海浪近岸时会受到同一的摩擦力效应而分解。
On approaching the shore, waves break because of the same friction effect.
水-岩作用造成的岩土体强度劣化及水力学效应一直被认为是水库岸坡稳定性降低的两个因素。
The deterioration of rock mass strength and the hydraulic effect caused by water-rock interaction have been well known as the two factors that could weaken the stability of reservoir bank.
由于库岸水岩相互作用是一个复杂的地理过程，具有时空动态性，传统方法对库岸的环境效应预测具有一定的难度。
The interaction of water and rock mass in reservoir is a complicated geographic progress with spatial dynamic so it is difficult to predict the environmental effects in bank with traditional ways.
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