When the block matrices are virtually impervious, groundwater may be taken as only flowing through joint networks in rock mass.
当岩块处于近乎隔水状态时，岩体中的渗流可看作为裂隙网络流。
When the block matrices are virtually impervious, groundwater may be taken as only flowing through joint networks in rock mass.
当岩块处于近乎隔水状态时，岩体中的渗流可看作为裂隙网络流。
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