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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
8630782c-7bdb-44f2-b051-3f737906bcf2
名前 / ファイル | ライセンス | アクション | |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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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 |
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著者別名 | ||||||
識別子 | ||||||
識別子 | 161953 | |||||
識別子Scheme | WEKO | |||||
姓名 | ||||||
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 |
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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 |