We prove that the quadratic approximation of the capillarity-driven free-boundary Darcy flow, derived in [26], is well posed in Ḣ 3/2 S 1 , and globally well-posed if the initial datum is small in Ḣ 3/2 S 1 .
Presentation of the problemFluid moving in porous media, such as sand or wood, are a common occurrence in nature. The simplest equation describing such physical phenomenon in the Darcy law