1993
DOI: 10.1029/ce042p0504
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Modeling of suspended sediment transport in a tidal river

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Cited by 3 publications
(1 citation statement)
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“…The calculation on the flux of erosion and deposition requires estimation of the critical bottom friction velocities of erosion and deposition. Futawatari and Kusuda (1993) suggest that the critical bottom friction velocity of erosion is between 0.025 to 0.030 m/sec and the critical bottom friction velocity of deposition is about 0.005 m/sec. There will be interactions between the suspended solids concentrations and the amount of deposited mud.…”
Section: The Simulationmentioning
confidence: 92%
“…The calculation on the flux of erosion and deposition requires estimation of the critical bottom friction velocities of erosion and deposition. Futawatari and Kusuda (1993) suggest that the critical bottom friction velocity of erosion is between 0.025 to 0.030 m/sec and the critical bottom friction velocity of deposition is about 0.005 m/sec. There will be interactions between the suspended solids concentrations and the amount of deposited mud.…”
Section: The Simulationmentioning
confidence: 92%