{"created":"2023-07-25T11:04:44.295731+00:00","id":7902,"links":{},"metadata":{"_buckets":{"deposit":"9781bd07-38f6-47af-88c2-828c755c15c7"},"_deposit":{"created_by":4,"id":"7902","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7902"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007902","sets":["1259:906:964"]},"author_link":["13049","11746"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ショウワキチ シュウヘン ノ コショウ ノ スイシツ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1977-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"42","bibliographicPageStart":"32","bibliographicVolumeNumber":"58","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":"日向野, 良治"},{"creatorName":"ヒガノ, リョウジ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"HIGANO, Ryoji","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_11":{"attribute_name":"抄録(日)","attribute_value_mlt":[{"subitem_description":"1967-68,1968-69年の夏季に昭和基地周辺の湖沼について,栄養塩類を中心に調査した結果をまとめた.湖沼水等について,水温,pHの測定,塩素量,溶存酸素,栄養塩,蒸発残留物等を分析し,これら相互間の解析を行った.結果を要約すると次の通りである.1)塩素量では,雪と湖沼水との間には,10-10^3倍の差があり,水分の濃縮は,池に注ぐ前に起こることもありうる.2)塩分と塩素量との間には,海水と類似の関係がみられた.3)栄養塩については,ケイ酸塩とアンモニウム塩以外は極めて低濃度であった.4)塩分濃度,pHなどの関係から,ケイ酸塩は,主として岩石からの溶解による.5)スカーレン地域の湖沼水のリンと窒素の原子数比は1:12で生物の影響がある.6)湖底より発生していた気泡の組成は,酸素を5%多くした大気の組成に等しかった.","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Limnological studies were conducted near Syowa Station during the summers 1967-68, 1968-69. Water temperature, pH, chlorinity, dissolved oxygen, nutrient salts and evaporated residues were determined and correlations among those compounds were studied, obtaining the results as follows. 1) The ratios of chlorinity in snow to that in pond water were 10 to 10^3 and concentration may have occurred before the snow flowed into the pond. 2) Relation between salinity and chlorinity in the lake and pond waters resembled that in the sea water. 3) There were extremely low concentrations of nutrient salts in the lake and pond waters with the exception of silicate and ammonium salt. 4) According to the analytical results of pond water the origin of most silicate in the pond water was ascribed to the erosion of rocks around. 5) The atomic ratio of phosphate-P to inorganic total nitrogen (NO_3^- + NO_2^- + NH_4^+) has 1 : 12 in the pond water collected in the Skallen district, where organic activity was observed on the bottom of the pond. 6) Composition of bubbles sampled from the bottom of a pond was almost the same as that of the air, but it was 5% greater in oxygen and 4% less in nitrogen than that of the air.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007902","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_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Hydrographic Department, Maritime Safety Agency"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"海上保安庁水路部"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1977-03-01"}],"displaytype":"detail","filename":"KJ00002477005.pdf","filesize":[{"value":"4.5 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002477005","url":"https://nipr.repo.nii.ac.jp/record/7902/files/KJ00002477005.pdf"},"version_id":"379e8bf3-170f-4c4f-a358-47f4cc34aa31"}]},"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":"昭和基地周辺の湖沼の水質","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"昭和基地周辺の湖沼の水質"},{"subitem_title":"Chemical Features of the Lake Waters around Syowa Station","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["964"],"pubdate":{"attribute_name":"公開日","attribute_value":"1977-03-01"},"publish_date":"1977-03-01","publish_status":"0","recid":"7902","relation_version_is_last":true,"title":["昭和基地周辺の湖沼の水質"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:51:02.081625+00:00"}