Instytut Budownictwa Wodnego
Polskiej Akademii Nauk

Essay #8806 details

ATTRIBUTEVALUE
typeA
database id8806
titleAn equilibrium transport formula for modeling sedimentation of dredged channels
authorsKaczmarek L. M.1, Sawczyński S.2, Biegowski J.3
affiliations
pages1750015-1 — 1750015-35
notesKopia w oprac. Tp4501
DOI10.1142/S0578563417500152
keywordsHydrodynamic equilibrium, sediment transport, bathymetry, grain size distribution, sedimentation, dredged channels
abstractsThe proposed formula for modeling sedimentation is based on a concept of hydrodynamic equilibrium in sediment transport. Hydrodynamic equilibrium occurs when the sediment transport is in a form of grain jumps with the distance traveled dx smaller than the one established in the numerical modeling. A first-order upwind scheme FDM is applied. It provides the solution to equations describing changes in bathymetry in time and space coupled with simultaneous changes of bed sediment distribution. A clear-cut division of sediment transport into those during wave crest and wave trough is proposed. The results of bathymetry modeling coincided satisfactorily with the laboratory data. Moreover, the longer the experiments run, the more the results of measurements are compliant with the calculations. A certain time is needed for sediment transport to reach the hydrodynamic equilibrium, especially when the suspended load is significant. It is reached after going through the initial stages of bed level changes coupled with simultaneous changes of grain size distribution. The application of the model to field conditions shows its ability to predict sedimentation of dredged channels. Furthermore, the calculations show a good agreement with measured bed grain size distributions of sediment samples taken from the sites within the navigational channel of Łeba Port in Poland.
attributes [reviewed] [scientific]
languageen
PART OF
typeC
database id8873
year2017
seriesCoastal Engineering Journal
issueVol. 59, No. 3

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