Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary

In this paper, based on the axisymmetric consolidation theory of unsaturated soil and equal-strain assumption, an analytical solution using the homogenization of boundary conditions and eigenfunction method is proposed to three-dimensional consolidation of unsaturated soil enhanced by vertical drain...

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Main Authors: QIN Ai-fang, JIANG Liang-hua, XU Wei-fang, MEI Guo-xiong
Format: Article
Language:English
Published: SCIENCE PRESS , 16 DONGHUANGCHENGGEN NORTH ST, BEIJING, PEOPLES R CHINA, 100717 2021-05-01
Series:Rock and Soil Mechanics
Subjects:
Online Access:http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2020.6301
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author QIN Ai-fang
JIANG Liang-hua
XU Wei-fang
MEI Guo-xiong
author_facet QIN Ai-fang
JIANG Liang-hua
XU Wei-fang
MEI Guo-xiong
author_sort QIN Ai-fang
collection DOAJ
description In this paper, based on the axisymmetric consolidation theory of unsaturated soil and equal-strain assumption, an analytical solution using the homogenization of boundary conditions and eigenfunction method is proposed to three-dimensional consolidation of unsaturated soil enhanced by vertical drains under instantaneous loading, in which the continuous permeable boundary conditions are properly introduced. Then, the proposed solution is verified by the special cases of double drainage boundary conditions. Finally, the solution is analyzed using examples and the results show that the proposed solution can be used to simulate the arbitrary distribution of permeability of the top and bottom boundary by setting reasonable interface parameters, which makes up for the problem that the permeability of the top and bottom boundary is between pervious and impervious condition or follows an asymmetric distribution. In addition, with a proper ratio of influence radius to drainage well radius and appropriate depth of vertical drain, the influence of vertical flows on the dissipation of excess pore pressures is small when the ratio of radial to vertical permeability coefficient is greater than two. Last but not the least, the above influence of excess pore pressures is more obvious with the enhancement of the permeability of the top and bottom boundary considering the vertical flows.
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spelling doaj.art-5ed4028c099740d6ac11f0be516b3ac82022-12-22T03:41:28ZengSCIENCE PRESS , 16 DONGHUANGCHENGGEN NORTH ST, BEIJING, PEOPLES R CHINA, 100717Rock and Soil Mechanics1000-75982021-05-014251345135410.16285/j.rsm.2020.6301Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundaryQIN Ai-fang0JIANG Liang-hua1XU Wei-fang2 MEI Guo-xiong3Department of Civil Engineering, Shanghai University, Shanghai 200072, China Department of Civil Engineering, Shanghai University, Shanghai 200072, China Department of Civil Engineering, Shanghai University, Shanghai 200072, China School of Transportation Engineering, Nanjing Tech University, Nanjing, Jiangsu 210029, ChinaIn this paper, based on the axisymmetric consolidation theory of unsaturated soil and equal-strain assumption, an analytical solution using the homogenization of boundary conditions and eigenfunction method is proposed to three-dimensional consolidation of unsaturated soil enhanced by vertical drains under instantaneous loading, in which the continuous permeable boundary conditions are properly introduced. Then, the proposed solution is verified by the special cases of double drainage boundary conditions. Finally, the solution is analyzed using examples and the results show that the proposed solution can be used to simulate the arbitrary distribution of permeability of the top and bottom boundary by setting reasonable interface parameters, which makes up for the problem that the permeability of the top and bottom boundary is between pervious and impervious condition or follows an asymmetric distribution. In addition, with a proper ratio of influence radius to drainage well radius and appropriate depth of vertical drain, the influence of vertical flows on the dissipation of excess pore pressures is small when the ratio of radial to vertical permeability coefficient is greater than two. Last but not the least, the above influence of excess pore pressures is more obvious with the enhancement of the permeability of the top and bottom boundary considering the vertical flows.http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2020.6301unsaturated soilanalytical solutioncontinuous permeable boundarythree-dimensional consolidationvertical drain
spellingShingle QIN Ai-fang
JIANG Liang-hua
XU Wei-fang
MEI Guo-xiong
Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
Rock and Soil Mechanics
unsaturated soil
analytical solution
continuous permeable boundary
three-dimensional consolidation
vertical drain
title Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
title_full Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
title_fullStr Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
title_full_unstemmed Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
title_short Analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
title_sort analytical solution to consolidation of unsaturated soil by vertical drains with continuous permeable boundary
topic unsaturated soil
analytical solution
continuous permeable boundary
three-dimensional consolidation
vertical drain
url http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2020.6301
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AT jianglianghua analyticalsolutiontoconsolidationofunsaturatedsoilbyverticaldrainswithcontinuouspermeableboundary
AT xuweifang analyticalsolutiontoconsolidationofunsaturatedsoilbyverticaldrainswithcontinuouspermeableboundary
AT meiguoxiong analyticalsolutiontoconsolidationofunsaturatedsoilbyverticaldrainswithcontinuouspermeableboundary