THE DEPENDENCE OF SUSPENDED SAND CONCENTRATION ON THE DEGREE OF STORM DEVELOPMENT

Ruben Kos'yan; Joachim Grune; Boris Divinsky; Igor Podymov; Chris Vincent; Houcine Oumeraci; Alireza Ahmari

doi:10.9753/icce.v32.sediment.19

No. 32 (2010), Sediment Transport and Morphology

No. 32 (2010)

THE DEPENDENCE OF SUSPENDED SAND CONCENTRATION ON THE DEGREE OF STORM DEVELOPMENT

Sediment Transport and Morphology

https://doi.org/10.9753/icce.v32.sediment.19

Published 2011-01-21

Ruben Kos'yan⁺⁻
Joachim Grune⁺⁻
Boris Divinsky⁺⁻
Igor Podymov⁺⁻
Chris Vincent⁺⁻
Houcine Oumeraci⁺⁻
Alireza Ahmari⁺⁻

Ruben Kos'yan

The Southern Branch of the P.P.Shirshov Institute of Oceanology, Russian Academy of Sciences, 353467, Krasnodar reg., Gelendzhik, Russia

Joachim Grune

Coastal Research Centre FZK of University Hannover & Technical University Braunschweig, Merkurstraße 11, 30419 Hannover, Germany

Boris Divinsky

The Southern Branch of the P.P.Shirshov Institute of Oceanology, Russian Academy of Sciences, 353467, Krasnodar reg., Gelendzhik, Russia

Igor Podymov

The Southern Branch of the P.P.Shirshov Institute of Oceanology, Russian Academy of Sciences, 353467, Krasnodar reg., Gelendzhik, Russia

Chris Vincent

School of Environmental Sciences, University of East Anglia, Norwich, U.K.

Houcine Oumeraci

Coastal Research Centre FZK of University Hannover & Technical University Braunschweig, Leichtweiß-Institute of Technical University Braunschweig Merkurstraße 11, 30419 Hannover, Germany

Alireza Ahmari

Coastal Research Centre FZK of University Hannover & Technical University Braunschweig, Merkurstraße 11, 30419 Hannover, Germany

Proceedings of the 32nd International Conference

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Keywords

laboratory experiment
Large Wave Channel
wave spectra
JONSWAP
suspended sediment concentration
wave-wave interactions

How to Cite

Kos’yan, R., Grune, J., Divinsky, B., Podymov, I., Vincent, C., Oumeraci, H., & Ahmari, A. (2011). THE DEPENDENCE OF SUSPENDED SAND CONCENTRATION ON THE DEGREE OF STORM DEVELOPMENT. Coastal Engineering Proceedings, 1(32), sediment.19. https://doi.org/10.9753/icce.v32.sediment.19

Abstract

The basic purpose of the present research is the establishment of connections between surface waves' spectral characteristics and laws of the bottom material suspension. The basic method is the laboratory experiment that allows controlling the interconnected dynamic parameters of the water environment and processes of bottom deposits transport. It is shown, that observed suspension laws physical preconditions are the nonlinear intrawave interactions and hence the redistribution of waves spectral energy in frequency area.

https://doi.org/10.9753/icce.v32.sediment.19

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References

Grune J., Kosyan R., Oumeraci H., Podymov I., Schmidt-Koppenhagen R., Vincent C. 2007. Largescale laboratory modelling of suspended sand concentration fluctuations under irregular waves, Proc. of the Coastal Sediments'07, ASCE.

Hasselmann, K., Barnett, T., Bouws, E., Carlson, H., Cartwright, D., Enke, P., Ewing, J., Gienapp, H., Hasselmann, D., Kruseman, P., Meerburg, A., Muller, P., Olbers, D., Richter, K., Sell, W. and Walden, H. 1973. Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP), Dtsch. Hydrogr. Z. Suppl. A, 8:-95.

Liu, Z. and Frigaard, P. 2001. Generation and analysis of random waves, Aalborg Universitet, 76 p.

Thompson, E. and Vincent, C. 1985. Significant wave height for shallow water design, ASCE Jour. Waterw., Port, Coastal and Ocean Engr., Vol. 111, pp. 828-842. http://dx.doi.org/10.1061/(ASCE)0733-950X(1985)111:5(828)

Authors retain copyright and grant the Proceedings right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this Proceedings.

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THE DEPENDENCE OF SUSPENDED SAND CONCENTRATION ON THE DEGREE OF STORM DEVELOPMENT

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