Dynamic response in a transversely isotropic and layered nonlocal poroelastic seabed subjected to vertical P-waves.

A novel model is put forward to characterize the seismic response excited by vertical P-waves in a transversely isotropic and layered nonlocal poroelastic seabed. The proposed model integrates nonlocal parameter, anisotropy, and stratification to accurately examine wave propagation behavior. The fundamental equations for the underlying seabed are formulated using Biot's poroelastodynamic theory and Eringen's nonlocal theory. The wave equation for the overlying water is expressed in terms of the velocity potential. General solutions in both the poroelastic seabed and water layer are derived by solving the involved ordinary differential equations. Employing the newly devised and unconditionally stable propagator matrix scheme, semi-analytical solutions are derived for the time-harmonic response in a layered poroelastic seabed subjected to vertical P-wave excitation within the frequency domain. The validity of the proposed solutions is confirmed through rigorous comparison with the previously established analytical solutions. The influence of key material properties of seabed on the velocities of P-waves and free-field response in the poroelastic seabed is estimated in detail, along with the free-field response in a nonhomogeneous poroelastic seabed. • A semi-analytical dynamic seabed model by vertical P-waves is presented. • 1D rigorous nonlocal Biot theory is proposed. • Dual-variable and position (DVP) method is utilized for solving layered seabed. • Effect of nonlocal parameters and anisotropy on wave propagation is analyzed. • Free-field response in a nonhomogeneous poroelastic seabed is estimated. [ABSTRACT FROM AUTHOR]