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...
Main Authors: | , , , , |
---|---|
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 |