三角洲河道动床之自我调整作用，因水库水位之回水影响，其输沙特性有异于明渠均匀流。
The sediment transport resulted from self adjustment of the channel bed due to backwater effects differs from that occurring in a uniform flow.
三角洲河道动床之自我调整作用，因水库水位之回水影响，其输沙特性有异于明渠均匀流。
The sediment transport resulted from self adjustment of the channel bed due to backwater effects differs from that occurring in a uniform flow.
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