Results 11 to 20 of about 363,183 (210)
Free surface flows in macro- and intermediate roughness conditions have a high aeration potential causing the flow characteristics to vary with slopes and discharges.
Stefano Pagliara +2 more
doaj +1 more source
Very-large-scale motions in rough-bed open-channel flow [PDF]
Acknowledgements The study has been supported by two EPSRC/UK grants, ‘High-resolution numerical and experimental studies of turbulence-induced sediment erosion and near-bed transport’ (EP/G056404/1) and ‘Bed friction in rough-bed free-surface flows: a ...
Cameron, S. M. +2 more
core +1 more source
Predicting Hydraulic Jump Length on Rough Beds Using Data-Driven Models [PDF]
The hydraulic jump can be used for some purpose such as dissipating the flow energy in order to prevent bed erosion; aerating water and facilitating the mixing procedure of chemical that used for water purification.
Payam Khosravinia +2 more
doaj +1 more source
Coherent structures in oscillatory flows within the laminar-to-turbulent transition regime for smooth and rough walls [PDF]
This is an Accepted Manuscript of an article published by Taylor & Francis Group in [Journal of hydraulic research] on [2016], available online at: http://www.tandfonline.com/10.1080/00221686.2016.1174960We investigate coherent structures present in ...
Bateman Pinzón, Allen +3 more
core +3 more sources
PREDICTING MOVABLE BED ROUGHNESS IN COASTAL WATERS [PDF]
Accurately predicting movable bed roughness is essential to the analyses of transport processes, but when the bottom is rippled, as it commonly is in the coastal environment, characterizing the roughness is less straightforward than when the bottom is flat.
Humbyrd, Chelsea Joy, Madsen, Ole S.
openaire +2 more sources
Impact of bed roughness and sediment permeability on mass exchange across sediment-water interface
The mass exchange process across sediment-water interface (SWI) plays an important role in contaminant migration and transformation in natural waters. The mass exchange across the SWI for rough bed depends on both bed roughness and sediment permeability.
Jingyu FAN +4 more
doaj +1 more source
When using point measurement for environmental or sediment laden flows, there is well-recognised risk for not having aligned measurements that causes misinterpretation of the measured velocity data. In reality, these kinds of mismeasurement mainly happen
Jaan H. Pu
doaj +1 more source
Hydrodynamics of steep streams with planar coarse-grained beds: Turbulence, flow resistance, and implications for sediment transport [PDF]
The hydraulics of steep mountain streams differ from lower gradient rivers due to shallow and rough flows, energetic subsurface flow, and macro-scale form drag from immobile boulders and channel- and bed-forms.
Brun, Fanny +2 more
core +2 more sources
Bed shear stress measurements over rough fixed and mobile sediment beds in swash flows [PDF]
Direct measurements of bed shear stress have been conducted over rough fixed and mobile sediment beds in dambreak driven swash flows. The comparison between rough fixed and mobile bed results indicated the significant importance of grain borne shear ...
Baldock, Tom E., Jiang, Zhonglian
core +2 more sources
Air–water low patterns of hydraulic jumps on uniform beds macroroughness [PDF]
Hydraulic jumps are characterized by strong flow turbulence, flow aeration, and three-dimensional flow motions. Whereas comprehensive research into hydraulic jumps on smooth bed has improved the understanding of flow aeration and turbulence, limited ...
Chanson, Hubert, Felder. Stefan
core +1 more source

