“…According to the uniaxial compression and uniaxial creep test results of frozen soft soil specimens in this study, the deformation trend and data were similar at different temperatures corresponding to the same stress level 35 – 38 . For example, at − 5 °C, − 10 °C, and − 15 °C, the final strains at different stress levels were as follows: With a 0.3σ c stress level, the final strains of clay were 2.49%, 2.30%, and 1.69%, respectively, those of silt were 2.60%, 2.09%, and 1.79%, respectively, and those of silty clay is 1.50%, 2.29%, and 2.20%, respectively; With a 0.5σ c stress level, the final strains of clay were 4.58%, 4.39%, and 3.79%, respectively, those of silt were 4.59%, 4.18%, and 3.60%, respectively, and those of silty clay were 3.99%, 4.30%, and 4.48%, respectively; and with a 0.7σ c stress level, the final strains of clay were 6.80%, 6.20% and 5.70%, respectively, those of silt were 6.60%, 6.30%, and 5.40%, respectively, and those of silty clay were 6.00%, 6.60%, and 6.90%, respectively.…”