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Effects of engineered channel morphology on water and sediment fluxes in a restored tidal marsh
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DOI：10.1016/j.ecoleng.2026.108043.png)
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Abstract
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• Peak flow velocity occurs shortly after marsh platform inundation and decreases with increasing channel sinuosity. • Higher channel sinuosity increases sediment retention within the system, but it reduces sediment delivery to the marsh. • Wider and shallower channel designs tend to promote greater water and sediment fluxes into restored tidal marshes.
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