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Numerical Simulation of Bed Material Transport in the Lower Mississippi River
The flood protection levees and other man-made changes along the Mississippi River have deprived the Louisiana coast of a large amount of sediment which is now being lost to the Gulf of Mexico. Numerical modeling of hydrodynamics and sediment transport was undertaken to assess the potential impacts...
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Published in: | Journal of coastal research 2009-01, Vol.SI (56), p.1449-1453 |
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creator | Pereire, J. F. McCorquodale, J.A. Meselhe, E.A. Georgiou, I.Y. Allison, M.A. |
description | The flood protection levees and other man-made changes along the Mississippi River have deprived the Louisiana coast of a large amount of sediment which is now being lost to the Gulf of Mexico. Numerical modeling of hydrodynamics and sediment transport was undertaken to assess the potential impacts of options to re-connect the River to the coastal wetlands as part of coastal restoration efforts. In this study, HEC-RAS 4.0, a 1-D mobile-bed numerical model was calibrated and applied to a reach of the lower Mississippi River. The calibration utilized long term historic sediment data as well as recent observations. The hydraulics and sediment modules were calibrated for the reach between Tarbert Landing (RM 306, km 492) and Venice (RM 11, km 17). During calibration, the Engelund-Hansen formula gave the best results compared to observations, while during validation, the model reproduced observed hydrodynamics, bed material loads and erosion/deposition patterns fairly well. The predicted sand loads at Belle Chasse (RM 76, km 122) were compared with available data and the agreement, expressed as a ratio of predicted to observed loads, was within the acceptable range of 0.5 to 2. |
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F. ; McCorquodale, J.A. ; Meselhe, E.A. ; Georgiou, I.Y. ; Allison, M.A.</creator><creatorcontrib>Pereire, J. F. ; McCorquodale, J.A. ; Meselhe, E.A. ; Georgiou, I.Y. ; Allison, M.A.</creatorcontrib><description>The flood protection levees and other man-made changes along the Mississippi River have deprived the Louisiana coast of a large amount of sediment which is now being lost to the Gulf of Mexico. Numerical modeling of hydrodynamics and sediment transport was undertaken to assess the potential impacts of options to re-connect the River to the coastal wetlands as part of coastal restoration efforts. In this study, HEC-RAS 4.0, a 1-D mobile-bed numerical model was calibrated and applied to a reach of the lower Mississippi River. The calibration utilized long term historic sediment data as well as recent observations. The hydraulics and sediment modules were calibrated for the reach between Tarbert Landing (RM 306, km 492) and Venice (RM 11, km 17). 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F.</au><au>McCorquodale, J.A.</au><au>Meselhe, E.A.</au><au>Georgiou, I.Y.</au><au>Allison, M.A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Numerical Simulation of Bed Material Transport in the Lower Mississippi River</atitle><jtitle>Journal of coastal research</jtitle><date>2009-01-01</date><risdate>2009</risdate><volume>SI</volume><issue>56</issue><spage>1449</spage><epage>1453</epage><pages>1449-1453</pages><issn>0749-0208</issn><eissn>1551-5036</eissn><abstract>The flood protection levees and other man-made changes along the Mississippi River have deprived the Louisiana coast of a large amount of sediment which is now being lost to the Gulf of Mexico. Numerical modeling of hydrodynamics and sediment transport was undertaken to assess the potential impacts of options to re-connect the River to the coastal wetlands as part of coastal restoration efforts. In this study, HEC-RAS 4.0, a 1-D mobile-bed numerical model was calibrated and applied to a reach of the lower Mississippi River. The calibration utilized long term historic sediment data as well as recent observations. The hydraulics and sediment modules were calibrated for the reach between Tarbert Landing (RM 306, km 492) and Venice (RM 11, km 17). During calibration, the Engelund-Hansen formula gave the best results compared to observations, while during validation, the model reproduced observed hydrodynamics, bed material loads and erosion/deposition patterns fairly well. The predicted sand loads at Belle Chasse (RM 76, km 122) were compared with available data and the agreement, expressed as a ratio of predicted to observed loads, was within the acceptable range of 0.5 to 2.</abstract><cop>Fort Lauderdale</cop><pub>Coastal Education & Research Foundation (CERF)</pub><tpages>5</tpages></addata></record> |
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subjects | Boundary conditions Calibration Coastal Computational fluid dynamics Estuarine & Wetland Restoration Flood protection Fluid flow Fluvial transport Hydraulics Hydrodynamics Hydrological modeling Levees Levees & battures Load Material transport processes Mathematical models Modeling Rivers Salinity Sand Sediment transport Sediments Simulation Studies |
title | Numerical Simulation of Bed Material Transport in the Lower Mississippi River |
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