2015
DOI: 10.1016/j.anucene.2014.08.071
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Radiocarbon mass balance for a Magnox nuclear power station

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Cited by 20 publications
(4 citation statements)
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“…However, the contributions from each precursor species are likely to differ due to variations in isotopic abundance and capture cross section, Table 1 . The contributions from each have been examined in the mass balance study of Wylfa Reactor 1 by Metcalfe and Mills [ 12 ], where it was found that for Wylfa in particular, the C-14 precursor C-13 makes a more significant contribution to the total activity than N-14 at 10 wppm. Although it must be stated that this is for Wylfa and not Oldbury as studied in this work and previous work has shown significant differences in these two reactors [ 8 ].…”
Section: Introductionmentioning
confidence: 99%
“…However, the contributions from each precursor species are likely to differ due to variations in isotopic abundance and capture cross section, Table 1 . The contributions from each have been examined in the mass balance study of Wylfa Reactor 1 by Metcalfe and Mills [ 12 ], where it was found that for Wylfa in particular, the C-14 precursor C-13 makes a more significant contribution to the total activity than N-14 at 10 wppm. Although it must be stated that this is for Wylfa and not Oldbury as studied in this work and previous work has shown significant differences in these two reactors [ 8 ].…”
Section: Introductionmentioning
confidence: 99%
“…Activation modelling has also been used successfully to account for C-14 gaseous discharges from a UK Magnox power station [12]. Activation modelling was used to predict C-14 production rates in both the graphite core and the carbon dioxide coolant over a selected period of operation and the results compared with monitored site C-14 discharges.…”
Section: Fispin (Fission Product Inventory) Libraries and Finally Fismentioning
confidence: 99%
“…There are also anthropogenic sources of 14 C. A large amount of 14 C was produced and released as a result of nuclear weapons testing in the 1950s and 60s and subsequently distributed via the carbon cycle, doubling the atmospheric inventory of 14 CO 2 (Nydal and Lovseth 1983;Levin et al 1985;Manning et al 1990). The nuclear power industry also releases 14 CO 2 , which offsets the depletion caused by fossil fuel combustion (Vokal and Kobal 1997;McNamara et al 1998;Fontugne et al 2004;Yim and Caron 2006;Magnusson 2007;Molnar et al 2007;Dias et al 2009;Graven and Gruber 2011;Aulagnier et al 2012;Svetlik et al 2012;Wang et al 2012Wang et al , 2013Wang et al , 2014Vogel et al 2013;Metcalfe and Mills 2015;Tierney et al 2016).…”
Section: Introductionmentioning
confidence: 99%