During subduction, metamorphic dehydration reactions in the downgoing slab release fluids, generating fluid overpressure. It has been suggested that fluid is driven to flow upward by buoyancy, but a sufficiently high permeability allowing formation of a fluid percolation network is required. Traditionally, fluid percolation has been identified based on the textural equilibrium assumption by measuring the dihedral angle at the triple junction of grains. According to this theory, grain boundaries generally cannot be infiltrated by fluid, and only the grain edge can form a fluid flow channel. We argue that this theory is insufficient because we have found that water from fluid can be adsorbed into the crystalline interface, that is, a layered mineral interlayer, a crack, or a grain boundary. The high pressure in a subducting slab drives water adsorption into the crystalline interface, forming a low‐dimensional fluidic phase, and thus fluid percolation is achieved. Because water adsorbed in the interface is fluidic, water diffusion drives fluid transport in the subducting slab. Due to water adsorption, fluid overpressure at the dehydration front may release, so that dehydration embrittlement may be excluded. Stable water adsorption in the subduction‐slab conditions is determined here by combining molecular dynamics simulations and thermodynamic calculations. Analysis based on simulations shows that water adsorption requires crystalline surfaces which do not form hydrogen bonds well. Plain Language Summary: Fluids are released during dehydration reactions of hydrous minerals in downgoing slabs. As the density of fluid is smaller than that of rock, buoyancy drives the upward flow of the fluid. However, if fluid domains are isolated rather than well connected in porous rock, this fluid flow may be inhibited. The traditional textural equilibrium theory used to determine whether there is percolation of the fluid network excludes the infiltration of fluid into grain boundaries. However, here, we show that under high pressure, water from fluid can be adsorbed into a crystalline interface, forming a fluidic phase, and thus facilitating fluid percolation. The crystalline interface we study here is the interlayer of layered minerals, but in analogy, the understanding provided in this study can be generalized to other crystalline interfaces, for example, cracks or grain boundaries. If the crystalline surfaces do not form hydrogen bonds well, water adsorption can occur. Fluid migration in a slab is mediated by water within the crystalline interface. Water adsorption into crystalline interface may also play the role of transmitting earthquake‐triggering fluid overpressure, so that brittle failure may be excluded. Stable adsorption of water is identified here with a thermodynamic study based on atomic‐scale simulations. Key Points: Water from fluid can be adsorbed into crystalline interfaces under a high pressure, becoming a fluidic low‐dimensional phaseThis low‐dimensional phase facilitates fluid percolation and migration in a subducting slabWater adsorption into crystalline interface releases fluid overpressure, so that dehydration embrittlement may be excluded [ABSTRACT FROM AUTHOR]