{"created":"2024-05-08T06:48:30.098619+00:00","id":2000599,"links":{},"metadata":{"_buckets":{"deposit":"b5f70b4b-5b11-4494-9dd1-541d9e7aeddf"},"_deposit":{"created_by":14,"id":"2000599","owner":"14","owners":[14],"pid":{"revision_id":0,"type":"depid","value":"2000599"},"status":"published"},"_oai":{"id":"oai:kyutech.repo.nii.ac.jp:02000599","sets":["8:24"]},"author_link":["35469"],"control_number":"2000599","item_21_biblio_info_6":{"attribute_name":"bibliographic_information","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2021","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"I_1014","bibliographicPageStart":"I_1009","bibliographicVolumeNumber":"77","bibliographic_titles":[{"bibliographic_title":"土木学会論文集. B1, 水工学","bibliographic_titleLang":"ja"},{"bibliographic_title":"Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering)","bibliographic_titleLang":"en"}]}]},"item_21_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"本研究は，山地源頭部の河床形態の出現特性を調べ，山地の地形的特徴量及び縦断形状との関係を明らかにしたものである．リーチスケールの河床形態の河床勾配は，fall-pool，cascade，step-pool及びpool-riffleの順に大きく，地質間で大きな差異はみられなかった．また，対象河川の縦断形状は直線型と凹型の2つに大別でき，直線型では河床形態の勾配が上下流で変化していないのに対し，凹型では同一の河床形態であっても上流側に勾配が増加する傾向がみられた．源頭部における河床の縦断形状や河床形態の出現特性に影響を及ぼす山地の特性量として，起伏量や開析度に関する指標が選択された．これらは，土砂生産や河床の比高差に関連する指標であることから，河床形態の分布を支配する重要な要因と考えられる．","subitem_description_language":"ja","subitem_description_type":"Abstract"},{"subitem_description":"This study investigates the relationship between distribution characteristics of fluvial morphology and geomorphic characteristics of the headstream area. The gradient of the fluvial morphology at the reach scale is large in the order of fall-pool, cascade, step-pool and pool-riffle. Slope relief and drainage density were selected as mountainous characteristic quantities that affect the longitudinal profile and the distribution characteristics of the fluvial morphology. These indices are considered to be important factors because they are related to sediment production and specific height difference of the stream bed.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_21_link_62":{"attribute_name":"研究者情報","attribute_value_mlt":[{"subitem_link_url":"https://hyokadb02.jimu.kyutech.ac.jp/html/100001703_ja.html"}]},"item_21_publisher_7":{"attribute_name":"出版社","attribute_value_mlt":[{"subitem_publisher":"土木学会"}]},"item_21_relation_12":{"attribute_name":"item_21_relation_12","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.2208/jscejhe.77.2_I_1009","subitem_relation_type_select":"DOI"}}]},"item_21_rights_13":{"attribute_name":"著作権関連情報","attribute_value_mlt":[{"subitem_rights":"Copyright (c) 2021 公益社団法人 土木学会"}]},"item_21_select_59":{"attribute_name":"item_21_select_59","attribute_value_mlt":[{"subitem_select_item":"yes"}]},"item_21_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"2185-467X","subitem_source_identifier_type":"EISSN"}]},"item_21_text_28":{"attribute_name":"論文ID（連携）","attribute_value_mlt":[{"subitem_text_value":"10429493"}]},"item_21_text_63":{"attribute_name":"連携ID","attribute_value_mlt":[{"subitem_text_value":"12019"}]},"item_21_version_type_58":{"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_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorAffiliations":[{"affiliationNames":[{"affiliationNameLang":"ja"}]}],"creatorNames":[{"creatorName":"厳島, 怜","creatorNameLang":"ja"},{"creatorName":"Itsukushima, Rei","creatorNameLang":"en"},{"creatorName":"イツクシマ, レイ","creatorNameLang":"ja-Kana"}],"familyNames":[{"familyName":"厳島","familyNameLang":"ja"},{"familyName":"Itsukushima","familyNameLang":"en"},{"familyName":"イツクシマ","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"怜","givenNameLang":"ja"},{"givenName":"Rei","givenNameLang":"en"},{"givenName":"レイ","givenNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"35469","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"30737656","nameIdentifierScheme":"e-Rad_Researcher","nameIdentifierURI":"https://nrid.nii.ac.jp/ja/nrid/1000030737656"},{"nameIdentifier":"54083114700","nameIdentifierScheme":"Scopus著者ID","nameIdentifierURI":"https://www.scopus.com/authid/detail.uri?authorId=54083114700"},{"nameIdentifier":"0000-0003-2645-6068","nameIdentifierScheme":"ORCiD","nameIdentifierURI":"https://orcid.org/0000-0003-2645-6068"},{"nameIdentifier":"100001703","nameIdentifierScheme":"九工大研究者情報","nameIdentifierURI":"https://hyokadb02.jimu.kyutech.ac.jp/html/100001703_ja.html"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","date":[{"dateType":"Available","dateValue":"2024-05-08"}],"filename":"10429493.pdf","filesize":[{"value":"571 KB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"url":"https://kyutech.repo.nii.ac.jp/record/2000599/files/10429493.pdf"},"version_id":"15aa0435-0c08-4c01-a704-4da0654ac564"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"headstream area","subitem_subject_scheme":"Other"},{"subitem_subject":"fluvial morphology","subitem_subject_scheme":"Other"},{"subitem_subject":"reach scale","subitem_subject_scheme":"Other"},{"subitem_subject":"geomorphic feature of mountains","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"item_resource_type","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"源頭部における河床形態の分布特性と山地の地形的特徴の関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"源頭部における河床形態の分布特性と山地の地形的特徴の関係","subitem_title_language":"ja"},{"subitem_title":"Relationship Between Distribution of Stream Bed Morphology and Geomorphic Feature of Mountains in Headstream Arera","subitem_title_language":"en"}]},"item_type_id":"21","owner":"14","path":["24"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-05-08"},"publish_date":"2024-05-08","publish_status":"0","recid":"2000599","relation_version_is_last":true,"title":["源頭部における河床形態の分布特性と山地の地形的特徴の関係"],"weko_creator_id":"14","weko_shared_id":-1},"updated":"2025-03-12T05:05:43.818363+00:00"}