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  1. I210 減災連携研究センター
  2. I210a 雑誌掲載論文
  3. 学術雑誌

Analysis of the effect of groundwater level on the seismic behavior of an unsaturated embankment on clayey ground

http://hdl.handle.net/2237/24924
http://hdl.handle.net/2237/24924
db18f122-2b90-4867-8c72-188a73d1f20d
名前 / ファイル ライセンス アクション
1-s2_0-S0267726116000476-main.pdf 1-s2_0-S0267726116000476-main.pdf (4.1 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2016-09-29
タイトル
タイトル Analysis of the effect of groundwater level on the seismic behavior of an unsaturated embankment on clayey ground
言語 en
著者 Yoshikawa, Takahiro

× Yoshikawa, Takahiro

WEKO 67013

en Yoshikawa, Takahiro

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Noda, Toshihiro

× Noda, Toshihiro

WEKO 67014

en Noda, Toshihiro

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Kodaka, Takeshi

× Kodaka, Takeshi

WEKO 67015

en Kodaka, Takeshi

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Takaine, Toshihiro

× Takaine, Toshihiro

WEKO 67016

en Takaine, Toshihiro

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 CCBY-NC-ND
キーワード
主題Scheme Other
主題 Soil–water–air coupled analysis
キーワード
主題Scheme Other
主題 Unsaturated soil
キーワード
主題Scheme Other
主題 Groundwater level
キーワード
主題Scheme Other
主題 Elasto-plastic constitutive equation
キーワード
主題Scheme Other
主題 Finite deformation analysis
キーワード
主題Scheme Other
主題 Dynamic/static analysis
キーワード
主題Scheme Other
主題 Clayey soil ground
抄録
内容記述タイプ Abstract
内容記述 Numerous river levees on clayey soil grounds were damaged by the 2011 off the Pacific coast of Tohoku Earthquake. In order to investigate such damage, the behavior of an unsaturated embankment on clayey ground was simulated during its construction, during an earthquake and after the earthquake. The simulation was carried out using a soil–water–air coupled finite deformation analysis code, with attention being focused on the effect of groundwater level. The results indicated that if the groundwater level is high, a saturated area (settlement-induced saturation area) is formed at the base of the embankment due to penetrative settlement during/after construction. In addition, the mean skeleton stress is low compared with the low groundwater level. As a consequence, in the embankment on ground with the high groundwater level, the co-seismic deformation is greater and the mean skeleton stress decreases sharply, particularly in the settlement-induced saturation area during the earthquake. It was also shown that after the earthquake, the groundwater level rises because water flows toward the unsaturated embankment from the settlement-induced saturation area and/or the saturated clayey ground. If the groundwater level is high, in particular, a phreatic line is formed temporarily within the embankment.
言語 en
出版者
出版者 Elsevier
言語 en
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
関連情報
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.soildyn.2016.02.008
ISSN
収録物識別子タイプ PISSN
収録物識別子 0267-7261
書誌情報 Soil Dynamics and Earthquake Engineering

巻 85, p. 217-230, 発行日 2016-06
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/24924
識別子タイプ HDL
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