“…A similar situation pertains with regard to the coupling between fluid flow and solid mechanics. Theoretical and numerical approaches based on Biot's Theory of poroelasticity (Biot, 1941), Terzaghi's effective stress principle (Terzaghi, 1943), and Mixture Theory (Siddique et al., 2017) have been successful at modeling systems with flow in deformable porous media including arteries, biofilms, boreholes, hydrocarbon reservoirs, seismic systems, membranes, soils, swelling clays, and fractures (Auton & MacMinn, 2017; Barry et al., 1997; Jha & Juanes, 2014; Lo et al., 2002, 2005; MacMinn et al., 2016; Mathias et al., 2017; Santillán et al., 2017). However, as mentioned above, we still have very little understanding of how flow‐induced deformation of these solid materials affects the macroscopic flow around them (and thus their boundary conditions) or how fluid‐fluid interfaces behave when pushed against a soft porous medium and vice versa.…”