High seepage pressure lead to damage zone growth in unfavorable fault zone and even transfixion may be the important reasons which result in bank slope instability.
高渗透压诱发岸坡不利断层带损伤区扩展,甚至贯通可能是导致岸坡失稳的重要原因。
High seepage pressure lead to damage zone growth in unfavorable fault zone and even transfixion may be the important reasons which result in bank slope instability.
高渗透压诱发岸坡不利断层带损伤区扩展,甚至贯通可能是导致岸坡失稳的重要原因。
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