{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360002216857770240.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/srep21543"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/srep21543"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/srep21543.pdf"}},{"identifier":{"@type":"PMID","@value":"26868138"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Cesium adsorption/desorption behavior of clay minerals considering actual contamination conditions in Fukushima"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Cesium adsorption/desorption experiments for various clay minerals, considering actual contamination conditions in Fukushima, were conducted using the <jats:sup>137</jats:sup>Cs radioisotope and an autoradiography using imaging plates (IPs). A 50 μl solution containing 0.185 ~ 1.85 Bq of <jats:sup>137</jats:sup>Cs (10<jats:sup>−11</jats:sup> ~ 10<jats:sup>−9 </jats:sup>molL<jats:sup>−1</jats:sup> of <jats:sup>137</jats:sup>Cs) was dropped onto a substrate where various mineral particles were arranged. It was found that partially-vermiculitized biotite, which is termed “weathered biotite” (WB) in this study, from Fukushima sorbed <jats:sup>137</jats:sup>Cs far more than the other clay minerals (fresh biotite, illite, smectite, kaolinite, halloysite, allophane, imogolite) on the same substrate. When WB was absent on the substrate, the amount of <jats:sup>137</jats:sup>Cs sorbed to the other clay minerals was considerably increased, implying that selective sorption to WB caused depletion of radiocesium in the solution and less sorption to the coexisting minerals. Cs-sorption to WB continued for about one day, whereas that to ferruginous smectite was completed within one hour. The sorbed <jats:sup>137</jats:sup>Cs in WB was hardly leached with hydrochloric acid at pH 1, particularly in samples with a longer sorption time. The presence/absence of WB sorbing radiocesium is a key factor affecting the dynamics and fate of radiocesium in Fukushima.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380847869980619140","@type":"Researcher","foaf:name":[{"@value":"Hiroki Mukai"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869980619143","@type":"Researcher","foaf:name":[{"@value":"Atsushi Hirose"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869980619142","@type":"Researcher","foaf:name":[{"@value":"Satoko Motai"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801187816448","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50832854"},{"@type":"NRID","@value":"1000050832854"},{"@type":"NRID","@value":"9000406039921"},{"@type":"NRID","@value":"9000296661831"},{"@type":"NRID","@value":"9000345287277"},{"@type":"NRID","@value":"9000406037195"},{"@type":"NRID","@value":"9000409475539"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/biotite-1M"}],"foaf:name":[{"@value":"Ryosuke Kikuchi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869980619138","@type":"Researcher","foaf:name":[{"@value":"Keitaro Tanoi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380847869980619137","@type":"Researcher","foaf:name":[{"@value":"Tomoko M. 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