2000
DOI: 10.1016/s0165-232x(00)00017-3
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Analytical viscoelastic solution for frost force in cold-region tunnels

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Cited by 90 publications
(30 citation statements)
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“…The solutions of the stress and displacement for the unfrozen zone are equal to the superposition of the unloading model solution [25] (Figure 2) and the initial ground stress and displacement. Therefore, according to the thick-walled-cylinder equation [26] and considering the interaction between the frozen wall and the surrounding soil, the stress and displacement solutions for the unfrozen zone can be determined in combination with (3) and (4):…”
Section: Stress and Displacement Solutions For Unfrozen Soil Zonementioning
confidence: 99%
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“…The solutions of the stress and displacement for the unfrozen zone are equal to the superposition of the unloading model solution [25] (Figure 2) and the initial ground stress and displacement. Therefore, according to the thick-walled-cylinder equation [26] and considering the interaction between the frozen wall and the surrounding soil, the stress and displacement solutions for the unfrozen zone can be determined in combination with (3) and (4):…”
Section: Stress and Displacement Solutions For Unfrozen Soil Zonementioning
confidence: 99%
“…According to the assumptions and definite solution conditions in Section 2, it is necessary to ensure that the surrounding soil does not attain the plastic state. At most, (26) satisfies the M-C yield criterion,…”
Section: Stress and Displacement Solutions For Unfrozen Soil Zonementioning
confidence: 99%
“…The first type, which is based on continuum mechanics and the classical heat transfer theory, studies thermal-hydro-mechanical (THM) coupling of rocks under low temperature and the freezing and thawing cycles [25], as well as distribution laws of frost heaving pressure influenced by frost heaving and temperature on tunnel surrounding rocks in cold regions [26,27]. The second type studies basic mechanical properties of rocks under freezing and thawing cycles based on damage mechanics.…”
Section: Introductionmentioning
confidence: 99%
“…So far, most of these models consider that the whole region can be separated into a frozen and an unfrozen zone. The frost heave force resulting from the penetration of the phase front surface that separate these two zones is then estimated from the liquid-to-ice volume change [19,20]. The complexity of these models depends intrinsically on the constitutive behavior of the surrounding rock mass.…”
Section: Introductionmentioning
confidence: 99%