Using observation data of underground water level proves to be a comparatively reliable method for inversion analysis of seepage parameters for fractured rocks.
利用地下水位的观测资料对岩体渗透参数进行反演是较为可靠的方法。
Using observation data of underground water level proves to be a comparatively reliable method for inversion analysis of seepage parameters for fractured rocks.
利用地下水位的观测资料对岩体渗透参数进行反演是较为可靠的方法。
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