Interactions of Wave and Poro-elastic Seabed under Uniform Current

일정 흐름장에서의 파랑과 다공질 탄성 해저지반의 상호작용

Ocean seabed is usually covered with various types of marine soils. A marine soil is a mixture of two phases: soil particles that forms an interlocking skeletal frame, pore fluids that occupy a major portion of pore space. When gravity water waves propagate over a porous movable seabed, a hydrodynamic pressure on the fluid-seabed interface and fluid flow in the porous medium are induced. (omitted)