“…We refrai using this term, as it may be misleading for pressures that are smaller th of subglacial materials in a few select scenarios, e.g., when pore-water flow due to porosity change in early stages of shear deformation is limited by low hydraulic diffusivities (e.g., Iverson, 2010). The mechanics of coupled granularfluid mixtures have previously been numerically investigated for studies of fluidized beds (e.g., Anderson and Jackson, 1967;Gidaspow et al, 1992;Hoomans et al, 1996;Xu and Yu, 1997;McNamara et al, 2000;Feng and Yu, 2004;Jajcevic et al, 2013), the stability of inclined, fluid-immersed granular materials (e.g., Topin et al, 2011;Mutabaruka et al, 2014), mechanics during confined deformation (e.g., Goren et al, 2011;Catalano et al, 2014), debris flow (e.g., Hutter et al, 1994;Mangeney et al, 2007;Goren et al, 2011), and for the design of industrial components, e.g., hydrocyclones (e.g., Wang et al, 2007;Zhou et al, 2010), or silos and hoppers (Kloss et al, 2012). In this study, we explore the interaction between the fluid and granular phases in water-saturated consolidated particle assemblages undergoing slow shear deformation.…”