Simulating Transient Sediment Waves in Aggraded Alluvial Channels by Double-Decomposition Method
Publication: Journal of Hydrologic Engineering
Volume 16, Issue 4
Abstract
By using the double-decomposition (DD) method, this study simulates transient sediment waves caused by aggradation described by a diffusion-type partial differential equation (PDE). The DD method solves the PDE by decomposing the solution function for sediment rate into a summation of number of components, where stands for the order of approximation. The solution was approximated by considering only the first three terms. The model satisfactorily simulated laboratory-measured aggradation bed profiles with, on average, a mean absolute error (MAE) of 0.70 cm, a root-mean-square error (RMSE) of 0.84 cm, a mean relative error (MRE) of 1.11%, and . The model performance was also tested by using numerical and error-function solutions. In addition, the results obtained from application of the DD solution to hypothetical field cases were found to be theoretically compatible with what may be observed in natural streams. However, sediment wave fronts in later periods of the simulation time reached equilibrium bed levels more quickly, around in the middle section of the channel.
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Acknowledgments
This research was supported by the Scientific and Technological Research Council of Turkey [TUBITAK] under Grant No. UNSPECIFIED106M274. The writers extend their sincere appreciation to TUBITAK for the financial support. The writers would also like to express their thanks to Professor Engin Aktas of the Civil Engineering Dept., Izmir Institute of Technology; and Professor Oguz Yilmaz of the Dept. of Mathematics, Izmir Institute of Technology for valuable discussions.
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© 2011 American Society of Civil Engineers.
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Received: Oct 2, 2009
Accepted: Sep 23, 2010
Published online: Sep 27, 2010
Published in print: Apr 1, 2011
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