Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel

Extreme conditions as flash floods in steep mobile-bed streams induce flows which carry a huge amount of sediment. Typically, the flow with the intense transport of sediment is stratified with a layered structure above an erodible plane bed. The paper deals with local flow characteristics in the lay...

Full description

Bibliographic Details
Main Authors: Zrostlík Štěpán, Bareš Vojtěch, Krupička Jan, Picek Tomáš, Matoušek Václav
Format: Article
Language:English
Published: EDP Sciences 2016-01-01
Series:EPJ Web of Conferences
Online Access:http://dx.doi.org/10.1051/epjconf/201611402144
id doaj-ff8d2fda0a904a3a9af3b42d91cc3452
record_format Article
spelling doaj-ff8d2fda0a904a3a9af3b42d91cc34522021-08-02T04:01:33ZengEDP SciencesEPJ Web of Conferences2100-014X2016-01-011140214410.1051/epjconf/201611402144epjconf_efm2016_02144Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channelZrostlík Štěpán0Bareš Vojtěch1Krupička Jan2Picek Tomáš3Matoušek Václav4Department of Hydraulics and Hydrology, Czech Technical University in PragueDepartment of Hydraulics and Hydrology, Czech Technical University in PragueDepartment of Hydraulics and Hydrology, Czech Technical University in PragueDepartment of Hydraulics and Hydrology, Czech Technical University in PragueDepartment of Hydraulics and Hydrology, Czech Technical University in PragueExtreme conditions as flash floods in steep mobile-bed streams induce flows which carry a huge amount of sediment. Typically, the flow with the intense transport of sediment is stratified with a layered structure above an erodible plane bed. The paper deals with local flow characteristics in the layered structure of the two-phase flow composed of water and sediment. We present experimental data and results for two different fractions of plastic particles obtained using two acoustic Doppler methods and a Prandtl probe. The results contain vertical profiles of longitudinal velocity component and local turbulent characteristics of the flow as the Reynolds stress and turbulent intensity. The effect of the layered character of the flow on the flow characteristics is discussed. Special attention is paid to the distribution of Reynolds stress in the sediment-rich transport layer above the bed and to the evaluation of ability of carrier turbulent eddies to support sediment grains in and above the transport layer.http://dx.doi.org/10.1051/epjconf/201611402144
collection DOAJ
language English
format Article
sources DOAJ
author Zrostlík Štěpán
Bareš Vojtěch
Krupička Jan
Picek Tomáš
Matoušek Václav
spellingShingle Zrostlík Štěpán
Bareš Vojtěch
Krupička Jan
Picek Tomáš
Matoušek Václav
Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
EPJ Web of Conferences
author_facet Zrostlík Štěpán
Bareš Vojtěch
Krupička Jan
Picek Tomáš
Matoušek Václav
author_sort Zrostlík Štěpán
title Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
title_short Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
title_full Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
title_fullStr Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
title_full_unstemmed Distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
title_sort distribution of velocity and turbulent characteristics in coarse-sediment laden flows above erodible plane bed in open channel
publisher EDP Sciences
series EPJ Web of Conferences
issn 2100-014X
publishDate 2016-01-01
description Extreme conditions as flash floods in steep mobile-bed streams induce flows which carry a huge amount of sediment. Typically, the flow with the intense transport of sediment is stratified with a layered structure above an erodible plane bed. The paper deals with local flow characteristics in the layered structure of the two-phase flow composed of water and sediment. We present experimental data and results for two different fractions of plastic particles obtained using two acoustic Doppler methods and a Prandtl probe. The results contain vertical profiles of longitudinal velocity component and local turbulent characteristics of the flow as the Reynolds stress and turbulent intensity. The effect of the layered character of the flow on the flow characteristics is discussed. Special attention is paid to the distribution of Reynolds stress in the sediment-rich transport layer above the bed and to the evaluation of ability of carrier turbulent eddies to support sediment grains in and above the transport layer.
url http://dx.doi.org/10.1051/epjconf/201611402144
work_keys_str_mv AT zrostlikstepan distributionofvelocityandturbulentcharacteristicsincoarsesedimentladenflowsaboveerodibleplanebedinopenchannel
AT baresvojtech distributionofvelocityandturbulentcharacteristicsincoarsesedimentladenflowsaboveerodibleplanebedinopenchannel
AT krupickajan distributionofvelocityandturbulentcharacteristicsincoarsesedimentladenflowsaboveerodibleplanebedinopenchannel
AT picektomas distributionofvelocityandturbulentcharacteristicsincoarsesedimentladenflowsaboveerodibleplanebedinopenchannel
AT matousekvaclav distributionofvelocityandturbulentcharacteristicsincoarsesedimentladenflowsaboveerodibleplanebedinopenchannel
_version_ 1721242881950220288