{"created":"2023-07-25T10:59:29.405938+00:00","id":1176,"links":{},"metadata":{"_buckets":{"deposit":"b24747f7-1c78-465c-96d6-b0363497c5ff"},"_deposit":{"created_by":4,"id":"1176","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"1176"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00001176","sets":["1:356:373"]},"author_link":["897","14639","1345"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1981-10","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"151","bibliographicPageStart":"141","bibliographicVolumeNumber":"19","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Ono, Akira","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Ito, Tomoyuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Iwai, Kunimoto","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":"In order to obtain a better understanding of the character of the aerosol in \"clean\" air, a series of continuous aerosol measurements was carried out at Syowa Station, Antarctica for two consecutive years (February 1977-January 1979) with emphasis on the chemistry of individual aerosols. From the annual and meteorological variations in the concentration and size distribution of size-fractionated aerosols together with the physical and chemical properties of individual aerosols, it is found that the antarctic aerosol is characterized by the presence of newborn sulfuric acid aerosols, and that aged ammonium sulfate aerosols coexist with sea salt aerosols. Some of the implications of the present findings in relation to the origin of the antarctic aerosol are discussed.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","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":"Meteorological Research Institute"},{"subitem_text_language":"en","subitem_text_value":"Department of Earth Science, Faculty of Education, Shinshu University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1981-10-01"}],"displaytype":"detail","filename":"KJ00000011702.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000011702","url":"https://nipr.repo.nii.ac.jp/record/1176/files/KJ00000011702.pdf"},"version_id":"7b6bd20d-0a7e-4aa7-a441-1aabc729a1e9"}]},"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":"A Note on the Origin and Nature of the Antarctic Aerosol","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"A Note on the Origin and Nature of the Antarctic Aerosol","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["373"],"pubdate":{"attribute_name":"公開日","attribute_value":"1981-10-01"},"publish_date":"1981-10-01","publish_status":"0","recid":"1176","relation_version_is_last":true,"title":["A Note on the Origin and Nature of the Antarctic Aerosol"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T14:00:23.433314+00:00"}