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We experimentally tested the effect of a  largerange in helical flow intensity and  sedimentmobility on equilibrium transverse  slopes,which resulted in a function for slope  effectsdepending on bed state and  sedimenttransport mode, that deviates from  linearfunctions with sediment mobility in  literature.Furthermore, we obtained basic  relationsfor sorting patterns as a function of  transverseslope and sediment mobility 

Original languageEnglish
Pages50-51
Publication statusPublished - 2017
EventNCR-Days 2017 - Wageningen, Netherlands
Duration: 1 Feb 20173 Feb 2017

Conference

ConferenceNCR-Days 2017
CountryNetherlands
CityWageningen
Period1/02/173/02/17
OtherNetherlands Centre for River Studies is a corporation of the Universities of Delft, Utrecht, Nijmegen, Twente and Wageningen, UNESCO-IHE, RWS-WVL and Deltares

ID: 42133684