{"created":"2023-07-25T11:00:59.823857+00:00","id":2907,"links":{},"metadata":{"_buckets":{"deposit":"3a1f7a95-a397-4664-af2f-00bfff7e5313"},"_deposit":{"created_by":4,"id":"2907","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2907"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002907","sets":["1259:1260:1262:425:428"]},"author_link":["4061","4059","4057","4063","4062","4060","4064","4058"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"Isotopic mass fractionation of snow due to depth hoar formation"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2000-11","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"7","bibliographicPageStart":"1","bibliographicVolumeNumber":"14","bibliographic_titles":[{"bibliographic_title":"Polar meteorology and glaciology"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ハチクボ, アキヒロ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ハシモト, シゲマサ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ナカオ, マサヨシ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ニシムラ, コウイチ"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Hachikubo, Akihiro","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Hashimoto, Shigemasa","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nakawo, Masayoshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nishimura, Kouichi","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":"To clarify the isotopic changes (δD and δ^<18>O) of snow due to depth hoar formation, large temperature gradients were imposed on snow samples using a closed and insulated box for several days. δD and δ^<18>O increased in the high temperature region where sublimation enriched heavy H_2O, and decreased in the low temperature region where light H_2O was concentrated. Isotope diagrams of the data showed slopes of 2.4-4.9,which indicated that isotopic fractionation on sublimation depends on the kinetic isotope effect. It was also suggested that the transfer coefficient of water vapor in snow increases slightly due to convection; and the changes of isotopic profiles depend primary on the snow density as it affects permeability to vapor diffusion.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002907","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA1129795X","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Kitami Institute of Technology"},{"subitem_text_language":"en","subitem_text_value":"Institute for Hydrospheric-Atmospheric Sciences, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Institute for Hydrospheric-Atmospheric Sciences, Nagoya University"},{"subitem_text_language":"en","subitem_text_value":"Institute of Low Temperature Science, Hokkaido University"}]},"item_1_text_3":{"attribute_name":"記事種別(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Scientific Paper"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2000-11-01"}],"displaytype":"detail","filename":"KJ00002364394.pdf","filesize":[{"value":"757.9 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002364394","url":"https://nipr.repo.nii.ac.jp/record/2907/files/KJ00002364394.pdf"},"version_id":"b8e3ce22-7552-41f0-bc18-fee6994615a9"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Isotopic mass fractionation of snow due to depth hoar formation","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Isotopic mass fractionation of snow due to depth hoar formation"}]},"item_type_id":"1","owner":"4","path":["428"],"pubdate":{"attribute_name":"公開日","attribute_value":"2000-11-01"},"publish_date":"2000-11-01","publish_status":"0","recid":"2907","relation_version_is_last":true,"title":["Isotopic mass fractionation of snow due to depth hoar formation"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:40:53.380465+00:00"}