{"created":"2023-07-25T08:05:04.565051+00:00","id":3418,"links":{},"metadata":{"_buckets":{"deposit":"dd74961e-e05e-4116-b858-008b076b82c2"},"_deposit":{"created_by":18,"id":"3418","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"3418"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00003418","sets":["228:262:4604","39:40"]},"author_link":["101666","4768"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-12-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"11","bibliographicPageStart":"1","bibliographicVolumeNumber":"55","bibliographic_titles":[{"bibliographic_title":"鹿児島大学水産学部紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Memoirs of Faculty of Fisheries Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2006-12-25","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"Three-dimensional tidal flow patterns in Kagoshima Bay were calculated using Quoddy3 developed in Dartmouth College. Temperature and salinity were assumed to be uniform and only M2 harmonic component was adopted. The behavior of Lagrange particles scattered on the sea surface was also investigated. The current around the center of Sakurajima Channel increased abruptly and decreased gradually at both flood and ebb tides. \nThe current speed of the bottom layer around the center of Sakurajima Channel was about half that of the surface layer.\nA strong southward residual current appeared along the west coast of the central basin, as well as a weak northward residual current along the east coast. \nThe surface and bottom residual currents were comparatively different at the center of the basin and the locations where the surface residual current was large. \nThe directions and distances traveled by Lagrange particles were seriously affected by slight spatial and temporal differences of the particles, particularly at Sakurajima Channel. \nEven in locations with weak residual current, some of the Lagrange particles traveled long distances.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0453087X","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00040498","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"660","subitem_subject_scheme":"NDC"}]},"item_7_subject_20":{"attribute_name":"NIIsubject","attribute_value_mlt":[{"subitem_subject":"自然科学","subitem_subject_language":"ja","subitem_subject_scheme":"Other"}]},"item_7_version_type_14":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"水野, 孝明","creatorNameLang":"ja"},{"creatorName":"Mizuno, Takaaki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"101666","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"菊川, 浩行","creatorNameLang":"ja"},{"creatorName":"Kikukawa, Hiroyuki","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"4768","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000060041729","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-27"}],"displaytype":"detail","filename":"55-1-mizuno.pdf","filesize":[{"value":"8.9 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"55-1-mizuno.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/3418/files/55-1-mizuno.pdf"},"version_id":"b84f9b72-455b-46bd-9dea-74a46ef53298"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"finite element method","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Quoddy3","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Kagoshima Bay","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"tide","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Lagrange particle","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"3次元有限要素法による鹿児島湾の潮流解析","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"3次元有限要素法による鹿児島湾の潮流解析","subitem_title_language":"ja"},{"subitem_title":"Three Dimensional FEM Analysis of the Tide in Kagoshima Bay","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["40","4604"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-01-21"},"publish_date":"2015-01-21","publish_status":"0","recid":"3418","relation_version_is_last":true,"title":["3次元有限要素法による鹿児島湾の潮流解析"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-07-30T01:14:03.794056+00:00"}