地应力卸荷、风化、流水侵蚀、植物根劈是危岩发育的主要原因。
The developing of dangerous rock is due to release of in-situ stress in rock, aeolation, water erosion and root flerry.
由此产生的应力被压存了数百万年，直到隆起伴随着密西西比的侵蚀导致下面的旧断层松脱释放。
The resulting stress remained stored for millions of years until uplift associated with the Mississippi erosion event led to the unclamping of old faults lying beneath.
耐火材料损坏除了化学侵蚀以外，还有热机械应力。
Thermal and mechanical stress besides chemical corrosion is the main wear mechanism of refractories.
针对氯盐侵蚀的预应力混凝土结构，讨论了氯离子扩散系数的计算。
The calculation of chloride diffusion coefficient in prestressed concrete structures eroded by chloride ion is discussed.
从水力条件出发，研究了应力状态对土体渗透侵蚀起动及破坏水力梯度的影响。
From the hydraulic point of view, the influence of complex stress states on the initiation and development of seepage erosion is investigated.
从水力条件出发，研究了应力状态对土体渗透侵蚀起动及破坏水力梯度的影响。
From the hydraulic point of view, the influence of complex stress states on the initiation and development of seepage erosion is investigated.
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