Discussion at Maximum Sediment Discharge Theory

Authors

  • Levent Yilmaz Nisantasi University, 1453 Neocampus, Civil Engineering Department, Hydraulic Division, 80626, Maslak, Istanbul, Turkey

DOI:

https://doi.org/10.30564/jgr.v3i1.1572

Abstract

It is observed the gravel river sediment discharge with existing empirical regime relationships. The aim of the research is to give a mathematical model about the stable cross-section geometry and to determine a model for the stable slope of an alluvial channel which is in nature seldom stable. In an alluvial channel to reach an equilibrium condition, it changes its plane geometry until to have a stable condition in plane configuration. There are three different parameters in plan configuration about river behavior: width, depth and slope.

Keywords:

Sediment transport; Mathematical model; Empirical regime relationship

References

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[3] Bray, D. I.. Regime Equations for gravel bed rivers.Proceedings of the International workshop on engineering Problems in the Management of Gravel Bed Rivers, Newtown, Powys, United Kingdom,1980.

[4] Kennedy, R. G.. On the Prevention of Silting in irrigation channels. Proceedings, Institution of Civil Engineering, 1895, 119.

[5] Lacey, G.. Stable channels in alluvium. Proceedings,Institution of Civil Engineers, 1930, 229:259-384.

[6] Ramette, M.. A Theoretical Approach on Fluvial Processes. International Symposium on River Sedimentation, Beijing, China, 1980.

[7] Yilmaz, L.. On the problem of the meander development in alluvial channels. Bulletin of the Technical University of Istanbul, 1990, 43(4): 553-365.

[8] Yilmaz, L.. Meanderbildung, Beitrag in Türkisches Wissenschafts - Technologiezentrum e.V. Berlin [IWAWI]. Technische Universitaet Berlin, West Germany, 1989.

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How to Cite

Yilmaz, L. (2020). Discussion at Maximum Sediment Discharge Theory. Journal of Geographical Research, 3(1), 1–5. https://doi.org/10.30564/jgr.v3i1.1572