{"created":"2023-07-25T11:04:04.500603+00:00","id":7100,"links":{},"metadata":{"_buckets":{"deposit":"709c97c2-b788-444b-a29f-b756a4610734"},"_deposit":{"created_by":4,"id":"7100","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7100"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007100","sets":["1259:906:918"]},"author_link":["11040","11036","11041","11037"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ナンキョクカイ カイテイド ノ ユウキシツ ガンリョウ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1961-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"1073","bibliographicPageStart":"1071","bibliographicVolumeNumber":"12","bibliographic_titles":[{"bibliographic_title":"南極資料"}]}]},"item_1_creator_6":{"attribute_name":"著者名(日)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"杉村, 行男"},{"creatorName":"スギムラ, ユキオ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"野口, 喜三雄"},{"creatorName":"ノグチ, キミオ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"SUGIMURA, Yukio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"NOGUCHI, Kimio","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"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":"The samples investigated were collected off Lutzow-Holm Bay in Antarctica by Dr. T. TORII aboard the \"SOYA\", research ship of the 2nd Japanese Antarctic Research Expedition (1957-58). The summary of the results is as follows (See the appendix). (1) Organic carbon in dry sediments ranges between 0.15 and 0.30% and organic nitrogen varies from 0.014 to 0.032%. However, the value of org. N/org.C, 0.05-0.17, does not differ from the corresponding values for bottom sediments from other ocean floors. (2) Chlorophyll derivatives which express an amount of pheophytin equivalent are 4-17 p.p.m. The values are less than the correspending values for the sediments off California, 18-46 p.p.m. (3) Marine humus, as calculated from the value of organic carbon and TRASK'S factor (1.72), varies from 0.3 to 0.5%. The values much differs from the corresponding values for the sediments of the northern Pacific, the southern Pacific and the Atlantic oceans, 1-1.5%, 0.4-1.0% and 0.3-1.5%. (4) Carbonate content shows that the value owes mostly to foraminiferal residues, as CaCO_3 varies from 2 to 11%. The number of the observations so far made is greatly limited. Therefore, the tendencies described above are only approaches to further investigation.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007100","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"国立極地研究所"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00181831","subitem_source_identifier_type":"NCID"}]},"item_1_source_id_20":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00857289","subitem_source_identifier_type":"ISSN"}]},"item_1_subject_21":{"attribute_name":"国際十進分類法","attribute_value_mlt":[{"subitem_subject":"551.46","subitem_subject_scheme":"UDC"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Geochemical Laboratory, Meteorological Research Institute"},{"subitem_text_language":"en","subitem_text_value":"Chemistry Department, Faculty of Science, Tokyo Metropolitan University"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"気象研究所"},{"subitem_text_value":"東京都立大学理学部化学教室"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1961-03-01"}],"displaytype":"detail","filename":"KJ00002476022.pdf","filesize":[{"value":"551.5 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002476022","url":"https://nipr.repo.nii.ac.jp/record/7100/files/KJ00002476022.pdf"},"version_id":"5adf4ea4-e19d-4457-880f-8ad13f6b9f16"}]},"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":"南極海海底土の有機質含量","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"南極海海底土の有機質含量"},{"subitem_title":"CONTENT OF ORGANIC MATTER IN THE BOTTOM SEDIMENTS OFF LUTZOW-HOLM BAY COLLECTED BY THE 2nd JAPANESE ANTARCTIC RESEARCH EXPEDITION","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["918"],"pubdate":{"attribute_name":"公開日","attribute_value":"1961-03-01"},"publish_date":"1961-03-01","publish_status":"0","recid":"7100","relation_version_is_last":true,"title":["南極海海底土の有機質含量"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:57:59.839591+00:00"}