The contribution of vegetation to CWRI aggravate slope evolution, accelerate slope losing steady and the occurrences of deep seated landslide.
植被对于CWRI的贡献促进了斜坡演化，加速斜坡失稳和深层滑坡的发生。
The crack of slope rock is growth and link up in various pattern under CWRI and liquid pressure, which cause rock and rock mass developed into loose material and the strength reduced.
CWRI和水压力共同作用下，斜坡岩石裂纹呈现多种模式扩展和贯通，造成岩石和岩体向松散介质转化及强度降低。
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