{"created":"2023-07-25T08:07:38.183933+00:00","id":6812,"links":{},"metadata":{"_buckets":{"deposit":"50dedc97-db89-484b-a2c1-9705255ee8e2"},"_deposit":{"created_by":3,"id":"6812","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"6812"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00006812","sets":["228:280:5038"]},"author_link":["68035"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicPageEnd":"27","bibliographicPageStart":"21","bibliographicVolumeNumber":"58","bibliographic_titles":[{"bibliographic_title":"鹿児島大学教育学部研究紀要. 自然科学編"},{"bibliographic_title":"Bulletin of the Faculty of Education, Kagoshima University. Natural science","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2007-03-29"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"鹿児島県志布志砂丘では，台風0416号および0418号の接近に伴う暴漁が原因とみられる地形変化が観察された。本研究では，当地域において，現地踏査，地形漸量，堆積物の観察および粒度分析を行い，海岸砂丘に生じる暴浪時の地形プロセスを考察した。砂丘は一部を除いて，海側から順に，草本に覆われる砂丘Aと海岸林の立地する砂丘Bに区分される。砂丘前面には，遡上波の侵食により平均1．5mの崖が形成された。さらに砂丘に達する越波が発生したためこ，砂丘Aで面状侵食による平坦化と植生破壊が起きた。また，砂丘Aでは木片およびゴミを含む軽石礫が，砂丘Bでは混入物のほとんどない砂が，それぞれ堆積した。後者の主な供給源は，後浜のうち暴浪時以外は風の営力が卓越する範囲と砂丘Aである。砂丘Aまで達する越波は過去に最低でも5回発生しているが，砂丘Bまで達することは比較的少ないと推定される。","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"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03896692","subitem_source_identifier_type":"ISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00408518","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_7_text_24":{"attribute_name":"公開者よみ","attribute_value_mlt":[{"subitem_text_value":"カゴシマ ダイガク"}]},"item_7_text_25":{"attribute_name":"公開者別名","attribute_value_mlt":[{"subitem_text_value":"Kagoshima University"}]},"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":"伊藤, 晶文"}],"nameIdentifiers":[{"nameIdentifier":"68035","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-28"}],"displaytype":"detail","filename":"ito.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ito.pdf","url":"https://ir.kagoshima-u.ac.jp/record/6812/files/ito.pdf"},"version_id":"4856718b-a001-4fa5-9dee-51ac64e49923"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"志布志砂丘","subitem_subject_scheme":"Other"},{"subitem_subject":"越波","subitem_subject_scheme":"Other"},{"subitem_subject":"暴扱","subitem_subject_scheme":"Other"},{"subitem_subject":"台風","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":"鹿児島県志布志砂丘における暴浪時の地形プロセス","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"鹿児島県志布志砂丘における暴浪時の地形プロセス"}]},"item_type_id":"7","owner":"3","path":["42","5038"],"pubdate":{"attribute_name":"公開日","attribute_value":"2015-01-15"},"publish_date":"2015-01-15","publish_status":"0","recid":"6812","relation_version_is_last":true,"title":["鹿児島県志布志砂丘における暴浪時の地形プロセス"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2024-01-30T02:06:24.416262+00:00"}