Despite the existing knowledge concerning the hydrodynamic processes at river junctions, there is still a lack of information regarding the particular case of low width and discharge ratios, which are the typical conditions of mountain river confluences. Aiming at filling this gap, laboratory and numerical experiments were conducted, comparing the results with literature findings. Ten different confluences from 45 ∘ to 90 ∘ were simulated to study the effects of the junction angle on the flow structure, using a numerical code that solves the 3D Reynolds Averaged Navier-Stokes (RANS) equations with the k- ϵ turbulence closure model. The results showed that the higher the junction angle, the wider and longer the retardati...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Despite the existing knowledge concerning the hydrodynamic processes at river junctions, there is st...
Despite the existing knowledge concerning the hydrodynamic processes at river junctions, there is st...
The effect of main channel curvature on the flow pattern in river junctions is a complex and importa...
Confluences exist not only in nature, like in streams or rivers but also constructed environment lik...
Confluences exist not only in nature, like in streams or rivers but also constructed environment lik...
Flow connection in channels is a phenomenon which frequently happens in rivers, water and drainage c...
This thesis investigates controls on and the nature of three-dimensional flow structures at river ch...
Open-channel confluences are common in nature as well as in hydraulic structures and urban drainage ...
Open channel and river confluences have received a lot of attention in hydraulic literature, because...
River confluences are important due to their role on transport of sediments, erosion, transport of n...
River confluences are important due to their role on transport of sediments, erosion, transport of n...
The effect of main channel curvature on the flow pattern in river junctions is a complex and importa...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Despite the existing knowledge concerning the hydrodynamic processes at river junctions, there is st...
Despite the existing knowledge concerning the hydrodynamic processes at river junctions, there is st...
The effect of main channel curvature on the flow pattern in river junctions is a complex and importa...
Confluences exist not only in nature, like in streams or rivers but also constructed environment lik...
Confluences exist not only in nature, like in streams or rivers but also constructed environment lik...
Flow connection in channels is a phenomenon which frequently happens in rivers, water and drainage c...
This thesis investigates controls on and the nature of three-dimensional flow structures at river ch...
Open-channel confluences are common in nature as well as in hydraulic structures and urban drainage ...
Open channel and river confluences have received a lot of attention in hydraulic literature, because...
River confluences are important due to their role on transport of sediments, erosion, transport of n...
River confluences are important due to their role on transport of sediments, erosion, transport of n...
The effect of main channel curvature on the flow pattern in river junctions is a complex and importa...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...
Two major morphological phenomena in alluvial river confluences are the development of an avalanche ...