{"created":"2024-09-05T06:50:21.803145+00:00","id":2000361,"links":{},"metadata":{"_buckets":{"deposit":"43b8cd1f-415a-4cf3-a98d-c18c56de01f7"},"_deposit":{"created_by":26,"id":"2000361","owner":"26","owners":[26],"pid":{"revision_id":0,"type":"depid","value":"2000361"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:02000361","sets":["1259:1267:1697504001000"]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2023-12-31","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"101006","bibliographicVolumeNumber":"38","bibliographic_titles":[{"bibliographic_title":"Polar Science","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The study focuses on the current state of englacial Lake Dålk (Larsemann Hills Oasis), which was completely devastated in January 2017 by a catastrophic outburst and formed again in February 2020. A set of works including ground-penetrating radar (GPR) profiling, geodetic survey, core drilling, thermometric measurements and isotopic analysis was performed. As a result, new data were obtained about the modern boundaries of the reservoir, ice thickness and depths, as well as about the peculiarities of freezing of the lake after re-formation. Based on the field data obtained, one-dimensional mathematical modeling of Lake Dålk freezing was carried out, the results of which showed further scenarios of its evolution.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_language":"en","subitem_relation_name_text":"10.1016/j.polar.2023.101006"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://doi.org/10.1016/j.polar.2023.101006","subitem_relation_type_select":"DOI"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"18739652","subitem_source_identifier_type":"ISSN"}]},"item_10001_version_type_20":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_be7fb7dd8ff6fe43","subitem_version_type":"NA"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Sukhanova Anastasiia","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Bantsev Dmitry","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Popov Sergey","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Boronina Alina","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Shimanchuk Egor","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Polyakov Sergey","creatorNameLang":"en"}]}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Antarctic lakes","subitem_subject_language":"en"},{"subitem_subject":"Mathematical modeling","subitem_subject_language":"en"},{"subitem_subject":"Ground-penetrating radar","subitem_subject_language":"en"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"The current state of Lake Dålk (Larsemann Hills, East Antarctica)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"The current state of Lake Dålk (Larsemann Hills, East Antarctica)","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"26","path":["1697504001000"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-12-31"},"publish_date":"2023-12-31","publish_status":"0","recid":"2000361","relation_version_is_last":true,"title":["The current state of Lake Dålk (Larsemann Hills, East Antarctica)"],"weko_creator_id":"26","weko_shared_id":-1},"updated":"2024-09-05T06:53:58.228181+00:00"}