WEKO3
アイテム
{"_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": ["456", "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", "download_preview_message": "", "file_order": 0, "filename": "6_83-96.pdf", "filesize": [{"value": "855.0 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 855000.0, "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"], "permalink_uri": "http://hdl.handle.net/10191/39045", "pubdate": {"attribute_name": "公開日", "attribute_value": "2016-03-04"}, "publish_date": "2016-03-04", "publish_status": "0", "recid": "28176", "relation": {}, "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_shared_id": null}
新潟平野における”沖積層”の土質工学的性質について
http://hdl.handle.net/10191/39045
http://hdl.handle.net/10191/390458630782c-7bdb-44f2-b051-3f737906bcf2
名前 / ファイル | ライセンス | アクション |
---|---|---|
6_83-96.pdf (855.0 kB)
|
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2016-03-04 | |||||
タイトル | ||||||
タイトル | 新潟平野における”沖積層”の土質工学的性質について | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 新潟平野における”沖積層”の土質工学的性質について | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他のタイトル | ||||||
その他のタイトル | Soil engineering properties of so-called Alluvial deposits in Niigata Plain | |||||
著者 |
仲川, 隆夫
× 仲川, 隆夫 |
|||||
著者別名 | ||||||
識別子 | 161953 | |||||
識別子Scheme | WEKO | |||||
姓名 | Nakagawa, Takao | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 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. | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 6, p. 83-96, 発行日 1985-01 |
|||||
出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |