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Elastic visco‐plastic consolidation modelling of clay foundation at Berthierville test embankment
Author(s) -
Zhu Guofu,
Yin JianHua
Publication year - 2000
Publication title -
international journal for numerical and analytical methods in geomechanics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.419
H-Index - 91
eISSN - 1096-9853
pISSN - 0363-9061
DOI - 10.1002/(sici)1096-9853(20000425)24:5<491::aid-nag78>3.0.co;2-v
Subject(s) - geotechnical engineering , consolidation (business) , levee , foundation (evidence) , geology , engineering , accounting , business , archaeology , history
This paper applies for the first time a highly non‐linear One‐Dimensional Elastic Visco‐Plastic (1‐D EVP) model to the consolidation analysis of the clay layer underneath Berthierville test embankment in Quebec, Canada. This paper firstly gives a brief description of the main equations of the Finite Element (FE) consolidation modelling incorporating the 1‐D EVP model. Special issues encountered in the consolidation modelling of the field problem are addressed. Water head fluctuations at the upper and lower boundaries of the clay are considered by giving an appropriate definition of excess porewater pressure. An optimization procedure is suggested for the determination of the 1‐D EVP model parameters. The determination of initial strains in the field is explained. The FE model can consider (a) multi‐layered soil profile, (b) time‐dependent loading and hydraulic boundary conditions and (c) different constitutive models for different soils (1‐D EVP model for clay and Terzaghi's model for silty sand). A parametric FE modelling study is carried out to determine two uncertain parameters of the silty sand layer underlying the clay layer. It is found that the parameter m v affects the compressibility of the silty sand layer, but has no influence on the consolidation behaviour of the clay. However, the parameter k can affect the compression of the silty sand layer and the clay layer. FE consolidation modelling of the soils underneath Berthierville test embankment is carried out using the model parameters determined. It is found that the compression of the clay layer computed from the FE model is in good agreement with field measured values. Porewater pressures from the FE modelling are close to the measured values except for the values at the initial loading stage. This discrepancy at this initial stage is discussed in this paper. Copyright © 2000 John Wiley & Sons, Ltd.