WEKO3
アイテム
{"_buckets": {"deposit": "3554d74a-d665-4882-83b8-9daeecca4870"}, "_deposit": {"created_by": 4, "id": "3605", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "3605"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00003605", "sets": ["527"]}, "author_link": ["5076", "5073", "5075", "5074"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^\u003c2-\u003e BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1990-01", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "50", "bibliographicPageStart": "43", "bibliographicVolumeNumber": "3", "bibliographic_titles": [{"bibliographic_title": "Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]}, "item_1_creator_7": {"attribute_name": "著者名よみ", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "オサダ, カズオ"}], "nameIdentifiers": [{"nameIdentifier": "5073", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ヒグチ, ケイジ"}], "nameIdentifiers": [{"nameIdentifier": "5074", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "OSADA, Kazuo", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "5075", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "HIGUCHI, Keiji", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "5076", "nameIdentifierScheme": "WEKO"}]}]}, "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": "Transport rates of Na^+, Cl^-, NO_3^- and SO_4^\u003c2-\u003e by drifting snow are estimated to evaluate the contribution to material transport process at Mizuho Station, Antarctica. Daily transport rates of Na^+ and Cl^- by drifting snow in winter are about 3 times as large as their transport rates in summer, whereas daily transport rates of NO_3^- and SO_4^\u003c2-\u003e in winter are two thirds of those in summer. Transport rates of chemical constituents by ice flow are also estimated to compare with the results by drifting snow. Transport rates of chemical constituents by drifting snow comprise between 9% and 18% of the amount transported by ice flow. This result indicates that not only ice flow but also drifting snow has an important role for transport of chemical constituents toward the coastal region. Differences in NO_3^- and SO_4^\u003c2-\u003e concentrations (in μg・l^\u003c-1\u003e) between ice core (56 and 51) and snow drift in summer (315 and 199,respectively) suggest that deposition of snow layer in summer probably does not occur at altitudes from 2000m to 3000m in the katabatic wind region. Annual transport of sulfate by drifting snow across the 2000m contour is estimated to compare with the sulfate amount transported through the whole Antarctic atmosphere estimated by R. J. DELMAS (Nature, 299,677,1982). Amount of sulfate transport (1.4×(10)^6 kg・(yr)^\u003c-1\u003e) by drifting snow toward the coastal region below altitude 2000m is three orders smaller than that through the whole Antarctic atmosphere.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00003605", "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"}]}, "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", "download_preview_message": "", "file_order": 0, "filename": "KJ00000767811.pdf", "filesize": [{"value": "1.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1100000.0, "url": {"label": "KJ00000767811", "url": "https://nipr.repo.nii.ac.jp/record/3605/files/KJ00000767811.pdf"}, "version_id": "932b287a-ed05-48ca-9625-b5ed9cc6fb27"}]}, "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": "TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^\u003c2-\u003e BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^\u003c2-\u003e BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA"}]}, "item_type_id": "1", "owner": "4", "path": ["527"], "permalink_uri": "https://doi.org/10.15094/00003605", "pubdate": {"attribute_name": "公開日", "attribute_value": "1990-01-01"}, "publish_date": "1990-01-01", "publish_status": "0", "recid": "3605", "relation": {}, "relation_version_is_last": true, "title": ["TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^\u003c2-\u003e BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA"], "weko_shared_id": 4}
TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^<2-> BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA
https://doi.org/10.15094/00003605
https://doi.org/10.15094/00003605af234e35-a0a8-4f3c-8068-3883487db581
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000767811 (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1990-01-01 | |||||
タイトル | ||||||
タイトル | TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^<2-> BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003605 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | TRANSPORT RATES OF Na^+, Cl^-, NO_3^- AND SO_4^<2-> BY DRIFTING SNOW AT MIZUHO STATION, ANTARCTICA | |||||
著者名よみ |
オサダ, カズオ
× オサダ, カズオ× ヒグチ, ケイジ |
|||||
著者名(英) |
OSADA, Kazuo
× OSADA, Kazuo× HIGUCHI, Keiji |
|||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Water Research Institute, Nagoya University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Transport rates of Na^+, Cl^-, NO_3^- and SO_4^<2-> by drifting snow are estimated to evaluate the contribution to material transport process at Mizuho Station, Antarctica. Daily transport rates of Na^+ and Cl^- by drifting snow in winter are about 3 times as large as their transport rates in summer, whereas daily transport rates of NO_3^- and SO_4^<2-> in winter are two thirds of those in summer. Transport rates of chemical constituents by ice flow are also estimated to compare with the results by drifting snow. Transport rates of chemical constituents by drifting snow comprise between 9% and 18% of the amount transported by ice flow. This result indicates that not only ice flow but also drifting snow has an important role for transport of chemical constituents toward the coastal region. Differences in NO_3^- and SO_4^<2-> concentrations (in μg・l^<-1>) between ice core (56 and 51) and snow drift in summer (315 and 199,respectively) suggest that deposition of snow layer in summer probably does not occur at altitudes from 2000m to 3000m in the katabatic wind region. Annual transport of sulfate by drifting snow across the 2000m contour is estimated to compare with the sulfate amount transported through the whole Antarctic atmosphere estimated by R. J. DELMAS (Nature, 299,677,1982). Amount of sulfate transport (1.4×(10)^6 kg・(yr)^<-1>) by drifting snow toward the coastal region below altitude 2000m is three orders smaller than that through the whole Antarctic atmosphere. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 3, p. 43-50, 発行日 1990-01 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |