Seismic waves undergo attenuation in mixed gas and water media, a phenomenon driven by mechanisms such as wave-induced fluid flow between the different fluid phases.
The retrieved papers consistently support the claim that seismic or acoustic waves undergo attenuation when propagating through media containing mixtures of gas and water (such as partially saturated porous media). Papers [4], [5], [7], and [10] explicitly model and confirm wave attenuation and anelasticity in these mixed gas-water environments. There are no papers refuting this principle.