{"created":"2023-06-19T11:40:45.642225+00:00","id":992,"links":{},"metadata":{"_buckets":{"deposit":"72be48d5-5a5f-4af6-8997-d530d41cfb45"},"_deposit":{"created_by":14,"id":"992","owners":[14],"pid":{"revision_id":0,"type":"depid","value":"992"},"status":"published"},"_oai":{"id":"oai:setsunan.repo.nii.ac.jp:00000992","sets":["120:133:154:155"]},"author_link":["1754","1751","1750","1753"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2016-10-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"50","bibliographicPageStart":"40","bibliographicVolumeNumber":"2","bibliographic_titles":[{"bibliographic_title":"摂南大学 融合科学研究所論文集"},{"bibliographic_title":"Bulletin of the Transdisciplinary Science Research Institute, Setsunan University","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The purpose of this study is to evaluate the influence of freezing direction on the permeability of freeze-thawed soils. In this study, the permeability of both ice lens (IL) and IL orthogonal directions in the freeze-thawed soil were experimentally investigated. As a result, the permeability of IL direction was greater than IL orthogonal direction. Especially, the permeability of open-system freeze-thawed soils increased remarkably and it received not only the overburden pressure but also the influenced of both condition of pre-consolidation pressure and the number of freeze-thaw cycles. The permeability of closed-system freeze-thawed soils was lower than that of open-system. It was concluded that the permeability of freeze-thawed soil of IL direction is greater because of the remarkably greater void ratio in the colder temperature side of freezing.","subitem_description_type":"Abstract"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"2432-5031","subitem_source_identifier_type":"ISSN"}]},"item_10002_text_24":{"attribute_name":"記事種別","attribute_value_mlt":[{"subitem_text_value":"研究論文"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"廣瀬, 剛"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"伊藤, 譲"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"HIROSE, Go","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"ITO, Yuzuru","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-03-31"}],"displaytype":"detail","filename":"2016_002_01_008_hirose.pdf","filesize":[{"value":"2.0 MB"}],"format":"application/pdf","license_note":"Copyright (c) 2017 by Setsunan University\n","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"飽和細粒土の凍結融解によるアイスレンズ方向の透水係数変化 ―融解後の間隙比分布の影響―　","url":"https://setsunan.repo.nii.ac.jp/record/992/files/2016_002_01_008_hirose.pdf"},"version_id":"1ac942f0-0b49-43f0-8465-6e543b8e710d"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"凍結融解","subitem_subject_scheme":"Other"},{"subitem_subject":"透水係数","subitem_subject_scheme":"Other"},{"subitem_subject":"アイスレンズ","subitem_subject_scheme":"Other"},{"subitem_subject":"飽和細粒土","subitem_subject_scheme":"Other"},{"subitem_subject":"freeze-thaw","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"coefficient of permeability, ice lens, saturated fine-grained soil","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"飽和細粒土の凍結融解によるアイスレンズ方向の透水係数変化 ―融解後の間隙比分布の影響―　","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"飽和細粒土の凍結融解によるアイスレンズ方向の透水係数変化 ―融解後の間隙比分布の影響―　"},{"subitem_title":"Difference of Permeability of Freeze-Thawed Soils by the Directions of Ice Lens  - Influence of Void Ratio Distribution after Thawing -","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"14","path":["155"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-03-31"},"publish_date":"2017-03-31","publish_status":"0","recid":"992","relation_version_is_last":true,"title":["飽和細粒土の凍結融解によるアイスレンズ方向の透水係数変化 ―融解後の間隙比分布の影響―　"],"weko_creator_id":"14","weko_shared_id":-1},"updated":"2023-06-19T12:19:59.125631+00:00"}