{"created":"2023-07-25T11:01:33.755840+00:00","id":3613,"links":{},"metadata":{"_buckets":{"deposit":"ae7c3e11-41d9-45c9-84d7-adbfd7b74f69"},"_deposit":{"created_by":4,"id":"3613","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"3613"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00003613","sets":["1259:1260:1262:524:527"]},"author_link":["5123","5127","5124","5126","5125","5122"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1990-01","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"101","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"YAMATO, Masahiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"IWASAKA, Yasunobu","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"QIAN, GongWang","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ONO, Akira","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"YAMANOUCHI, Takashi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"NISHIO, Fumihiko","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Aerosol were sampled in the Antarctic marine atmosphere over Breid Bay (70°12′S) from December 1986 to February 1987. According to electron microscope observation of the particles collected on calcium thin film, most particles are sulfuric acid particles. Size distribution of the reaction rings suggests that the particles are rather smaller than that collected inland in Antarctica in summer, although both aerosols are sulfuric acid particles. This suggests that the particle formation, growth and removal processes of particles in Antarctic marine atmosphere differ from those in the inner Antarctic region.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00003613","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA10756213","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Water Research Institute, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"National Institute of Polar Research"},{"subitem_text_language":"en","subitem_text_value":"National Institute of Polar Research"}]},"item_1_text_3":{"attribute_name":"記事種別(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"ABSTRACT"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1990-01-01"}],"displaytype":"detail","filename":"KJ00000767819.pdf","filesize":[{"value":"82.2 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000767819","url":"https://nipr.repo.nii.ac.jp/record/3613/files/KJ00000767819.pdf"},"version_id":"463f12fc-51bf-4c1a-9a54-d52e11812725"}]},"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":"AEROSOL PARTICLES IN THE ANTARCTIC MARINE ATMOSPHERE","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"AEROSOL PARTICLES IN THE ANTARCTIC MARINE ATMOSPHERE"}]},"item_type_id":"1","owner":"4","path":["527"],"pubdate":{"attribute_name":"公開日","attribute_value":"1990-01-01"},"publish_date":"1990-01-01","publish_status":"0","recid":"3613","relation_version_is_last":true,"title":["AEROSOL PARTICLES IN THE ANTARCTIC MARINE ATMOSPHERE"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:31:29.492365+00:00"}