Atmospheric 14CH4, 14CO2 and 37Ar measurements around a Swiss pressurized water reactor during an annual revision period

Since the 1980s, radiocarbon (<sup>14</sup>C) has gained attention as a valuable tool to quantify the amount of fossil and non-fossil emissions of CO<sub>2</sub> and CH<sub>4</sub> in the atmosphere. Since the 1970s, however, important <sup>14</sup>C emissions in the atmosphere also occur through the operation of nuclear power plants. The limited knowledge about these emissions challenges the use of <sup>14</sup>C as a universal source apportionment tool. Depending on the reactor type, <sup>14</sup>C is emitted in different forms; in particular, pressurized water reactors emit <sup>14</sup>C as a mixture of <sup>14</sup>CH<sub>4</sub> and <sup>14</sup>CO<sub>2</sub>. However, few atmospheric <sup>14</sup>C measurements close to nuclear power plants are available, which mostly address <sup>14</sup>CO<sub>2</sub> emissions. Argon-37 (<sup>37</sup>Ar) can also be produced in nuclear reactors; however, its atmospheric measurement is challenging, resulting in limited available data. In this study, we sampled ambient air during 20-75 min into 18 individual bags around the pressurized water reactor in Gösgen, Switzerland, at the beginning of the annual revision period in 2019, when <sup>14</sup>C and <sup>37</sup>Ar emissions can be expected due to the depressurization of the reactor. These samples were analyzed for <sup>14</sup>CH<sub>4</sub>, <sup>14</sup>CO<sub>2</sub> and partly for <sup>37</sup>Ar. About 1 km downwind of the stack, we found background-corrected activities up to 1900, 370, and 93 mBq m<sup>-3</sup> respectively. Considering corresponding background activities of 0.3, 48 and 2 mBq m<sup>-3</sup> for <sup>14</sup>CH<sub>4</sub>, <sup>14</sup>CO<sub>2</sub>, and <sup>37</sup>Ar, this represents an excess of about 6300, 7.4, and 47 times, respectively. Using an atmospheric dispersion model, we satisfactorily simulated the <sup>14</sup>CH<sub>4</sub> and <sup>14</sup>CO<sub>2</sub> activities in the surroundings of the reactor during this event. Our measurements emphasize the importance of nuclear power plants in the interpretation of atmospheric <sup>14</sup>C measurements and show that pressurized water reactors represent a serious limitation in the use of <sup>14</sup>C for source apportionment of CH<sub>4</sub> sources. Our results also provide insights into the approximate magnitude of civilian <sup>37</sup>Ar emissions from nuclear facilities specifically during maintenance operations.

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Journal
Journal of Environmental Radioactivity
Published
2024-11-24
DOI
https://doi.org/10.1016/j.jenvrad.2024.107576
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
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article

Atmospheric 14CH4, 14CO2 and 37Ar measurements around a Swiss pressurized water reactor during an annual revision period

Christophe Espic, Roland Purtschert, Thomas Laemmel, Stephan Henne et al.
Journal of Environmental Radioactivity
Atmospheric and Environmental Gas Dynamics
article

Atmospheric 14CH4, 14CO2 and 37Ar measurements around a Swiss pressurized water reactor during an annual revision period

Christophe Espic, Roland Purtschert, Thomas Laemmel, Stephan Henne, Sönke Szidat
article en

Abstract

Since the 1980s, radiocarbon (<sup>14</sup>C) has gained attention as a valuable tool to quantify the amount of fossil and non-fossil emissions of CO<sub>2</sub> and CH<sub>4</sub> in the atmosphere. Since the 1970s, however, important <sup>14</sup>C emissions in the atmosphere also occur through the operation of nuclear power plants. The limited knowledge about these emissions challenges the use of <sup>14</sup>C as a universal source apportionment tool. Depending on the reactor type, <sup>14</sup>C is emitted in different forms; in particular, pressurized water reactors emit <sup>14</sup>C as a mixture of <sup>14</sup>CH<sub>4</sub> and <sup>14</sup>CO<sub>2</sub>. However, few atmospheric <sup>14</sup>C measurements close to nuclear power plants are available, which mostly address <sup>14</sup>CO<sub>2</sub> emissions. Argon-37 (<sup>37</sup>Ar) can also be produced in nuclear reactors; however, its atmospheric measurement is challenging, resulting in limited available data. In this study, we sampled ambient air during 20-75 min into 18 individual bags around the pressurized water reactor in Gösgen, Switzerland, at the beginning of the annual revision period in 2019, when <sup>14</sup>C and <sup>37</sup>Ar emissions can be expected due to the depressurization of the reactor. These samples were analyzed for <sup>14</sup>CH<sub>4</sub>, <sup>14</sup>CO<sub>2</sub> and partly for <sup>37</sup>Ar. About 1 km downwind of the stack, we found background-corrected activities up to 1900, 370, and 93 mBq m<sup>-3</sup> respectively. Considering corresponding background activities of 0.3, 48 and 2 mBq m<sup>-3</sup> for <sup>14</sup>CH<sub>4</sub>, <sup>14</sup>CO<sub>2</sub>, and <sup>37</sup>Ar, this represents an excess of about 6300, 7.4, and 47 times, respectively. Using an atmospheric dispersion model, we satisfactorily simulated the <sup>14</sup>CH<sub>4</sub> and <sup>14</sup>CO<sub>2</sub> activities in the surroundings of the reactor during this event. Our measurements emphasize the importance of nuclear power plants in the interpretation of atmospheric <sup>14</sup>C measurements and show that pressurized water reactors represent a serious limitation in the use of <sup>14</sup>C for source apportionment of CH<sub>4</sub> sources. Our results also provide insights into the approximate magnitude of civilian <sup>37</sup>Ar emissions from nuclear facilities specifically during maintenance operations.

Journal of Environmental RadioactivityVol. 281
University of Bern (CH), Oeschger Centre for Climate Change Research (CH), Swiss Federal Laboratories for Materials Science and Technology (CH)
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Clean water and sanitation
Openalex Percentile: Top 81%
Atmospheric and Environmental Gas Dynamics
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