On local velocity measurement in gravity-driven flows with intense bedload of coarse lightweight particles
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F16%3A00301953" target="_blank" >RIV/68407700:21110/16:00301953 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.flowmeasinst.2016.06.023" target="_blank" >http://dx.doi.org/10.1016/j.flowmeasinst.2016.06.023</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.flowmeasinst.2016.06.023" target="_blank" >10.1016/j.flowmeasinst.2016.06.023</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
On local velocity measurement in gravity-driven flows with intense bedload of coarse lightweight particles
Popis výsledku v původním jazyce
A broad dataset of sheet-flow experiments with granular material under steady and uniform conditions is presented in this paper with the focus on measurements of streamwise velocity component. Three different lightweight sediment fractions were used during 128 experimental runs across a wide range of sheet-flow modes which were represented by dimensionless Shields parameter from 0.3 up to 2.3. The local velocity information was obtained using three independent methods: Prandtl probe (PT), Ultrasonic Velocity Profiler (UVP) and Acoustic Doppler Velocity Profiler (ADVP). The measurement methods were compared to each other using results in absolute and dimensionless velocity magnitudes. Limitations of the methods are discussed. The results were consistent for all experimental runs and are further used for a description of the observed flow internal structure. The capability of individual measuring methods is demonstrated here on an identification of a transport layer of a linear velocity distribution and of a basal sublayer at the transition between the stationary bed and the transport layer.
Název v anglickém jazyce
On local velocity measurement in gravity-driven flows with intense bedload of coarse lightweight particles
Popis výsledku anglicky
A broad dataset of sheet-flow experiments with granular material under steady and uniform conditions is presented in this paper with the focus on measurements of streamwise velocity component. Three different lightweight sediment fractions were used during 128 experimental runs across a wide range of sheet-flow modes which were represented by dimensionless Shields parameter from 0.3 up to 2.3. The local velocity information was obtained using three independent methods: Prandtl probe (PT), Ultrasonic Velocity Profiler (UVP) and Acoustic Doppler Velocity Profiler (ADVP). The measurement methods were compared to each other using results in absolute and dimensionless velocity magnitudes. Limitations of the methods are discussed. The results were consistent for all experimental runs and are further used for a description of the observed flow internal structure. The capability of individual measuring methods is demonstrated here on an identification of a transport layer of a linear velocity distribution and of a basal sublayer at the transition between the stationary bed and the transport layer.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
BK - Mechanika tekutin
OECD FORD obor
—
Návaznosti výsledku
Projekt
<a href="/cs/project/GA16-21421S" target="_blank" >GA16-21421S: Analýza stratifikovaného proudění s volnou hladinou založená na kinetické teorii zrnitých směsí</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Flow Measurement and Instrumentation
ISSN
0955-5986
e-ISSN
—
Svazek periodika
51
Číslo periodika v rámci svazku
October
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
11
Strana od-do
68-78
Kód UT WoS článku
000386318000008
EID výsledku v databázi Scopus
2-s2.0-84984876238