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Effect of water content on permanent deformation of fine/coarse soil mixtures with varying coarse grain contents and subjected to multi-stage cyclic loading

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Abstract

An interlayer soil in ancient rail tracks was identified as a mixture of ballast grains and subgrade fines. As the permanent strain \({\varepsilon }_{1}^{p}\) of such mixture was affected by water content, cyclic triaxial tests were performed, under varying water contents of fines wf and coarse grain contents fv. Comparison between present and previous studies showed the significant effect of sample preparation method on \({\varepsilon }_{1}^{p}\). In the present study, a constant fine dry density ρd-f was maintained, leading to an unchanged suction of mixture whatever the fv value. In this case, only the reinforcement effect of fv on \({\varepsilon }_{1}^{p}\) was identified. By contrast, in previous studies, the global dry density of mixture ρd was kept constant, resulting in a decrease in ρd-f with increasing fv and consequently a decrease in suction. In this case, when the negative effect of decreasing suction prevailed on the positive reinforcement effect of increasing fv, the \({\varepsilon }_{1}^{p}\) increased.

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Abbreviations

\({\varepsilon }_{1}\) :

Axial strain

\({\varepsilon }_{1}^{r}\) :

Resilient strain

\({\varepsilon }_{1}^{p}\) :

Permanent strain

\({\varepsilon }_{1}^{p (M)}\) :

Measured permanent strain at loading level M

\({\varepsilon }_{1}^{p (M+1)}\) :

Estimated permanent strain at loading level M + 1

\({\delta \varepsilon }_{1}^{p (M+1)}\) :

Increment of permanent strain at loading level M + 1

f v :

Volumetric coarse grain content

f v-cha :

Characteristic volumetric coarse grain content

N :

Number of loading cycles

ρ d :

Dry density of sample

ρ d -f :

Dry density of fine soil

ρ dmax -f :

Maximum dry density of fine soil

q :

Deviator stress

q max :

Maximum deviator stress

q min :

Minimum deviator stress

Δ q :

Deviator stress amplitude

Δ p :

Mean stress amplitude

S r :

Degree of saturation

w opt-f :

Optimum water content of fine soil

w f :

Water content of fine soil

\({\upsigma }_{3}\) :

Confining pressure

θ :

Increasing slope of permanent strain with loading cycles at the end of loading cycles for a given stress amplitude

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Acknowledgements

This work was supported by the China Scholarship Council (CSC) and Ecole des Ponts ParisTech.

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Correspondence to Yu Su.

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Su, Y., Cui, YJ., Dupla, JC. et al. Effect of water content on permanent deformation of fine/coarse soil mixtures with varying coarse grain contents and subjected to multi-stage cyclic loading. Acta Geotech. 17, 3259–3268 (2022). https://doi.org/10.1007/s11440-021-01445-w

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