Unsaturated elasto-plastic constitutive equations for compacted kaolin under consolidated drained and shearing-infiltration conditions

Harianto Rahardjo*, Nguyen Cong Thang, Yongmin Kim, Eng Choon Leong

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

9 Citations (Scopus)

Abstract

Transient process of water flow changes the equilibrium conditions of an unsaturated soil, resulting in volume change of a soil. The volume change alters the hydraulic properties of the soil and thus influences the transient process of water flow through the soil. Therefore, the interactive processes between stress-strain behavior and pore-water pressure are the primary processes affecting the mechanical behavior of unsaturated soils. This paper presents coupled elasto-plastic constitutive equations for unsaturated compacted kaolin under consolidated drained and shearing-infiltration conditions. The study focused on the development of the suction increase (SI) yield curve that incorporates changes in matric suction during transient processes. In addition, the relationship of change in specific water volume with respect to net mean stress and matric suction was also proposed by incorporating the hysteresis of soil-water characteristic curve. The simulated results by the proposed constitutive model were compared with those obtained from isotropically consolidated drained tests and shearing infiltration tests of compacted kaolin to verify the proposed model. The simulated results are in close agreement with the experimental results.

Original languageEnglish
Pages (from-to)534-546
Number of pages13
JournalSoils and Foundations
Volume58
Issue number3
DOIs
Publication statusPublished - Jun 2018
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2018

ASJC Scopus Subject Areas

  • Civil and Structural Engineering
  • Geotechnical Engineering and Engineering Geology

Keywords

  • Elasto-plastic constitutive model
  • Hysteresis
  • Matric suction
  • Soil deformation
  • Unsaturated soils
  • Volume change

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