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dc.contributor.author風間, 卓仁ja
dc.contributor.author山本, 圭吾ja
dc.contributor.author大柳, 諒ja
dc.contributor.author岡田, 和見ja
dc.contributor.author大島, 弘光ja
dc.contributor.author竹中, 悠亮ja
dc.contributor.author若林, 環ja
dc.contributor.author井口, 正人ja
dc.contributor.alternativeKAZAMA, Takahitoen
dc.contributor.alternativeYAMAMOTO, Keigoen
dc.contributor.alternativeOYANAGI, Ryoen
dc.contributor.alternativeOKADA, Kazumien
dc.contributor.alternativeOSHIMA, Hiromitsuen
dc.contributor.alternativeTAKENAKA, Yusukeen
dc.contributor.alternativeWAKABAYASHI, Tamakien
dc.contributor.alternativeIGUCHI, Masatoen
dc.date.accessioned2022-02-26T05:41:23Z-
dc.date.available2022-02-26T05:41:23Z-
dc.date.issued2021-12-
dc.identifier.urihttp://hdl.handle.net/2433/268145-
dc.description.abstractRelative gravity values were repeatedly measured at 19 gravity points in and around Sakurajima Volcano in October 2020 and March 2021, to monitor spatiotemporal mass variations associated with volcanic activity. The gravity values obtained from 1998 to 2021 showed a clear increase of up to +4.3 μGal/yr in the central part of the volcano. The gravity increase was even observed by the LaCoste’s G31 and G375 gravimeters; these gravimeters have been used at Sakurajima Volcano since 1975, and their temporal variations in reading values are negligibly small these days. These facts indicate that the gravity increase observed in the central Sakurajima is the actual one, because the artificial gravity change due to temporal variation of instrumental scale factor is expected to be small for the G31 and G375 gravimeters. The gravity increase can be explained by the point mass increase of 1.9×10¹⁰ kg/yr under the Kita-dake summit at the depth of 3 km below sea level. This result implies that volcanic mass continuously increases under Sakurajima Volcano, even during the quiet period of eruptive activities at the Minami-dake crater.en
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject桜島火山ja
dc.subject相対重力ja
dc.subject質量移動ja
dc.subject地殻変動ja
dc.subject陸水重力擾乱ja
dc.subjectスケール定数ja
dc.subjectSakurajima Volcanoen
dc.subjectrelative gravityen
dc.subjectmass redistributionen
dc.subjectcrustal deformationen
dc.subjecthydrological gravity disturbanceen
dc.subjectscale factoren
dc.subject.ndc519.9-
dc.title桜島火山における繰り返し相対重力測定(2020年10月および2021年3月)ja
dc.title.alternativeRepeated Relative Gravity Measurements in Sakurajima Volcano (October 2020 and March 2021)en
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume64-
dc.identifier.issueB-
dc.identifier.spage73-
dc.identifier.epage85-
dc.textversionpublisher-
dc.sortkey08-
dc.address京都大学大学院理学研究科ja
dc.address京都大学防災研究所ja
dc.address京都大学大学院理学研究科ja
dc.address北海道大学大学院理学研究院ja
dc.address北海道大学大学院理学研究院ja
dc.address京都大学防災研究所ja
dc.address京都大学大学院理学研究科ja
dc.address京都大学防災研究所ja
dc.address.alternativeGraduate School of Science, Kyoto Universityen
dc.address.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.address.alternativeGraduate School of Science, Kyoto Universityen
dc.address.alternativeGraduate School of Science, Hokkaido Universityen
dc.address.alternativeGraduate School of Science, Hokkaido Universityen
dc.address.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.address.alternativeGraduate School of Science, Kyoto Universityen
dc.address.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/publications/nenpo/-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
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