Consolidation analysis of saturated multi-layered soils with anisotropic permeability caused by a point sink
SUMMARY This paper presents the analytical layer‐element method to analyze the consolidation of saturated multi‐layered soils caused by a point sink by considering the anisotropy of permeability. Starting from the governing equations of the problem, the solutions of displacements and stresses for a...
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Published in | International journal for numerical and analytical methods in geomechanics Vol. 37; no. 7; pp. 758 - 770 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Chichester
Blackwell Publishing Ltd
01.05.2013
Wiley Wiley Subscription Services, Inc |
Subjects | |
Online Access | Get full text |
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Summary: | SUMMARY
This paper presents the analytical layer‐element method to analyze the consolidation of saturated multi‐layered soils caused by a point sink by considering the anisotropy of permeability. Starting from the governing equations of the problem, the solutions of displacements and stresses for a single soil layer are obtained in the Laplace–Hankel transformed domain. Then, the analytical layer‐element method is utilized to further derive the solutions for the saturated multi‐layered soils in the transformed domain by combining with the boundary conditions of the soil system and continuity conditions between adjacent layers. The actual solutions in the physical domain can be acquired by the inversion of Laplace–Hankel transform. Numerical results are carried out to show the accuracy and stability of the proposed method and evaluate the influence of sink depth and anisotropic permeability on excess pore pressure and surface settlement. Copyright © 2011 John Wiley & Sons, Ltd. |
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Bibliography: | National Natural Science Foundation of China - No. 50578121 ArticleID:NAG1126 ark:/67375/WNG-WSGWV9ZS-B istex:8BD1399132AE30BA162D6660BDB147422884BDD6 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0363-9061 1096-9853 |
DOI: | 10.1002/nag.1126 |