{"created":"2023-05-15T14:43:20.952658+00:00","id":59379,"links":{},"metadata":{"_buckets":{"deposit":"36767f53-6cce-4ada-a9f0-86718c983e30"},"_deposit":{"created_by":1,"id":"59379","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"59379"},"status":"published"},"_oai":{"id":"oai:repo.qst.go.jp:00059379","sets":["10:29"]},"author_link":["591025","591024","591026","591023"],"item_10005_date_7":{"attribute_name":"発表年月日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2002-05-31","subitem_date_issued_type":"Issued"}]},"item_10005_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Using the Th-234 activity in the seawater and settling particle, the POC export flux were estimated inn the western and central equatorial Pacific.  Samples were taken during the MR98-K02, MR99-K07 and MR00-K08 aboard the R. V. Mirai of JAMSTEC.  The total mass fluxes in the central area were 2 times higher than those in the western Pacific. POC export fluxes were estimated from the Th-234 removal flux in seawater and the POC/Th-234 ratio in the settling particle. The high values in the western area compared to the central area were shown.  As the primary productions are different in the effect by ENSO, the variation of POC export fluxes seems to be the effect by composition of particles and plank ton species. ","subitem_description_type":"Abstract"}]},"item_10005_description_6":{"attribute_name":"会議概要（会議名, 開催地, 会期, 主催者等）","attribute_value_mlt":[{"subitem_description":"地球惑星科学関連学会2002年合同大会","subitem_description_type":"Other"}]},"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":"青野, 辰雄"}],"nameIdentifiers":[{"nameIdentifier":"591023","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"山田, 正俊"}],"nameIdentifiers":[{"nameIdentifier":"591024","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"青野 辰雄","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"591025","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"山田 正俊","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"591026","nameIdentifierScheme":"WEKO"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"conference object","resourceuri":"http://purl.org/coar/resource_type/c_c94f"}]},"item_title":"太平洋赤道域におけるTh-234から推定するPOCエクスポートフラックスについて","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"太平洋赤道域におけるTh-234から推定するPOCエクスポートフラックスについて"}]},"item_type_id":"10005","owner":"1","path":["29"],"pubdate":{"attribute_name":"公開日","attribute_value":"2002-08-07"},"publish_date":"2002-08-07","publish_status":"0","recid":"59379","relation_version_is_last":true,"title":["太平洋赤道域におけるTh-234から推定するPOCエクスポートフラックスについて"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-05-15T22:05:35.907535+00:00"}