Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water

In order to better explain the phenomenon of foundation pit inrush caused by confined water, the Hansbo non-Darcy seepage theory was introduced into the Terzaghi one-dimensional saturated soil consolidation equation. Finite difference methods were applied to the numerical solution of excess pore pre...

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Autores principales: YING Hongwei, XU Dingye, WANG Di, ZHANG Lisha
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Publicado: Editorial Office of Journal of Shanghai Jiao Tong University 2020
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spelling oai:doaj.org-article:36188c87a6c74fae8687d0f49c38e6232021-11-04T09:34:51ZAnalysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water1006-246710.16183/j.cnki.jsjtu.2019.036https://doaj.org/article/36188c87a6c74fae8687d0f49c38e6232020-12-01T00:00:00Zhttp://xuebao.sjtu.edu.cn/CN/10.16183/j.cnki.jsjtu.2019.036https://doaj.org/toc/1006-2467In order to better explain the phenomenon of foundation pit inrush caused by confined water, the Hansbo non-Darcy seepage theory was introduced into the Terzaghi one-dimensional saturated soil consolidation equation. Finite difference methods were applied to the numerical solution of excess pore pressure caused by the fluctuation of confined water. Then, the numerical solution was reduced to Darcy seepage and compared with the analytical solution. The effects of non-Darcy parameters, fluctuation periods of confined water, and initial water levels on the variation of excess pore pressure in the aquitard were analyzed. The results show that the excess pore pressure in aquitard volatility increases over time under the fluctuation of confined water, and reaches a stable fluctuating state after several cycles. The greater the initial hydraulic gradient and test constant of non-Darcy, the more obvious the hysteresis phenomenon of excess pore pressure, and the smaller the amplitude. The longer period of pressure water fluctuation or the higher the initial water level, the greater the amplitude of excess pore pressure oscillation. In addition, when the base is subjected to higher levels of initial confined water, the excess pore pressure in aquitard becomes more susceptible to the change of confined water pressure. The application of a case indicates that the designed drawdown depth of the confined water level could be reduced if the non-Darcy factor is considered.YING HongweiXU DingyeWANG DiZHANG LishaEditorial Office of Journal of Shanghai Jiao Tong Universityarticlenon-darcy flowfoundation pitexcess pore pressure responseaquitardexit gradientEngineering (General). Civil engineering (General)TA1-2040Chemical engineeringTP155-156Naval architecture. Shipbuilding. Marine engineeringVM1-989ZHShanghai Jiaotong Daxue xuebao, Vol 54, Iss 12, Pp 1300-1306 (2020)
institution DOAJ
collection DOAJ
language ZH
topic non-darcy flow
foundation pit
excess pore pressure response
aquitard
exit gradient
Engineering (General). Civil engineering (General)
TA1-2040
Chemical engineering
TP155-156
Naval architecture. Shipbuilding. Marine engineering
VM1-989
spellingShingle non-darcy flow
foundation pit
excess pore pressure response
aquitard
exit gradient
Engineering (General). Civil engineering (General)
TA1-2040
Chemical engineering
TP155-156
Naval architecture. Shipbuilding. Marine engineering
VM1-989
YING Hongwei
XU Dingye
WANG Di
ZHANG Lisha
Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
description In order to better explain the phenomenon of foundation pit inrush caused by confined water, the Hansbo non-Darcy seepage theory was introduced into the Terzaghi one-dimensional saturated soil consolidation equation. Finite difference methods were applied to the numerical solution of excess pore pressure caused by the fluctuation of confined water. Then, the numerical solution was reduced to Darcy seepage and compared with the analytical solution. The effects of non-Darcy parameters, fluctuation periods of confined water, and initial water levels on the variation of excess pore pressure in the aquitard were analyzed. The results show that the excess pore pressure in aquitard volatility increases over time under the fluctuation of confined water, and reaches a stable fluctuating state after several cycles. The greater the initial hydraulic gradient and test constant of non-Darcy, the more obvious the hysteresis phenomenon of excess pore pressure, and the smaller the amplitude. The longer period of pressure water fluctuation or the higher the initial water level, the greater the amplitude of excess pore pressure oscillation. In addition, when the base is subjected to higher levels of initial confined water, the excess pore pressure in aquitard becomes more susceptible to the change of confined water pressure. The application of a case indicates that the designed drawdown depth of the confined water level could be reduced if the non-Darcy factor is considered.
format article
author YING Hongwei
XU Dingye
WANG Di
ZHANG Lisha
author_facet YING Hongwei
XU Dingye
WANG Di
ZHANG Lisha
author_sort YING Hongwei
title Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
title_short Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
title_full Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
title_fullStr Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
title_full_unstemmed Analysis of Non-Darcy Flow in Aquitard at Bottom of Foundation Pit Under Fluctuation of Confined Water
title_sort analysis of non-darcy flow in aquitard at bottom of foundation pit under fluctuation of confined water
publisher Editorial Office of Journal of Shanghai Jiao Tong University
publishDate 2020
url https://doaj.org/article/36188c87a6c74fae8687d0f49c38e623
work_keys_str_mv AT yinghongwei analysisofnondarcyflowinaquitardatbottomoffoundationpitunderfluctuationofconfinedwater
AT xudingye analysisofnondarcyflowinaquitardatbottomoffoundationpitunderfluctuationofconfinedwater
AT wangdi analysisofnondarcyflowinaquitardatbottomoffoundationpitunderfluctuationofconfinedwater
AT zhanglisha analysisofnondarcyflowinaquitardatbottomoffoundationpitunderfluctuationofconfinedwater
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