“…If the fault were filled with extremely low‐ionic‐strength fluid, such as ∼10 −3 M, then the strong EDL force would cause a large repulsive force to act between the particles (solid yellow line in Figure 4b). This strong EDL force is due to the far extension of the EDL around the particle (i.e., long Debye length), and when relative motion occurs between particles in such a state, the interaction between ionic clouds (e.g., overlapping and their distortions) occurs as a stronger viscous resistance force (i.e., the electroviscous effect; Montoro & Francisca, 2019; Rubio‐Hernández et al., 2004) and thus contribute to the suppression of fault sliding. In contrast, where salinity is high, as in the case of the Tohoku‐oki Fault, the interparticle energy is very low (solid red line in Figure 4b), and this may have contributed to a reduction in viscous resistance and thus facilitated fault slip.…”