This study investigates the rheological properties of saturated soft clay surrounding a tunnel using the generalized Voigt viscoelastic model. The model incorporates linear semi-permeability boundary conditions to describe the behavior of the clay. Furthermore

two-dimensional rheological consolidation control equations are derived based on the Terzaghi-Rendulic theory

considering the excess pore water pressure as a variable. To solve the equations

conformal transformation and separation of variables methods are employed

resulting in two independent equations representing the excess pore pressure in terms of time and space variables. The Laplace transformation and partial fractional summation method are then utilized to obtain the solution for excess pore pressure dissipation in the time domain. The reliability of the solution is verified by comparing it with the existing four-element Burgers and five-element model

both of which are derived from the generalized Voigt model. Furthermore

the influence of liner permeability

Kelvin body number

independent Newtonian dashpot viscosity coefficient

and tunnel depth on the dissipation and distribution of excess pore pressure is analyzed based on the established solutions. The findings indicate that a higher relative permeability of the liner and soil leads to an earlier onset of excess pore pressure dissipation and a faster dissipation rate. Increasing the number of Kelvin bodies results in slower dissipation rate. Moreover

larger independent viscous coefficients lead to smaller viscous deformation and faster dissipation rates. Additionally

greater tunnel depth prolongs soil percolation path

slowing down the dissipation of excess pore pressure. When the relative permeability coefficient is 0.01

the excess pore pressure gradually decreases with distance from the outer wall of the tunnel. However

when the relative permeability coefficient is 1

the excess pore pressure initially increases and then decreases with distance. As the relative permeability coefficient increases

the influence of the number of Kelvin bodies on the dissipation of super pore pressure diminishes

the variation in super pore pressure dissipation caused by different independent Newtonian dashpot viscosity coefficients gradually decreases

and the role of tunnel liners as new permeable boundaries within the soil layer is becoming increasingly prominent.