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A monotonic bounding surface critical state model for clays

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Abstract

This study investigates a simple constitutive model based on the critical state framework and bounding surface (BS) plasticity that is suitable for reconstituted clays over a wide range of overconsolidation ratios under monotonic loading. For heavily overconsolidated (OC) clays, rather than using the conventional Hvorslev line, an empirical surface is introduced into the model formulation based on two image points on the BS. The peak strength and the dilatancy of heavily OC clays can thus be predicted satisfactorily. Comparisons with triaxial test data show that the model well captures the peak strength and the dilatancy of heavily OC clays under monotonic loading.

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References

  1. Schofield A, Wroth P (1968) Critical state soil mechanics. McGraw Hill, London

    Google Scholar 

  2. Roscoe KH, Burland J (1968) On the generalized stress-strain behaviour of wet clay. In: Heyman J, Leckie FA (eds) Engineering plasticity. Cambridge University Press, pp 535–609

  3. Dasari G (1996) Modeling of the variation of soil stiffness during sequential construction. Ph.D. Thesis, Cambridge University, UK

  4. Mita KA (2002) Constitutive testing of soil on the dry side of critical state. Ph.D. Thesis, National University of Singapore, Singapore

  5. Prévost JH (1977) Mathematical modelling of monotonic and cyclic undrained clay behaviour. Int J Numer Anal Meth Geomech 1(2):195–216

    Article  MATH  Google Scholar 

  6. Mroz Z, Norris V, Zienkiewicz O (1979) Application of an anisotropic hardening model in the analysis of elasto-plastic deformation of soils. Geotechnique 29(1):1–34

    Article  Google Scholar 

  7. Al-Tabbaa A (1987) Permeability and stress–strain response of speswhite kaolin. Ph.D. Thesis, University of Cambridge, UK

  8. Stallebrass S, Taylor R (1997) The development and evaluation of a constitutive model for the prediction of ground movements in overconsolidated clay. Géotechnique 47(2):235–253

    Article  Google Scholar 

  9. Yin Z-Y, Xu Q, Hicher P-Y (2013) A simple critical-state-based double-yield-surface model for clay behavior under complex loading. Acta Geotech 8(5):509–523

    Article  Google Scholar 

  10. Whittle AJ (1987) A constitutive model for overconsolidated clays with application to the cyclic loading of friction piles. Ph.D. Dissertation, Massachusetts Institute of Technology, USA

  11. Collins IF, Kelly PA (2002) A thermomechanical analysis of a family of soil models. Geotechnique 52(7):507–518

    Article  Google Scholar 

  12. Hvorslev M (1960) Physical components of the shear strength of saturated clays. In: Proceedings of ASCE Research Conference on the Shear Strength of Cohesive Soils. Boulder, Colorado, pp 169–273

  13. Atkinson JH, Bransby PL (1978) The mechanics of soils: an introduction to critical state soil mechanics. McGraw Hill, London

    Google Scholar 

  14. Yao YP, Hou W, Zhou AN (2009) Uh model: three-dimensional unified hardening model for overconsolidated clays. Geotechnique 59(5):451–469

    Article  Google Scholar 

  15. Atkinson J (2007) Peak strength of overconsolidated clays. Géotechnique 57(2):127–135

    Article  Google Scholar 

  16. Yao YP, Gao ZW, Zhao JD, Wan Z (2012) Modified uh model: constitutive modeling of overconsolidated clays based on a parabolic Hvorslev envelope. J Geotech Geoenviron Eng 138(7):860–868

    Article  Google Scholar 

  17. Bryson LS, Salehian A (2011) Performance of constitutive models in predicting behavior of remolded clay. Acta Geotech 6(3):143–154

    Article  Google Scholar 

  18. Potts DM, Zdravkovic L (1999) Finite element analysis in geotechnical engineering: theory, vol 1. Thomas Telford, London

    Book  Google Scholar 

  19. Atkinson J, Richardson D (1987) The effect of local drainage in shear zones on the undrained strength of overconsolidated clay. Geotechnique 37(3):393–403

    Article  Google Scholar 

  20. Pestana JM, Whittle AJ (1999) Formulation of a unified constitutive model for clays and sands. Int J Numer Anal Meth Geomech 23(12):1215–1243

    Article  MATH  Google Scholar 

  21. Yao YP, Wang ND (2014) Transformed stress method for generalizing soil constitutive models. J Eng Mech 140(3):614–629

    Article  Google Scholar 

  22. Zienkiewicz O, Leung K, Pastor M (1985) Simple model for transient soil loading in earthquake analysis. I. Basic model and its application. Int J Numer Anal Meth Geomech 9(5):453–476

    Article  MATH  Google Scholar 

  23. Banerjee P, Stipho A (1978) Associated and non-associated constitutive relations for undrained behaviour of isotropic soft clays. Int J Numer Anal Meth Geomech 2(1):35–56

    Article  Google Scholar 

  24. Banerjee P, Stipho A (1979) An elasto-plastic model for undrained behaviour of heavily overconsolidated clays. Int J Numer Anal Meth Geomech 3(1):97–103

    Article  MATH  Google Scholar 

  25. Nakai T, Hinokio M (2004) A simple elastoplastic model for normally and over consolidated soils with unified material parameters. Soils Found 44(2):53–70

    Article  Google Scholar 

Download references

Acknowledgments

The author would like to thank Professor Chow Yean Khow, Professor Choo Yoo Sang and Dr. Goh Siang Huat of the National University of Singapore for many fruitful discussions on the model and the Lloyd’s Register Foundation (LRF) for the support through the Centre for Offshore Research and Engineering at the National University of Singapore.

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Correspondence to Jinbo Chen.

Appendix

Appendix

Atkinson [15] proposed a criterion for the peak strength of heavily overconsolidated clays as follows:

$$\frac{q}{{Mp^{\prime}}} = 1 + \frac{\beta }{\lambda - \kappa }\xi_{d}$$
(6)

where ξ d is the state parameter measuring the vertical distance between the current stress point A(vp′) and the CSL in the v − ln p′ space. β is the peak strength parameter. From Fig. 6, the following equation holds:

$$\xi_{d} = \varGamma - v_{\kappa } = \lambda \ln \left( {\frac{{p^{\prime}_{cr\_v} }}{{p^{\prime}}}} \right)$$
(7)

where Γ is the intercept of the CSL with the v-axis in the v − ln p′ space. v κ is the intercept of a line, which passes through A(vp′) and parallels with the CSL, with the v-axis in the v − ln p′ space. p cr_v is the mean effective stress on the CSL at the current specific volume v, and is determined through:

$$v = \varGamma - \lambda \ln p^{\prime}_{cr\_v}$$
(8)
Fig. 6
figure 6

Stress state in v − ln p′ space

Substituting Eq. (7) into (6) yields

$$\frac{q}{{Mp^{\prime}}} = 1 + \beta \frac{\lambda }{\lambda - \kappa }\ln \left( {\frac{{p^{\prime}_{cr\_v} }}{{p^{\prime}}}} \right)$$
(9)

v can also be specified through the isotropic normal compression line (NCL) as follows:

$$v = N - \lambda \ln p^{\prime}_{e}$$
(10)

where N is the intercept of the CSL with the v-axis in the v − ln p′ space. p e ′ is the equivalent pressure, the effective pressure on the NCL at v. Combining Eq. (8) with (10) gives

$$\ln p^{\prime}_{cr\_v} = \frac{\varGamma - N}{\lambda } + \ln p^{\prime}_{e}$$
(11)

From Fig. 6, the following equation holds:

$$\kappa \ln \left( {\frac{{p^{\prime}_{c} }}{{p^{\prime}}}} \right) = \lambda \ln \left( {\frac{{p^{\prime}_{c} }}{{p^{\prime}_{e} }}} \right)$$
(12)

Combining Eq. (11) with (12) yields

$$\ln p^{\prime}_{cr\_v} = \frac{\varGamma - N}{\lambda } + \frac{\lambda - \kappa }{\lambda }\ln p^{\prime}_{c} + \frac{\kappa }{\lambda }\ln p^{\prime}$$
(13)

Substituting Eq. (13) into Eq. (9) yields

$$\frac{q}{{Mp^{\prime}}} = 1 + \frac{\beta }{\lambda - \kappa }\left( {\varGamma - N} \right) + \beta \ln \left( {\frac{{p^{\prime}_{c} }}{{p^{\prime}}}} \right)$$
(14)

(Γ − N) can be determined from the relation of the pre-consolidation pressure and the critical state pressure, and is shown as follows:

$$\varGamma - N = \left( {\kappa - \lambda } \right)\ln \frac{{2 + R_{w} }}{2}$$
(15)

Substituting Eq. (15) into Eq. (14) and noticing p cr ′ = 2p′/(2 + R w ) yields Eq. (3) in the main text.

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Chen, J. A monotonic bounding surface critical state model for clays. Acta Geotech. 12, 225–230 (2017). https://doi.org/10.1007/s11440-016-0439-7

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