{"created":"2023-07-25T11:00:49.703124+00:00","id":2738,"links":{},"metadata":{"_buckets":{"deposit":"8a942040-e11e-4c06-82f4-7eeeecd9e0a0"},"_deposit":{"created_by":4,"id":"2738","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2738"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002738","sets":["1259:1260:1265:414:420"]},"author_link":["3006","3005","3008","3001","3002","3003","3004","3007"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"ORIGIN OF DISSOLVED SALTS INFERRED FROM LITHIUM ABUNDANCE IN LAKE AND POND WATERS IN THE ANTARCTIC McMURDO DRY VALLEYS"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1993-09","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"152","bibliographicVolumeNumber":"6","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Antarctic Geosciences"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"タカマツ, ノブキ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"カトウ, ナオユキ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"マツモト, ゲンキ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"トリイ, テツヤ"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"TAKAMATSU, Nobuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"KATO, Naoyuki","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"MATSUMOTO, Genki I.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"TORII, Tetsuya","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":"Lithium and major ionic components in lake, pond and meltstream waters and ice samples in the McMurdo Dry Valleys of southern Victoria Land, Antarctica were determined to elucidate the origin of dissolved salts. The Li concentration of the bottom water in Lake Fryxell (0.13mg/L) was similar to that of seawater (0.178mg/L), but those of Lakes Bonney (5.1-8.8mg/L) and Vanda (27.0mg/L), and Don Juan Pond (390mg/L) were much higher. In contrast, the Li concentrations in the pond waters, glacial meltwaters, pond ice core in the Labyrinth were generally low (less than 88.0μg/L). The enrichment factor for Li [Ef_