{"@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/1363388846231055232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.atmosenv.2007.07.014"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1352231007006280?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1352231007006280?httpAccept=text/plain"}}],"dc:title":[{"@value":"Distinguishing the sources of Asian dust based on electron spin resonance signal intensity and crystallinity of quartz"}],"description":[{"notation":[{"@value":"Abstract   We report a newly developed provenance-tracing method by using a combination of electron spin resonance (ESR) signal intensity of the E1′ center in quartz and crystallinity index (CI) of quartz, which reflect the formation age and crystallization conditions of quartz in their source rocks, respectively. ESR signal intensity and CI were determined for quartz in fine silt plus clay fraction ("}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388846231055238","@type":"Researcher","foaf:name":[{"@value":"Youbin Sun"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055235","@type":"Researcher","foaf:name":[{"@value":"Ryuji Tada"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055234","@type":"Researcher","foaf:name":[{"@value":"Jun Chen"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055232","@type":"Researcher","foaf:name":[{"@value":"Huizhong Chen"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055237","@type":"Researcher","foaf:name":[{"@value":"Shin Toyoda"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055241","@type":"Researcher","foaf:name":[{"@value":"Atsushi Tani"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055236","@type":"Researcher","foaf:name":[{"@value":"Yuko Isozaki"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055239","@type":"Researcher","foaf:name":[{"@value":"Kana Nagashima"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055240","@type":"Researcher","foaf:name":[{"@value":"Hitoshi Hasegawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388846231055233","@type":"Researcher","foaf:name":[{"@value":"Junfeng Ji"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13522310"}],"prism:publicationName":[{"@value":"Atmospheric Environment"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2007-12","prism:volume":"41","prism:number":"38","prism:startingPage":"8537","prism:endingPage":"8548"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S1352231007006280?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S1352231007006280?httpAccept=text/plain"}],"createdAt":"2007-07-18","modifiedAt":"2019-01-06","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004230119508736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"ESR signal intensity and crystallinity of quartz from Gobi and sandy deserts in East Asia and implication for tracing Asian dust provenance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283696087056512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recent 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