“…During the loading and unloading of the cyclic train loads, the volume of the void area created between sleeper and trackbed changes sharply, which results in suction in the void area and causes fine particles to migrate upward to the surface of ballast layer, thereby forming mud pumping [13,34]. For ballastless track, the existing studies have shown that mud pumping is the phenomenon of fine particle migration driven by excess pore-water pressure (PWP) generated by moving train loads on saturated roadbed [3,4,15,16,18,20,25,26,[37][38][39][40]. However, the channel of rainwater intruding into the roadbed, the distribution conditions of the intrusion rainwater, and the migration mechanism of fine particles all remain unclear.…”