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

Proceedings of the International Conference on Coastal Engineering

Joachim Grüne³  Ruben Kos'yan¹  Alireza Ahmari³  Igor Podymov¹  Boris Divinsky¹  Chris Vincent²  Houcine Oumeraci⁴ 

[1] The Southern Branch of the P.P.Shirshov Institute of Oceanology, Russian Academy of Sciences, 353467, Krasnodar reg., Gelendzhik, Russia;School of Environmental Sciences, University of East Anglia, Norwich, U.K.;Coastal Research Centre FZK of University Hannover & Technical University Braunschweig, Merkurstraße 11, 30419 Hannover, Germany;Coastal Research Centre FZK of University Hannover & Technical University Braunschweig, Leichtweiß-Institute of Technical University Braunschweig Merkurstraße 11, 30419 Hannover, Germany

关键词: laboratory experiment;    Large Wave Channel;    wave spectra;    JONSWAP;    suspended sediment concentration;    wave-wave interactions;   

DOI  :  10.9753/icce.v32.sediment.19

学科分类：建筑学

来源: Coastal Engineering Research Council

【 摘 要 】

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.

【 授权许可】

Unknown