Text PDFEnviron Sci Technol
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National Isotope Center, GNS Science, Lower Hutt 5040, New Zealand.
Independent identification of carbon emission peaks determined from fuel inventories is a challenging goal. Because of the complete depletion of radiocarbon (C) in fossil fuel sources, the measurement of atmospheric CO has proven to offer a means of achieving this goal. Here, we present a study identifying peak carbon emissions from two Chinese cities using urban tree-ring ΔC time series during 2000-2019.
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Department of Biology, Indiana University, Bloomington, IN, United States.
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