{"created":"2021-03-01T06:33:57.409680+00:00","id":28176,"links":{},"metadata":{"_buckets":{"deposit":"9c8e3abd-b120-490a-9e74-4e5c916bbce5"},"_deposit":{"id":"28176","owners":[],"pid":{"revision_id":0,"type":"depid","value":"28176"},"status":"published"},"_oai":{"id":"oai:niigata-u.repo.nii.ac.jp:00028176","sets":["453:456","503:836:1555:1577"]},"item_7_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Soil engineering properties of so-called Alluvial deposits in Niigata Plain"}]},"item_7_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1985-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"96","bibliographicPageStart":"83","bibliographicVolumeNumber":"6","bibliographic_titles":[{"bibliographic_title":"新潟大学積雪地域災害研究センター研究年報"},{"bibliographic_title":"新潟大学積雪地域災害研究センター研究年報","bibliographic_titleLang":"en"}]}]},"item_7_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"In Niigata Plain, so-called Alluvial deposits are well developed and they are subdivided into two formations, namely the Shirone Formation (Late Pleistocene) and the Holocene Higashi-Niigata Formation (Kurotori Formation) in ascending order. Soil engineering properties of these formations are investigated, with special referenced to the relationships between geological age and engineering properties. As a result, some correlations of engineering properties show significant defference (Figs. 13 to 19). Among them, the correlation between liquid limit (w_L) and void ratio (e) have well tendency, and following discriminant is obtained. Z=1.846e -4.048log w_L +4.599 Comparison of the results of subdivision of so-called Alluvial deposits by this discriminant with the results by stratigraphical method shows more than 80% of them corresponded well togather. And the application of this discriminant to database system of ground geology is discussed.","subitem_description_type":"Abstract"}]},"item_7_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"161953","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakagawa, Takao"}]}]},"item_7_publisher_7":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"新潟大学積雪地域災害研究センター"}]},"item_7_select_19":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_7_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00183327","subitem_source_identifier_type":"NCID"}]},"item_7_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03877892","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"仲川, 隆夫"}],"nameIdentifiers":[{"nameIdentifier":"161952","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2019-08-20"}],"displaytype":"detail","filename":"6_83-96.pdf","filesize":[{"value":"855.0 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"6_83-96.pdf","url":"https://niigata-u.repo.nii.ac.jp/record/28176/files/6_83-96.pdf"},"version_id":"1d528174-8d56-4ae2-862d-011ca684c144"}]},"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":"新潟平野における”沖積層”の土質工学的性質について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"新潟平野における”沖積層”の土質工学的性質について"},{"subitem_title":"新潟平野における”沖積層”の土質工学的性質について","subitem_title_language":"en"}]},"item_type_id":"7","owner":"1","path":["456","1577"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-03-04"},"publish_date":"2016-03-04","publish_status":"0","recid":"28176","relation_version_is_last":true,"title":["新潟平野における”沖積層”の土質工学的性質について"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-15T03:58:09.882966+00:00"}