{"@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/1361981471009898240.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0377-0273(81)90016-0"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0377027381900160?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0377027381900160?httpAccept=text/plain"}}],"dc:title":[{"@value":"Evaluation methods of heat discharge and their applications to the major active volcanoes in Japan"}],"description":[{"notation":[{"@value":"Abstract   The rates at which thermal energy is released by non-eruptive mechanisms associated with active volcanoes in Japan have been estimated from surface temperature distributions or from shapes of the fumarolic plume rise. Values of 5.3 x 107 W and 1.2 x 108 W have been calculated for non-eruptive release rates in 100-km segments of the Northeast and the Southwest Japan Arc, respectively. It appears that non-eruptive heat discharge is of the same order as that caused by eruptions."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004057873230215","@type":"Researcher","foaf:name":[{"@value":"T. Kagiyama"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03770273"}],"prism:publicationName":[{"@value":"Journal of Volcanology and Geothermal Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1981-01","prism:volume":"9","prism:number":"1","prism:startingPage":"87","prism:endingPage":"97"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0377027381900160?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0377027381900160?httpAccept=text/plain"}],"createdAt":"2003-08-08","modifiedAt":"2019-03-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050852870543559424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The 2018 phreatic eruption at Mt. Motoshirane of Kusatsu–Shirane volcano, Japan: Eruption and intrusion of hydrothermal fluid observed by a borehole tiltmeter network"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707146762240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal activity within the western-slope geothermal zone of Aso volcano, Japan: Development of a new thermal area"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707319293312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"He, N and C isotopes and fluxes in Aira caldera: Comparative study of hydrothermal activity in Sakurajima volcano and Wakamiko crater, Kyushu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340540818688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heat transport process associated with the 2021 eruption of Aso volcano revealed by thermal and gas monitoring"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511860352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mathematical simulation of magma-hydrothermal activity associated with the 1977 eruption of Usu volcano"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513524608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Heat discharge estimation using satellite remote sensing data on the Iwodake volcano in Satsuma-Iwojima, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712971122816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Kusatsu-Shirane volcano as a site of phreatic eruptions"},{"@language":"ja","@value":"水蒸気噴火発生場としての草津白根火山"},{"@language":"ja-Kana","@value":"スイジョウキ フンカ ハッセイジョウ ト シテ ノ クサツ シロネ カザン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417117557248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quantitative relationship between plume emission and multiple deflations after the 2014 phreatic eruption at Ontake volcano, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/0377-0273(81)90016-0"},{"@type":"OPENAIRE","@value":"doi_dedup___::46c94cd7fc66379f6bc2cdbe2be3652a"},{"@type":"CROSSREF","@value":"10.1186/bf03353020_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01475-4_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1016/j.geothermics.2012.01.003_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1124-5_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2013.04.003_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-01984-y_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.1186/bf03351788_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0060_references_DOI_6JcexcRdXnYGFtPMAwXwsNVadhb"}]}