{"@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/1362825894157766144.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001gl014197"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001GL014197"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL014197"}}],"dc:title":[{"@value":"Low‐temperature remanence in stable single domain magnetite"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>A numerical model is developed in order to simulate the loss of low‐temperature remanence while warming through the Verwey transition. We concentrate on the amount of remanence lost (δ<jats:sub><jats:italic>fc</jats:italic></jats:sub> and δ<jats:sub><jats:italic>zfc</jats:italic></jats:sub>) during field cooled and zero field cooled low temperature demagnetization curves for stable single domain (SSD) particles of (1) inorganic magnetite and (2) biogenic magnetite in the form of magnetosome chains. The model predicts that delta ratios (δ<jats:sub><jats:italic>fc</jats:italic></jats:sub>/δ<jats:sub><jats:italic>zfc</jats:italic></jats:sub>) for inorganic SSD magnetite increase from 1 to 1.6 with increasing aspect ratio and that magnetosome chains have elevated delta ratios of at least 2.0. Disaggregated magnetosomes are predicted to behave similarly to inorganic acicular SSD magnetite. The numerical results agree with experimental results.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579818731485186","@type":"Researcher","foaf:name":[{"@value":"Brian Carter‐Stiglitz"}],"jpcoar:affiliationName":[{"@value":"Institute for Rock Magnetism, Newton Horace Winchell School of Earth Sciences University of Minnesota  USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579818731485185","@type":"Researcher","foaf:name":[{"@value":"Mike Jackson"}],"jpcoar:affiliationName":[{"@value":"Institute for Rock Magnetism, Newton Horace Winchell School of Earth Sciences University of Minnesota  USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579818731485184","@type":"Researcher","foaf:name":[{"@value":"Bruce Moskowitz"}],"jpcoar:affiliationName":[{"@value":"Institute for Rock Magnetism, Newton Horace Winchell School of Earth Sciences University of Minnesota  USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2002-04","prism:volume":"29","prism:number":"7","prism:startingPage":"1029"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001GL014197"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL014197"}],"createdAt":"2002-10-27","modifiedAt":"2023-10-31","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050020209660477056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A brief review of single silicate crystal paleointensity: rock-magnetic characteristics, mineralogical backgrounds, methods and applications"}]},{"@id":"https://cir.nii.ac.jp/crid/1050583159613899776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleomagnetic studies on single crystals separated from the middle Cretaceous Iritono granite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229800814336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low‐temperature magnetic properties of pelagic carbonates: Oxidation of biogenic magnetite and identification of magnetosome chains"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489140096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rock magnetic study of fluvial Holocene soil from Buenos Aires province (Argentina)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2001gl014197"},{"@type":"CROSSREF","@value":"10.1002/2013jb010381_references_DOI_H7YkYEbXNLcrci3q3xqbblJTZvC"},{"@type":"CROSSREF","@value":"10.1186/bf03352634_references_DOI_H7YkYEbXNLcrci3q3xqbblJTZvC"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-01994-w_references_DOI_H7YkYEbXNLcrci3q3xqbblJTZvC"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0945-y_references_DOI_H7YkYEbXNLcrci3q3xqbblJTZvC"}]}