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 empiricalregime relationships. The aim of the research is to give a mathematicalmodel about the stable cross-section geometry and to determine a modelfor 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 planegeometry until to have a stable condition in plane configuration. There arethree different parameters in plan configuration about river behavior: width,depth and slope.

Keywords:

Sediment transport, Mathematical model, Empirical regime relationship

References

[1] Ackers, P.. Experiments on small streams in alluvium. Journal of the Hydraulics Division, ASCE,1964,90(HY4): 1-38.

[2] Ackers, P.. Use of sediment transport concepts in stable channel design. International Workshop on Alluvial River Problems, Roorkee, India, March, 1980.

[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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Published

2020-07-02

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

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