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The considerable particle loss rate (13% [100 m]^\u003c-1\u003e) below the mesopelagic layers in a short period suggests the occurrence of consumption processes induced by the sporadic supply of freshly produced particles from above.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00005339", "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": "AA10819561", "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 Biotechnology, Senshu University of Ishinomaki"}, {"subitem_text_language": "en", "subitem_text_value": "Department of Biotechnology, Senshu University of Ishinomaki"}, {"subitem_text_language": "en", "subitem_text_value": "Department of Biotechnology, Senshu University of Ishinomaki"}, {"subitem_text_language": "en", "subitem_text_value": "Institute for Hydrospheric-Atmospheric Sciences, Nagoya University"}, {"subitem_text_language": "en", "subitem_text_value": "Institute for Hydrospheric-Atmospheric Sciences, 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": "Proceeding"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1997-02-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000767682.pdf", "filesize": [{"value": "623.9 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 623900.0, "url": {"label": "KJ00000767682", "url": "https://nipr.repo.nii.ac.jp/record/5339/files/KJ00000767682.pdf"}, "version_id": "27a0a49b-c80a-40a7-b457-777f7f71543a"}]}, "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": "SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology)", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology)"}]}, "item_type_id": "1", "owner": "4", "path": ["646"], "permalink_uri": "https://doi.org/10.15094/00005339", "pubdate": {"attribute_name": "公開日", "attribute_value": "1997-02-01"}, "publish_date": "1997-02-01", "publish_status": "0", "recid": "5339", "relation": {}, "relation_version_is_last": true, "title": ["SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology)"], "weko_shared_id": 4}
SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology)
https://doi.org/10.15094/00005339
https://doi.org/10.15094/0000533966b7c7b4-5daf-498c-9af7-b553df685e4e
名前 / ファイル | ライセンス | アクション |
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KJ00000767682 (623.9 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-02-01 | |||||
タイトル | ||||||
タイトル | SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology) | |||||
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 | 10.15094/00005339 | |||||
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) | |||||
記事種別(英) | ||||||
en | ||||||
Proceeding | ||||||
論文名よみ | ||||||
その他のタイトル | SPORADIC INCREASE OF PARTICLE SEDIMENTATION AT THE ICE EDGE OF THE ANTARCTIC OCEAN DURING THE AUSTRAL SUMMER 1994-1995 (18th Symposium on Polar Biology) | |||||
著者名よみ |
ササキ, ヒロシ
× ササキ, ヒロシ× スズキ, ヒデカツ× タカヤマ, マコト× スズキ, コウジ× ハンダ, ノブヒコ× クドウ, サカエ× フクチ, ミツオ |
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著者名(英) |
SASAKI, Hiroshi
× SASAKI, Hiroshi× SUZUKI, Hidekatsu× TAKAYAMA, Makoto× SUZUKI, Koji× HANDA, Nobuhiko× KUDOH, Sakae× FUKUCHI, Mitsuo |
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著者所属(英) | ||||||
en | ||||||
Department of Biotechnology, Senshu University of Ishinomaki | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Biotechnology, Senshu University of Ishinomaki | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Biotechnology, Senshu University of Ishinomaki | ||||||
著者所属(英) | ||||||
en | ||||||
Institute for Hydrospheric-Atmospheric Sciences, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute for Hydrospheric-Atmospheric Sciences, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Time-series sediment traps were deployed at depths of 537 m, 796 m, 1259 m, 1722 m and 2727 m at ice edge of the Antarctic Ocean (64°42'S, 139°58'E) from 26 December 1994 to 20 January 1995. During a short period from 7 to 9 January, a sporadic flux increase within a few days in terms of total dry weight of 774 mg m^<-2>d^<-1> at 537 m was observed. The mass of sinking particles forming the flux maximum sank down to the deepest trap (2727 m) within 7-11 days, indicating that about 5% of these particles were transported downward to the bottom with the sinking rate of 199-313 m d^<-1> (mean 243 m d^<-1>). The considerable particle loss rate (13% [100 m]^<-1>) below the mesopelagic layers in a short period suggests the occurrence of consumption processes induced by the sporadic supply of freshly produced particles from above. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10819561 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Biology 巻 10, p. 50-55, 発行日 1997-02 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |