“…Dispersion phenomenon can be observed when Scholte wave propagates on the seabed, its phase velocity varies with the variation of frequency (Spanos, 2009;Kumar and Saini, 2012;Daniel and Marco, 2019;Chen et al, 2023). In recent years, with the development of marine seismic exploration acquisition equipment, especially the application of efficient seabed surface wave acquisition system with the combination of OBS (Ocean Bottom Seismometer) and air gun source, the Scholte surface wave detection is widely used in seabed engineering geological survey, marine oil and gas exploration and so on (Wu et al, 2021;Qi, 1993;Kugler et al, 2007;Zahra et al, 2016;Krylov et al, 2022a;Liang et al, 2022). The thick sedimentary seabed is usually porous and saturated with seawater in the pores between skeletons which are formed by the long-term deposition and accumulation of granular solid minerals.…”