{"created":"2024-10-03T01:16:08.744728+00:00","id":2010797,"links":{},"metadata":{"_buckets":{"deposit":"ef008bca-d552-4fc9-9991-a37d61687516"},"_deposit":{"created_by":10,"id":"2010797","owners":[10],"pid":{"revision_id":0,"type":"depid","value":"2010797"},"status":"published"},"_oai":{"id":"oai:fra.repo.nii.ac.jp:02010797","sets":["1:8:1724311990269"]},"author_link":["467"],"control_number":"2010797","item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003-08","bibliographicIssueDateType":"Issued"},"bibliographicNumberOfPages":"7","bibliographicPageEnd":"21","bibliographicPageStart":"15","bibliographicVolumeNumber":"8","bibliographic_titles":[{"bibliographic_title":"水産総合研究センター研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of  Fisheries Research Agency","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The distribution of dissolved copper (Cu) was investigated in January (winter) and September (autumn) of 1995 in the central Yellow Sea and found to be influenced by the variation in the components of the water mass. Cu was plotted against the salinity, and the points plotted were classified into three groups corresponding to the characteristics of three types of water masses: the water influenced by the enhanced discharge of the Huanghe and the Changjiang, the Yellow Sea Cold Bottom Water (YSCBW), and the bottom water with high salinity and high temperature originated from the Kuroshio.","subitem_description_language":"en","subitem_description_type":"Abstract"},{"subitem_description":"黄海中央部における銅の分布を1995年 1 月（冬）と9 月（秋）に調査した。黄海は東シナ海に接している縁辺海であるが，その水塊分布は季節により特色が現われ，黄河，長江等の河川流量の季節変動に大きく影響を受けている。銅を塩分に対してプロットすると，冬季は盛んな鉛直混合の影響で，プロット点は塩分32.7付近にかたまる傾向であった。秋季になると河川水流量の増加により表層付近の塩分が低くなり，また25m付近に温度躍層が形成されていた。躍層より上層では冬から秋にかけての塩分の低下とともに，銅濃度の増加が認められ，これは河川水との混合の影響であると考えられる。一方下層では，冬季から残存する水塊（黄海中央冷水），および黒潮に起源をもつ比較的高塩分（32.9以上）の底層水の這い上がりが認められ，銅－塩分プロットでもそれぞれの水塊別に明瞭に区別された。このように黄海における銅の分布は，水塊組成の変動に影響されることが明らかになった。","subitem_description_language":"ja","subitem_description_type":"Abstract"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"水産総合研究センター","subitem_publisher_language":"ja"}]},"item_10002_relation_16":{"attribute_name":"情報源","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"fra_k_8_15","subitem_relation_type_select":"Local"}}]},"item_10002_relation_17":{"attribute_name":"関連サイト","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"日本農学文献記事索引（AgriKnowledge）"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://agriknowledge.affrc.go.jp/RN/2010690835","subitem_relation_type_select":"URI"}}]},"item_10002_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA11589591","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1346-9894","subitem_source_identifier_type":"PISSN"}]},"item_10002_version_type_20":{"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_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":[{"creatorAffiliations":[{"affiliationNameIdentifiers":[],"affiliationNames":[{"affiliationName":"","affiliationNameLang":"ja"}]}],"creatorNames":[{"creatorName":"Abe, Kazuo","creatorNameLang":"en"},{"creatorName":"阿部, 和雄","creatorNameLang":"ja"},{"creatorName":"アベ, カズオ","creatorNameLang":"ja-Kana"}],"familyNames":[{"familyName":"Abe","familyNameLang":"en"},{"familyName":"阿部","familyNameLang":"ja"},{"familyName":"アベ","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"Kazuo","givenNameLang":"en"},{"givenName":"和雄","givenNameLang":"ja"},{"givenName":"カズオ","givenNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"467","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"20372013","nameIdentifierScheme":"e-Rad","nameIdentifierURI":"https://kaken.nii.ac.jp/ja/search/?qm=20372013"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_access","date":[{"dateType":"Available","dateValue":"2024-10-02"}],"filename":"fra_k_8_15.pdf","filesize":[{"value":"165.9 KB"}],"format":"application/pdf","licensetype":"license_0","mimetype":"application/pdf","url":{"url":"https://fra.repo.nii.ac.jp/record/2010797/files/fra_k_8_15.pdf"},"version_id":"89b486cc-d599-41bb-b800-5e7a0c7a6d7c"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Cu distribution; Cu - salinity plot; the Huanghe and the Changjiang; the Yellow Sea","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"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":"黄海における水塊組成と関連した銅の分布","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"黄海における水塊組成と関連した銅の分布","subitem_title_language":"ja"},{"subitem_title":"Copper distribution associated with various water masses in the Yellow Sea","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"10","path":["1724311990269"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2024-10-02"},"publish_date":"2024-10-02","publish_status":"0","recid":"2010797","relation_version_is_last":true,"title":["黄海における水塊組成と関連した銅の分布"],"weko_creator_id":"10","weko_shared_id":-1},"updated":"2025-03-27T04:08:50.225345+00:00"}