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Experimental and Theoretical Study on Frost Deformation and Damage of Red Sandstones with Different Water Contents

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Abstract

Volumetric expansion of water by 9% in saturated pores and cracks causes substantial frost deformation in rock masses. Frost deformation is an important index reflecting the frost resistance of rocks; however, water saturation has a great influence on the frost deformation characteristics. In this research, the frost strains and acoustic emission activities of red sandstone with different water saturations are monitored under freeze–thaw conditions. The experimental results show that both the peak and the residual frost heaving strains greatly increase for sandstone beyond 85% water saturation. However, there is no significant frost heaving strain that occurs in low-saturation red sandstone (less than 85% water saturation). The acoustic emission activities show the same change trend and further confirm the existence of this critical saturation. In addition, the pore size distribution also has a great influence on the frost heaving strain and freeze–thaw damage. All the liquid pore water in this red sandstone is frozen at − 20 °C because the pores are larger than the critical freezing radius (2.58 nm at − 20 °C) according to the measured pore size distribution. Based on the pore micromechanics and Gibbs–Thomson equation, a developed frost heaving model is proposed considering the effects of water saturation and the pore size distribution. The proposed model can be used to predict the frost heaving strain at any freezing temperature for unsaturated red sandstone. This study thus provides the frost deformation characteristics of red sandstone and contributes to a better understanding of the freeze–thaw damage mechanism of unsaturated sandstone.

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Abbreviations

ρ r, ρ i, ρ l :

Densities of rock matrix, solid ice and water, respectively

UCS:

Uniaxial compressive strength

E r, E i :

Elastic moduli of red sandstone and solid ice, respectively

μ r, μ i :

Poisson’s ratio of red sandstone and solid ice, respectively

n :

Porosity of red sandstone

v r :

P-wave velocity of rock

α r :

Thermal expansion coefficient of rock

\(\ell\) :

Latent heat per unit mass of water

T m :

Freezing point of bulk water

γ il :

Free energy of ice-liquid interfacial

m r1, m r2 :

Masses of the red sandstone sample before and after sticking the strain gauges

m d, m s1 :

Masses of the dry and saturated red sandstone sample, respectively

m t :

Mass of the sandstone sample corresponding to the specific saturation

S r :

Saturation of rock

\(\varepsilon_{{\text{n}}}^{{\text{d}}}\), \(\varepsilon_{{\text{r}}}^{{\text{d}}}\) :

Total nominal strain and the actual strain of dry red sandstone, respectively

\(\varepsilon_{{\text{e}}}\) :

Strain error

T, T 0 :

Current temperature and initial temperature, respectively

\(\alpha_{{\text{n}}}^{{\text{d}}}\) :

Nominal thermal expansion coefficient of red sandstone

\(\alpha_{{\text{r}}}^{{\text{d}}}\) :

Actual thermal expansion coefficient of red sandstone

\({\alpha }_{\mathrm{e}}\) :

Thermal expansion coefficient of the glue and strain gauge

\(\varepsilon_{{\text{p}}}^{{{\text{sa}}}}\) :

Peak frost heaving strain of saturated sandstone

\(\varepsilon_{{{\text{re}}}}^{{{\text{sa}}}}\) :

Residual strain of saturated sandstone

\({a}_{1}\), \({b}_{1}{,a}_{2}\), \({b}_{2}\) :

Unknown frost heaving parameters

\(K_{{\text{r}}}\) :

Bulk modulus of rock

\(\varepsilon_{{\text{T}}}\) :

Linear thermal strain

\(\varepsilon_{{\text{f}}}\) :

Linear frost heaving strain caused by ice pressure

\(b\) :

Biot coefficient

\(p_{{\text{i}}}^{{\text{s}}}\) :

Equivalent pore ice pressure

\(w_{{\text{u}}} (T)\) :

Unfrozen water content

\(F(r)\) :

Cumulative distribution function of the pore size

\(r\) :

Radius of the sphere pore

m 1, m 2 :

Characteristic size of coarse pores and thin pores, respectively

V 1, V 2 :

Volume fractions of the coarse and thin pores, respectively.

\(\xi (S_{{\text{r}}} )\) :

Impact coefficient of water saturation

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Acknowledgements

This work was supported by National Natural Science Foundation of China (Grant nos. 42072300 and 41702291), Natural Science Foundation of Shaanxi Province (Grant no. 2019JQ171).

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Correspondence to Shibing Huang or Yanzhang Liu.

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Huang, S., Cai, Y., Liu, Y. et al. Experimental and Theoretical Study on Frost Deformation and Damage of Red Sandstones with Different Water Contents. Rock Mech Rock Eng 54, 4163–4181 (2021). https://doi.org/10.1007/s00603-021-02509-9

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