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Mechanism for sediment convergence in the anthropogenically altered microtidal Nakdong Estuary, South Korea
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文摘

Rate and timing of sedimentation were examined at the altered Nakdong Estuary of Korea.

Altimeter observed episodic sedimentation of 6 cm during summer discharge in the main channel.

Sediment flux gradient was the main mechanism for the deposition during high discharge.

Gradual deposition of 4 cm also corresponds to the long-term rate in the west Nakdong.

Wave-enhanced sediment flux was the primary mechanism for gradual deposition.

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