WEKO3
アイテム
{"_buckets": {"deposit": "89eef77f-9468-4a61-a630-9af553be3c99"}, "_deposit": {"created_by": 17, "id": "10094", "owners": [17], "pid": {"revision_id": 0, "type": "depid", "value": "10094"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00010094", "sets": []}, "author_link": ["18719", "18362", "18715", "18722", "18366", "18716", "18721", "18717", "18364", "18720", "18365", "18358", "18360", "18718", "18359", "18723", "18361", "18363"], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2008-12", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "285", "bibliographicPageStart": "277", "bibliographicVolumeNumber": "2", "bibliographic_titles": [{"bibliographic_title": "Polar science"}, {"bibliographic_title": "Polar science", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "To accurately estimate soil organic carbon (SOC) storage in upper alpine to nival zones on the Tibetan Plateau, we inventoried SOC pools in 0-0.3 m profiles along an altitudinal gradient (4400-5300 m asl). We also studied vegetation properties and decomposition activity along the gradient to provide insight into the mechanisms of SOC storage. The vegetation cover and belowground root biomass showed a gradual increased with altitude, reaching a peak in the upper alpine zone at 4800-4950 m before decreasing in the nival zone at 5200-5300 m.Decomposition activity was invariant along the altitudinal gradient except in the nival zone. SOC pools at lower sites were relatively small (2.6 kg C m^\u003c-2\u003e at 4400 m), but increased sharply with altitude, reaching a peak in the upper alpine zone (4950 m; 13.7 kg C m^\u003c-2\u003e) before decreasing (1.0 kg C m^\u003c-2\u003e at 5300 m) with altitude in the nival zone. SOC pool varied greatly within individual alpine meadows by a factor of five or more, as did bulk density, partly due to the effect of grazing. Inventory data for both carbon density and bulk density along altitudinal gradients in alpine ecosystems are of crucial importance in estimating global tundra SOC storage.", "subitem_description_type": "Abstract"}]}, "item_10001_description_6": {"attribute_name": "内容記述", "attribute_value_mlt": [{"subitem_description": "チベット高原の高山帯上部から植生限界(標高4400 m‐5300 m) において、深度30 cmまでの土壌圏有機炭素(SOC)プールの測定を行った。また綿シートを用いて標高傾度に伴う分解活性の差異を検討した。低標高ではSOCプールは小さく(2.6 kg C m-2, 4400 m)、標高が上がるにつれて増加して4950 mで最大(13.7 kg C m-2)となった。分解活性は植生限界である5200-5300 mを除くと、ほとんど変化しなかった。標高のわずかな違いによってSOCプールや仮比重は大きく変動し、高山ツンドラでのSOCプールの推定において標高傾度に伴う調査が重要であることが示唆された。", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "国立極地研究所"}]}, "item_10001_relation_12": {"attribute_name": "論文ID(NAID)", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "110007089159", "subitem_relation_type_select": "NAID"}}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_name": [{"subitem_relation_name_text": "10.1016/j.polar.2008.08.003"}], "subitem_relation_type_id": {"subitem_relation_type_id_text": "http://doi.org/10.1016/j.polar.2008.08.003", "subitem_relation_type_select": "DOI"}}]}, "item_10001_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AA12240481", "subitem_source_identifier_type": "NCID"}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "18739652", "subitem_source_identifier_type": "ISSN"}]}, "item_access_right": {"attribute_name": "アクセス権", "attribute_value_mlt": [{"subitem_access_right": "metadata only access", "subitem_access_right_uri": "http://purl.org/coar/access_right/c_14cb"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Ohtsuka, Toshiyuki"}], "nameIdentifiers": [{"nameIdentifier": "18715", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Hirota, Mitsuru"}], "nameIdentifiers": [{"nameIdentifier": "18716", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Zhang, Xianzhou"}], "nameIdentifiers": [{"nameIdentifier": "18717", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Shimono, Ayako"}], "nameIdentifiers": [{"nameIdentifier": "18718", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Senga, Yukiko"}], "nameIdentifiers": [{"nameIdentifier": "18719", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Du, Minguan"}], "nameIdentifiers": [{"nameIdentifier": "18720", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yonemura, Seiichiro"}], "nameIdentifiers": [{"nameIdentifier": "18721", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kawashima, Shigeto"}], "nameIdentifiers": [{"nameIdentifier": "18722", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tang, Yanhong"}], "nameIdentifiers": [{"nameIdentifier": "18723", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Ohtsuka, Toshiyuki", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18358", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Hirota, Mitsuru", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18359", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Zhang, Xianzhou", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18360", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Shimono, Ayako", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18361", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Senga, Yukiko", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18362", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Du, Minguan", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18363", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yonemura, Seiichiro", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18364", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Kawashima, Shigeto", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18365", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tang, Yanhong", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "18366", "nameIdentifierScheme": "WEKO"}]}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Soil organic carbon", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Alpine ecosystems", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Tibetan Plateau", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Altitudinal gradient", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Soil organic carbon", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Alpine ecosystems", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Tibetan Plateau", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Altitudinal gradient", "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau"}, {"subitem_title": "Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau", "subitem_title_language": "en"}]}, "item_type_id": "10001", "owner": "17", "path": ["1365"], "permalink_uri": "https://nipr.repo.nii.ac.jp/records/10094", "pubdate": {"attribute_name": "公開日", "attribute_value": "2014-10-15"}, "publish_date": "2014-10-15", "publish_status": "0", "recid": "10094", "relation": {}, "relation_version_is_last": true, "title": ["Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau"], "weko_shared_id": -1}
Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau
https://nipr.repo.nii.ac.jp/records/10094
https://nipr.repo.nii.ac.jp/records/1009436f39197-9f64-4eb4-ba2f-3b4b1a06f2c7
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2014-10-15 | |||||
タイトル | ||||||
タイトル | Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Soil organic carbon pools in alpine to nival zones along an altitudinal gradient (4400-5300 m) on the Tibetan Plateau | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Soil organic carbon | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Alpine ecosystems | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Tibetan Plateau | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Altitudinal gradient | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Soil organic carbon | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Alpine ecosystems | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Tibetan Plateau | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Altitudinal gradient | |||||
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 | journal article | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
著者 |
Ohtsuka, Toshiyuki
× Ohtsuka, Toshiyuki× Hirota, Mitsuru× Zhang, Xianzhou× Shimono, Ayako× Senga, Yukiko× Du, Minguan× Yonemura, Seiichiro× Kawashima, Shigeto× Tang, Yanhong× Ohtsuka, Toshiyuki× Hirota, Mitsuru× Zhang, Xianzhou× Shimono, Ayako× Senga, Yukiko× Du, Minguan× Yonemura, Seiichiro× Kawashima, Shigeto× Tang, Yanhong |
|||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | To accurately estimate soil organic carbon (SOC) storage in upper alpine to nival zones on the Tibetan Plateau, we inventoried SOC pools in 0-0.3 m profiles along an altitudinal gradient (4400-5300 m asl). We also studied vegetation properties and decomposition activity along the gradient to provide insight into the mechanisms of SOC storage. The vegetation cover and belowground root biomass showed a gradual increased with altitude, reaching a peak in the upper alpine zone at 4800-4950 m before decreasing in the nival zone at 5200-5300 m.Decomposition activity was invariant along the altitudinal gradient except in the nival zone. SOC pools at lower sites were relatively small (2.6 kg C m^<-2> at 4400 m), but increased sharply with altitude, reaching a peak in the upper alpine zone (4950 m; 13.7 kg C m^<-2>) before decreasing (1.0 kg C m^<-2> at 5300 m) with altitude in the nival zone. SOC pool varied greatly within individual alpine meadows by a factor of five or more, as did bulk density, partly due to the effect of grazing. Inventory data for both carbon density and bulk density along altitudinal gradients in alpine ecosystems are of crucial importance in estimating global tundra SOC storage. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | チベット高原の高山帯上部から植生限界(標高4400 m‐5300 m) において、深度30 cmまでの土壌圏有機炭素(SOC)プールの測定を行った。また綿シートを用いて標高傾度に伴う分解活性の差異を検討した。低標高ではSOCプールは小さく(2.6 kg C m-2, 4400 m)、標高が上がるにつれて増加して4950 mで最大(13.7 kg C m-2)となった。分解活性は植生限界である5200-5300 mを除くと、ほとんど変化しなかった。標高のわずかな違いによってSOCプールや仮比重は大きく変動し、高山ツンドラでのSOCプールの推定において標高傾度に伴う調査が重要であることが示唆された。 | |||||
書誌情報 |
Polar science en : Polar science 巻 2, 号 4, p. 277-285, 発行日 2008-12 |
|||||
出版者 | ||||||
出版者 | 国立極地研究所 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 18739652 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA12240481 | |||||
論文ID(NAID) | ||||||
識別子タイプ | NAID | |||||
関連識別子 | 110007089159 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | http://doi.org/10.1016/j.polar.2008.08.003 | |||||
関連名称 | 10.1016/j.polar.2008.08.003 |