{"@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/1361699995401378432.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0377-0273(99)00169-9"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0377027399001699?httpAccept=text/plain"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0377027399001699?httpAccept=text/xml"}},{"identifier":{"@type":"NAID","@value":"30004768942"}},{"identifier":{"@type":"NAID","@value":"10030456950"}}],"dc:title":[{"@value":"D/H and 18 O/ 16 O ratios of water in the crater lake at Kusatsu-Shirane volcano, Japan"}],"description":[{"notation":[{"@value":"Abstract   The D/H and 18O/16O ratios of water in the active crater lake situated on the Kusatsu-Shirane volcano, Japan are about 20 and 6‰, respectively, higher than local meteoric water. The ratios show seasonal variations superimposed on a gradual change over nine years. The isotopic ratios started to increase in early 1990 and decrease in the spring of 1995. The seasonal variation which is high in winter and low in summer correlates with the temperature difference between lake water and ambient air. The large temperature difference in winter enhances the evaporation of lake water and produces the enriched isotopic ratios relative to the ratios in summer. The accumulation of snow and the decrease in the flux of meteoric water into the lake strengthens the winter-time isotopic enrichment. The enriched isotopic ratios of the lake water over a long time result from the addition of an end member with heavy isotopic ratios contained in a thermal fluid supplied to the lake. Considering the water balance in the lake, the isotopic ratios of the thermal fluid were found to be close to the lake water itself, suggesting the circulation of the lake water seeping through lake floor. Based on the correlation between Cl−concentration and the isotopic ratios, the contribution by the heavy end member was estimated to be 25–36% relative to the enrichment by evaporation. The heavy end member could be a liquid phase evolved from a parental fluid, which is a mixture of local meteoric water and a magmatic fluid as found in high-temperature volcanic gases."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580291226204460544","@type":"Researcher","foaf:name":[{"@value":"T. Ohba"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995401378432","@type":"Researcher","foaf:name":[{"@value":"J. Hirabayashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995401378433","@type":"Researcher","foaf:name":[{"@value":"K. Nogami"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03770273"},{"@type":"NCID","@value":"AA0070878X"}],"prism:publicationName":[{"@value":"Journal of Volcanology and Geothermal Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2000-04","prism:volume":"97","prism:number":"1-4","prism:startingPage":"329","prism:endingPage":"346"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0377027399001699?httpAccept=text/plain"},{"@id":"https://api.elsevier.com/content/article/PII:S0377027399001699?httpAccept=text/xml"}],"createdAt":"2002-07-26","modifiedAt":"2019-04-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050021846545474688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Controlled-source electromagnetic survey in a volcanic area: relationship between stacking time and signal-to-noise ratio and comparison with magnetotelluric data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232342644864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Resistivity structure and geochemistry of the Jigokudani Valley hydrothermal system, Mt. 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Motoshirane of Kusatsu-Shirane Volcano, 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/1523388080309678592","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"A photographic method for detailing the morphology of the floor of a dynamic crater lake : the El Chichon case (Chiapas, Mexico)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792011293312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Aeromagnetic survey in Kusatsu-Shirane volcano, central Japan, by using an unmanned helicopter"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0377-0273(99)00169-9"},{"@type":"CIA","@value":"30004768942"},{"@type":"CIA","@value":"10030456950"},{"@type":"OPENAIRE","@value":"doi_dedup___::6bc27b312c590e58edee8afce7424f1c"},{"@type":"CROSSREF","@value":"10.1186/bf03352610_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.3389/feart.2019.00249_references_DOI_JWmCxHBXJtk8LpU06VUxA4kuZvR"},{"@type":"CROSSREF","@value":"10.1186/bf03351737_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2016.06.010_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01466-5_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.741742_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1186/s40623-023-01799-3_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.20965/jdr.2019.p0991_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2022.107600_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1093/gji/ggae431_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaf006_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0060_references_DOI_PWW3wt1MRvf6BUTqnsygo5xJT9Z"}]}