{"created":"2023-07-25T11:01:04.540896+00:00","id":2976,"links":{},"metadata":{"_buckets":{"deposit":"77524444-f6ec-4da1-bf68-58adb2440720"},"_deposit":{"created_by":4,"id":"2976","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2976"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002976","sets":["1259:1260:1262:425:432"]},"author_link":["43952","4246","4071","20064","908","65453","65111"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"Chemical characteristics in a 22-m ice core on the Belukha Glacier, Russia"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2004-11","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"120","bibliographicPageStart":"114","bibliographicVolumeNumber":"18","bibliographic_titles":[{"bibliographic_title":"Polar meteorology and glaciology"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Iizuka, Yoshinori","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Fujita, Koji","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Matoba, Sumito","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Fujii, Yoshiyuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Matsuki, Kenichiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Kohno, Mika","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Aizen, Vladimir B.","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":"To better understand how the chemical composition of a glacier in an inland continental region relates to the local climate, we collected ice core samples from the Belukha Glacier, Russia, in July 2001. We analyzed the samples for pH, anions, and cations. The primary soluble ions were SO42-, NO3-, NH4+, Ca2+, and HCOO-. Moreover, we argue the following. 1) Ca2+ and its equivalent SO42-+ NO3- likely originated from terrestrial dust such as soil. 2) HCOO- and its equivalent NH4+ likely originated from vegetation and/or biomass burning. 3) The remaining SO42-+NO3- and NH4+ likely originated from livestock, commercial fertilizers, and natural fertilizers. 4) The NH4+ concentration was low when there was no contribution from vegetation and/or biomass burning.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002976","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":"AA1129795X","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":"Department of General Education, Yuge National College of Maritime Technology/Graduate School of Environmental Studies, Nagoya University/National Institute of Polar Research/National Institute of Polar Research/Graduate School of Environmental Studies, Nagoya University/National Institute of Polar Research/College of Mines and Earth Resources, University of Idaho"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2004-11-01"}],"displaytype":"detail","filename":"KJ00001036823.pdf","filesize":[{"value":"799.1 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00001036823","url":"https://nipr.repo.nii.ac.jp/record/2976/files/KJ00001036823.pdf"},"version_id":"31573145-879c-41db-9844-eabe3d4663d6"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Belukha Glacier","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"inland continental region","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"ice core","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"chemical characteristics","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":"Chemical characteristics in a 22-m ice core on the Belukha Glacier, Russia","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Chemical characteristics in a 22-m ice core on the Belukha Glacier, Russia"}]},"item_type_id":"1","owner":"4","path":["432"],"pubdate":{"attribute_name":"公開日","attribute_value":"2004-11-01"},"publish_date":"2004-11-01","publish_status":"0","recid":"2976","relation_version_is_last":true,"title":["Chemical characteristics in a 22-m ice core on the Belukha Glacier, Russia"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:39:42.793883+00:00"}