{"@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/1361699994256541568.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/jb089ib06p04196"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB06p04196"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB06p04196"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB089iB06p04196"}}],"dc:title":[{"@value":"Effect of humidity on time‐ and velocity‐dependent friction in rocks"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Friction experiments were conducted utilizing samples tested in a humid atmosphere (ambient laboratory humidity or argon bubbled through water) and samples that were carefully dried and tested in an atmosphere of very dry argon (H<jats:sub>2</jats:sub>O<1 ppm). Dry surfaces consistently yield a friction coefficient of 0.85 to 1.00 compared with 0.55 to 0.65 for the tests in a humid environment. Time‐dependent increases in the friction coefficient and large‐scale stick‐slip instability are characteristic of surfaces exposed to atmospheric water, but they are eliminated with careful drying. Direct dependence of frictional strength on slip speed persists under both dry and humid conditions.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994256541696","@type":"Researcher","foaf:name":[{"@value":"James H. Dieterich"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994256541568","@type":"Researcher","foaf:name":[{"@value":"Gerald Conrad"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1984-06-10","prism:volume":"89","prism:number":"B6","prism:startingPage":"4196","prism:endingPage":"4202"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB06p04196"},{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB089iB06p04196"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB089iB06p04196"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004230362546432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous and Aging Dynamics in Single and Stacked Thin Polymer Films"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757867136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional characteristics of single and polycrystalline muscovite and influence of fluid chemistry"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846642763201664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Glass transition dynamics of stacked thin polymer films"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303030144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rate- and State-dependent Friction and its Underlying Physics"},{"@language":"ja","@value":"速度・状態依存摩擦とその物理"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317073908352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Can clay minerals account for the behavior of non-asperity on the subducting plate interface？"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/jb089ib06p04196"},{"@type":"CROSSREF","@value":"10.1007/12_2012_172_references_DOI_GivUyTlr1zaervdcS4wKpCVP9vz"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.519_references_DOI_GivUyTlr1zaervdcS4wKpCVP9vz"},{"@type":"CROSSREF","@value":"10.1002/2015jb012286_references_DOI_GivUyTlr1zaervdcS4wKpCVP9vz"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0063-4_references_DOI_GivUyTlr1zaervdcS4wKpCVP9vz"},{"@type":"CROSSREF","@value":"10.1103/physreve.84.041808_references_DOI_GivUyTlr1zaervdcS4wKpCVP9vz"}]}