{"created":"2021-03-01T06:38:33.987955+00:00","id":30265,"links":{},"metadata":{"_buckets":{"deposit":"bc46582c-7c27-42c4-a8b6-fd3a0c150420"},"_deposit":{"id":"30265","owners":[],"pid":{"revision_id":0,"type":"depid","value":"30265"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00030265","sets":["2113:2449:2450:2510"]},"author_link":["100202","100203","100204","100205"],"item_10_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Rainfall runoff characteristics of the headwaters having a large-scale landslide","subitem_alternative_title_language":"en"}]},"item_10_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2017-04-28","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"120","bibliographicPageStart":"119","bibliographicVolumeNumber":"65","bibliographic_titles":[{"bibliographic_title":"中部森林研究"}]}]},"item_10_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"大規模崩壊地を含む山地流域の降雨流出特性は観測事例が少なく明らかではない。本研究では大規模崩壊地を含む山地流域の流出特性を明らかにするため現地観測を行った。その結果，大規模崩壊から生産された土砂が堆積する区間によりハイドログラフがゆるやかになる傾向がみられた。また，大規模崩壊地付近で発生した士石流が堆積区間で停止する様子が観測された。","subitem_description_language":"ja","subitem_description_type":"Abstract"}]},"item_10_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.18999/chufr.65.119","subitem_identifier_reg_type":"JaLC"}]},"item_10_publisher_32":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"中部森林学会事務局","subitem_publisher_language":"ja"}]},"item_10_select_15":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_10_source_id_61":{"attribute_name":"ISSN（print）","attribute_value_mlt":[{"subitem_source_identifier":"1342-971X","subitem_source_identifier_type":"PISSN"}]},"item_1615787544753":{"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_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":"勝山, 健司","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"100202","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"長田, 知也","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"100203","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"KATSUYAMA, Kenji","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"100204","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"OSADA, Tomoya","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"100205","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":"2020-06-24"}],"displaytype":"detail","filename":"chufr_65_119.pdf","filesize":[{"value":"541.9 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"chufr_65_119.pdf","objectType":"fulltext","url":"https://nagoya.repo.nii.ac.jp/record/30265/files/chufr_65_119.pdf"},"version_id":"9538ddaf-9644-462f-85a6-49d8897a2854"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"降雨流出","subitem_subject_scheme":"Other"},{"subitem_subject":"源流域","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":"大規模崩壊地を含む源流域の降雨流出特性","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"大規模崩壊地を含む源流域の降雨流出特性","subitem_title_language":"ja"}]},"item_type_id":"10","owner":"1","path":["2510"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2020-06-24"},"publish_date":"2020-06-24","publish_status":"0","recid":"30265","relation_version_is_last":true,"title":["大規模崩壊地を含む源流域の降雨流出特性"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-01-16T04:23:40.449857+00:00"}