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dc.contributor.authorOhta, Tomokoen
dc.contributor.authorFifield, L. Keithen
dc.contributor.authorPalcsu, Lászlóen
dc.contributor.authorTims, Stephen G.en
dc.contributor.authorPavetich, Stefanen
dc.contributor.authorMahara, Yasunorien
dc.contributor.alternative馬原, 保典ja
dc.date.accessioned2023-11-27T06:07:12Z-
dc.date.available2023-11-27T06:07:12Z-
dc.date.issued2023-11-11-
dc.identifier.urihttp://hdl.handle.net/2433/286181-
dc.description.abstractThe opportunity to measure the concentrations of ³H and ³⁶Cl released by the Fukushima nuclear accident in 2011 directly in rain was lost in the early stage of the accident. We have, however, been able to reconstruct the deposition record of atmospheric ³H and ³⁶Cl following the accident using a bore hole that was drilled in 2014 at Koriyama at a distance of 60 km from the accident. The contributions of ³H and ³⁶Cl from the accident are 1.4 × 10¹³ and 2.0 × 10¹² atoms m⁻² respectively at this site. Very high concentrations of both ³H (46 Bq L⁻¹) and ³⁶Cl (3.36 × 10¹¹ atoms L⁻¹) were found in the unsaturated soil at depths between 300 and 350 cm. From these, conservative estimates for the ³H and ³⁶Cl concentrations in the precipitation in the ~ 6 weeks following the accident were 607 Bq L⁻¹ and 4.74 × 10¹⁰ atoms L⁻¹, respectively. A second hole drilled in 2016 showed that ³H concentrations in the unsaturated soil and shallow groundwater had returned to close to natural levels, although the ³⁶Cl concentrations were still significantly elevated above natural levels.en
dc.language.isoeng-
dc.publisherSpringer Natureen
dc.rights© The Author(s) 2023en
dc.rightsThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.en
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/-
dc.subjectEnvironmental sciencesen
dc.subjectHydrologyen
dc.titleRecord of ³H and ³⁶Cl from the Fukushima nuclear accident recovered from soil water in the unsaturated zone at Koriyamaen
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.jtitleScientific Reportsen
dc.identifier.volume13-
dc.relation.doi10.1038/s41598-023-46853-y-
dc.textversionpublisher-
dc.identifier.artnum19672-
dc.identifier.pmid37952016-
dcterms.accessRightsopen access-
datacite.awardNumber24686098-
datacite.awardNumber17K07024-
datacite.awardNumber20H02674-
datacite.awardNumber.urihttps://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24686098/-
datacite.awardNumber.urihttps://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17K07024/-
datacite.awardNumber.urihttps://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20H02674/-
dc.identifier.eissn2045-2322-
jpcoar.funderName日本学術振興会ja
jpcoar.funderName日本学術振興会ja
jpcoar.funderName日本学術振興会ja
jpcoar.awardTitle海藻に刻印された人間活動に伴う海洋環境の変遷ja
jpcoar.awardTitle樹木中の放射性セシウム蓄積機構の解明と森林資源汚染の将来予測ja
jpcoar.awardTitleマルチトレーサ法を用いた129I/127I地下水年代測定法の成立性の検証ja
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