{"created":"2021-03-01T06:00:13.315019+00:00","id":7767,"links":{},"metadata":{"_buckets":{"deposit":"25c71bb7-e2e4-453b-9c98-ee745d09f413"},"_deposit":{"id":"7767","owners":[],"pid":{"revision_id":0,"type":"depid","value":"7767"},"status":"published"},"_oai":{"id":"oai:kitami-it.repo.nii.ac.jp:00007767","sets":["1:86"]},"author_link":["39918","39919","39920","39921","39914","44829","39916","39917"],"item_1646810750418":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_3_alternative_title_198":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"PRESSURE PROPAGATION VELOCITY AND PRESSURE ATTENUATION CHARACTERISTIC OF TSUNAMI IN ICE-COVERED RIVER"}]},"item_3_biblio_info_186":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013-06","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"380","bibliographicPageStart":"375","bibliographicVolumeNumber":"19","bibliographic_titles":[{"bibliographic_title":"河川技術論文集","bibliographic_titleLang":"ja"}]}]},"item_3_description_184":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"This study aimed to clarify the pressure propagation velocity and pressure attenuation characteristic\nof tsunami in ice-covered river. We carried out a hydraulics experiment for tsunami in ice-covered river.\nThis research clari ed the following things. The pressure propagation velocity of a  x-ice case is rapid\nas compared with an open-water case and free-ice case. This velocity of free-ice case becomes later than\nopen-water case. In free-ice case, the pressure propagation velocity becomes late when ice-size becomes\nsmaller. The pressure attenuation of a  x-ice case is largest. If ice-size becomes small, pressure will not\nattenuate. When ice-size is small, the dispersion wave train of the same phenomenon as open-water case\nhappens. On the other hand, When ice-size is big, It stops that dispersion wave train happens.","subitem_description_type":"Abstract"}]},"item_3_full_name_183":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"39918","nameIdentifierScheme":"WEKO"}],"names":[{"name":"YOSHIKAWA, Yasuhiro","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"39919","nameIdentifierScheme":"WEKO"}],"names":[{"name":"WATANABE, Yasuharu","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"39920","nameIdentifierScheme":"WEKO"}],"names":[{"name":"ABE, Takaaki","nameLang":"en"}]},{"nameIdentifiers":[{"nameIdentifier":"39921","nameIdentifierScheme":"WEKO"}],"names":[{"name":"OKUBO, Atsushi","nameLang":"en"}]}]},"item_3_publisher_212":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"公益社団法人 土木学会"}]},"item_3_select_195":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"open access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_abf2"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"吉川, 泰弘","creatorNameLang":"ja"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"渡邊, 康玄","creatorNameLang":"ja"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"阿部, 孝章","creatorNameLang":"ja"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"大久保, 敦","creatorNameLang":"ja"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-11-22"}],"displaytype":"detail","filename":"2013-06_河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性.pdf","filesize":[{"value":"3.4 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"2013-06_河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性.pdf","url":"https://kitami-it.repo.nii.ac.jp/record/7767/files/2013-06_河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性.pdf"},"version_id":"74111efb-3ed7-4be5-ab39-f561ff70e457"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Tsunami","subitem_subject_scheme":"Other"},{"subitem_subject":"Ice-covered river","subitem_subject_scheme":"Other"},{"subitem_subject":"Pressure","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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性","subitem_title_language":"ja"},{"subitem_title":"PRESSURE PROPAGATION VELOCITY AND PRESSURE ATTENUATION CHARACTERISTIC OF TSUNAMI IN ICE-COVERED RIVER","subitem_title_language":"en"}]},"item_type_id":"3","owner":"1","path":["86"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-06-10"},"publish_date":"2015-06-10","publish_status":"0","recid":"7767","relation_version_is_last":true,"title":["河川結氷時における河川津波の圧力伝搬速度と圧力減衰特性"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-13T02:21:09.634523+00:00"}