Groundwater runoff is the subsurface flow which flows from highhydraulic head to low hydraulic head in rock medium.It streams throughcommunicating interstices of fractured zones mostly.
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释义
地下径流是岩石介质中由水头高处向水头低处流动的地下水流,它主要通过断裂带等连通的空隙流动。
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