Wave propagation through a saturated frozen soil layer sandwiched by two elastic soil half-spaces is investigated in this paper. The saturated frozen soil layer in the middle consists of a saturated three-phase medium of solid, liquid and ice, which is considered isotropic. Due to the presence of the three-phase medium, three types of longitudinal waves and two types of shear waves exist in saturated frozen soil. The concept of state vector is introduced. The state transition differential equation is derived based on the reduction of order of the motion equations, and the state transfer matrix is obtained by solving the state transition differential equation. By introducing the interface conditions between saturated frozen soil and elastic soil, the state transition matrix is simplified, and redundant state vectors are eliminated to establish the relationship between the incident wave, reflection wave and transmission wave. Two cases (incident P wave and incident SV wave) are considered, and the reflection and transmission amplitude ratios varying with the incident angle are calculated. The results indicate that the incident wave frequency, porosity, saturation and cementation parameters have a substantial influence on the reflection and transmission. This study provides a new research perspective for controlling the propagation of elastic waves in saturated frozen soils.
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