When rainstorms persist, such soils will start to slide down the slope and be eroded, and furthermore, they rush down and form slurry, thus giving rise to slope mudflow.

 
  • 遇持續暴 雨作用,此種殘坡積土局部發(fā)生啟動(dòng)下滑-流土,進(jìn)而在動(dòng)水壓力作用下下瀉造漿形成坡面 泥石流。
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