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帯水層水頭上昇期の地盤沈下機構について : 新潟平野の地盤沈下を例として
http://hdl.handle.net/10191/39017
http://hdl.handle.net/10191/3901742e4b8fc-38fe-4c72-9f8c-2aa8a5d8fa52
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 | 2016-03-03 | |||||
タイトル | ||||||
タイトル | 帯水層水頭上昇期の地盤沈下機構について : 新潟平野の地盤沈下を例として | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 帯水層水頭上昇期の地盤沈下機構について : 新潟平野の地盤沈下を例として | |||||
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 | A Considevation of mechanism of land subsidence during the rising period of piezomtric head in aquifers | |||||
著者 |
吉田, 昭治
× 吉田, 昭治 |
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著者別名 | ||||||
識別子 | 162067 | |||||
識別子Scheme | WEKO | |||||
姓名 | Yoshida, Shoji | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | During the rising period of piezometric head within the confined aquifers of the multiple aquifer-aquitard system due to the regulations against groundwater withdrawals, land subsidence and delayed uplift of the ground surface have been observed in Niigata plain since about 1965. In order to explain how this phenomena can occur, a discussion of the mechanism of aquifer-aquitard system response to piezometric head changes is presented in this paper by introducing the concept of residual excess porewater pressure and through use of two constant storage coefficients for aquitards. | |||||
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 4, p. 99-106, 発行日 1982-11 |
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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 |