Chapter
Apr 26, 2012
Geometric and Statistical Characteristics of Bed Forms in the Lower Mississippi River
Authors: K. Kheiashy [email protected], J. McCorquodale [email protected], I. Georgiou [email protected], and E. Meselhe [email protected]Author Affiliations
Publication: Coastal Sediments '07
Abstract
Bed forms in alluvial systems are three dimensional. The most common bed forms are: ripples, dunes and bars. Under certain flows, different bed forms may be superimposed on each other, e.g. dunes superimposed on bars or ripples superimposed on dunes. The irregularity in the bed of alluvial streams caused by the existence of bed forms produces additional flow resistance, which affects the hydrodynamics and sediment transport properties of the system. The geometry of bed forms in large alluvial, rivers such as the Lower Mississippi River exhibits both coherent and random characteristics. Average wave lengths and heights alone cannot adequately describe these bed forms. A spectral approach was used in this study to capture the periodicity and frequency distributions of the observed bed forms along a study reach in the Lower Mississippi River extending from river mile zero (Head of Passes) to river mile 234 (near Baton Rouge, LA).
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© 2007 American Society of Civil Engineers.
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Published online: Apr 26, 2012
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Doctoral Candidate, Civil and Environmental Engineering Department, University of New Orleans, Hydraulic Modeler, C.H. Fenstermaker and Associates Inc. 135 Regency Square, Lafayette, LA 70518. E-mail: [email protected]
Professor, Civil and Environmental Engineering Department, University of New Orleans, New Orleans, LA 70148. E-mail: [email protected]
Assistant Professor, Earth and Environmental Sciences Department, University of New Orleans, New Orleans, LA 70148. E-mail: [email protected]
Professor, Civil Engineering Department, University of Louisiana at Lafayette, Senior Hydraulic Engineer, C.H. Fenstermaker and Associates Inc. 135 Regency Square, Lafayette, LA 70518,. E-mail: [email protected]
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