Field runoff and underground water worked together in freezing-thawing cycles which produced cavities in granular moraine layers and has reached a phase of balance.
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美
释义
工程条件下,地表水、地下水不会再在场区内冰碛层中形成新的架空块碎石结构,也不会发生渗透破坏,对工程影响微弱。
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