Consideration of microstructure in modelling the hydro-mechanical behaviour of unsaturated soils

The hydro-mechanical behaviour of unsaturated soils is often highly influenced by the microstructure; therefore, it can be beneficial to consider the effect of microstructure in a hydro-mechanical constitutive model. This paper considers the use of a microstructure-related model that adopts the effective degree of saturation as a microstructural index. The model can be used to reproduce the hydro-mechanical behaviour while the effect of the microstructure is considered. For comparison, a non-microstructuredependent model is also employed. The models are applied to simulate the behaviour of two different soilsand a comparison of the models’ performance in simulating triaxial test behaviour is made. Based on the comparison with experimental results and the non-microstructure-dependent model, it can be concluded thatthe adoption of the effective degree of saturation is beneficial to studying the hydro-mechanical behaviour of unsaturated soils affected by the microstructure.

[1]  Yong Wang,et al.  Structural Characteristics of Natural Loess in Northwest China and its Effect on Shear Behavior , 2020, Geotechnical and Geological Engineering.

[2]  D. Jeng,et al.  Pore scale study of the influence of particle geometry on soil permeability , 2019, Advances in Water Resources.

[3]  S. Almahbobi Experimental study of volume change and shear strength behaviour of statically compacted collapsible soil , 2018 .

[4]  S. Mooney,et al.  Bimodal Soil Pore Structure Investigated by a Combined Soil Water Retention Curve and X-Ray Computed Tomography Approach , 2017 .

[5]  Arghya Das,et al.  Evolution of pore size distribution in deforming granular materials , 2017 .

[6]  Simon J. Wheeler,et al.  Formulation of a three‐dimensional constitutive model for unsaturated soils incorporating mechanical–water retention couplings , 2013 .

[7]  Jing-Yuan Wang,et al.  Water characteristic curve of soil with bimodal grain-size distribution , 2013 .

[8]  Yazhou Zou,et al.  A macroscopic model for predicting the relative hydraulic permeability of unsaturated soils , 2012 .

[9]  Gerardo Severino,et al.  Using Bimodal Lognormal Functions to Describe Soil Hydraulic Properties , 2011 .

[10]  Henry Lin,et al.  Quantifying Soil Structure and Preferential Flow in Intact Soil Using X‐ray Computed Tomography , 2008 .

[11]  R. Heck,et al.  X-ray computed tomography of frozen soil , 2008 .

[12]  Paul Simms,et al.  Microstructure Investigation in Unsaturated Soils: A Review with Special Attention to Contribution of Mercury Intrusion Porosimetry and Environmental Scanning Electron Microscopy , 2008 .

[13]  Antonio Gens,et al.  A double structure generalized plasticity model for expansive materials , 2005 .

[14]  J. Locat,et al.  PORE SIZE DISTRIBUTION OF CLAYEY SOILS MEASURED BY MERCURY INTRUSION POROSIMETRY AND ITS RELATION TO HYDRAULIC CONDUCTIVITY , 2003 .

[15]  Simon J. Wheeler,et al.  Coupling of hydraulic hysteresis and stress–strain behaviour in unsaturated soils , 2003 .

[16]  C. Shackelford,et al.  Evaluating dual porosity of pelletized diatomaceous earth using bimodal soil-water characteristic curve functions , 2001 .

[17]  Y. Cui,et al.  Yielding and plastic behaviour of an unsaturated compacted silt , 1996 .

[18]  R. C. Joshi,et al.  Change in pore size distribution due to consolidation of clays , 1989 .

[19]  R. Cesareo,et al.  USING A COMPUTED TOMOGRAPHY MINISCANNER IN SOIL SCIENCE , 1986 .

[20]  M. Singer,et al.  Scanning Electron Microscope Studies of Surface Crusts Formed by Simulated Rainfall , 1984 .

[21]  A. Banin,et al.  SCANNING ELECTRON MICROSCOPE OBSERVATIONS ON SOIL CRUSTS AND THEIR FORMATION , 1980 .

[22]  Y. Cher SCANNING ELECTRON MICROSCOPE (SEM) OBSERVATIONS OF SOIL STRUCTURE CHANGES INDUCED BY SODIUM-CALCIUM EXCHANGE IN RELATION TO HYDRAULIC CONDUCTIVITY , 1975 .