{"created":"2023-07-25T08:07:19.107415+00:00","id":6387,"links":{},"metadata":{"_buckets":{"deposit":"30d00887-5754-40a7-a4eb-7c710f34209a"},"_deposit":{"created_by":18,"id":"6387","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"6387"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00006387","sets":["228:265:5431","43:194:6019"]},"author_link":["91727","2454","8500","91728"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1996-12-26","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"57","bibliographicPageStart":"1","bibliographicVolumeNumber":"24","bibliographic_titles":[{"bibliographic_title":"鹿児島大学農学部演習林研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Research bulletin of the Kagoshima University forests","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1996-12-26","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"鹿児島県垂水市市木字光石5065番地の標高540mのところにある累積性火山灰土壌断面は43土層(厚さ7.8m)よりなり, 36土層は20.000YBP～1914ADの桜島噴出物を母材とする土壌で, 最下層からの5土層は25.000YBPの姶良カルデラ起源, 表層から16,17番目の2土層は6.300YBPの鬼界カルデラからの噴出物とみなされている。この断面は土壌生成論・土壌肥沃論のみならず火山学, 地質・地層学, 地理学, 堆積学等々の諸学問に対して貴重な資料であり, 垂水市と鹿児島大学で永久保存することになっている。本断面43土層を詳細に現地観察した後, これらの土層から採取した土壌試料の物理的, 化学的および叙物学的性質を解明し, さらに, 土壌中の強磁性鉱物の微量元素組成も併せて明らかにした。その結果, この土壌断面は噴出年代の異なる桜島噴出物が14層理, 鬼界カルデラ噴出物1層理, 姶良カルデラ起源3層理より構成されていることが判明した。","subitem_description_language":"ja","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13449362","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN10592752","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"650","subitem_subject_scheme":"NDC"}]},"item_7_subject_20":{"attribute_name":"NIIsubject","attribute_value_mlt":[{"subitem_subject":"林学","subitem_subject_language":"ja","subitem_subject_scheme":"Other"}]},"item_7_version_type_14":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"品川, 昭夫","creatorNameLang":"ja"},{"creatorName":"シナガワ, アキオ","creatorNameLang":"ja-Kana"},{"creatorName":"SHINAGAWA, Akio","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"91727","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"馬田, 英隆","creatorNameLang":"ja"},{"creatorName":"ウマタ, ヒデタカ","creatorNameLang":"ja-Kana"},{"creatorName":"UMATA, Hidetaka","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"2454","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000030041669","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]},{"creatorNames":[{"creatorName":"宮内, 信文","creatorNameLang":"ja"},{"creatorName":"ミヤウチ, ノブフミ","creatorNameLang":"ja-Kana"},{"creatorName":"MIYAUCHI, Nobufumi","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"8500","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000070041621","nameIdentifierScheme":"NRID","nameIdentifierURI":" "}]},{"creatorNames":[{"creatorName":"長友, 由隆","creatorNameLang":"ja"},{"creatorName":"ナガトモ, ヨシタカ","creatorNameLang":"ja-Kana"},{"creatorName":"NAGATOMO, Yoshitaka","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"91728","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-28"}],"displaytype":"detail","filename":"KJ00000206339.pdf","filesize":[{"value":"4.7 MB"}],"format":"application/pdf","mimetype":"application/pdf","url":{"label":"KJ00000206339.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/6387/files/KJ00000206339.pdf"},"version_id":"ff164f9b-7143-4bac-b249-724213a49884"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"累積稽性火山灰土","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"桜島噴出物","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"埋没腐植層","subitem_subject_language":"ja","subitem_subject_scheme":"Other"},{"subitem_subject":"cumulic volcanic ash soils","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"ejecta originated from Volcano Sakurajima","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"buried humic layers","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"垂水市光石に見出される,主として桜島噴出物に由来する累積性火山灰土壌断面について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"垂水市光石に見出される,主として桜島噴出物に由来する累積性火山灰土壌断面について","subitem_title_language":"ja"},{"subitem_title":"Cumulic Volcanic Ash Soil Profile Mainly Originated from Volcano Sakurajima's Ejecta at Hikari-ishi, Tarumizu City.","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["5431","6019"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-04-27"},"publish_date":"2015-04-27","publish_status":"0","recid":"6387","relation_version_is_last":true,"title":["垂水市光石に見出される,主として桜島噴出物に由来する累積性火山灰土壌断面について"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-05-02T07:47:07.455269+00:00"}