AbstractLet S be a stream surface in a flow. Let ω3 be the vertical component of the vorticity on S. In the present work we make an extension of the concept of the vorticity on S; we define the geodesic vorticity Ω and the vortical deviation D and we present some of its properties. The geodesic vorticity Ω will be Ω=∂u2∂s1−∂u1∂s2 where u⃗=(u1,u2,0) is the velocity field on S, and s1, s2 are, respectively, the arc length parameters of the lines of the maximum and minimum normal curvature on the surface S. The vortical deviation D will be the difference between the geodesic vorticity Ω and the vorticity ω3, that is D=Ω−ω3. The main results of this work are the relation between D and the curvatures on S (total curvature, geodesic curvature)
A method of determining the boundary conditions for the Navier-Stokes equations in stream function-v...
Accurate field data have been collected along the Febbraro River (central Italian Alps) during quasi...
In this paper it is shown how the analysis of Came and Marsh ( I) can be extended to provide estima...
AbstractLet S be a stream surface in a flow. Let ω3 be the vertical component of the vorticity on S....
The vortex is a common phenomenon in fluid field. In this paper, vortex can be represented by curvat...
By means of the solution of the linearized equation for the vertical components of the vorticity, th...
The complete form of the vertical vorticity tendency equation (the complete-form vorticity equation)...
<p>Changes of cross-sectional mean vorticity from the bottom of the river to 1.3 meters above the ri...
© 2019 Rina PervenStreamline geometry has been studied in case of turbulent wall flows. Complex but ...
Turbulence has a significant influence on fluvial processes. Especially in the sharp bends of geomet...
Abstract A theory is developed for the vorticity and its substantial derivative just downstream of a...
In this paper we suppose that the initial datum for the 2D Navier–Stokes equations are of the vortex...
The development of streamwise vortices and transition of the three-dimensional boundary layer flow o...
The mechanism of the flow resistance in open channels and pipelines is of vital importance for vario...
In this paper the gradients of flow parameters and the expression for vorticity vector behind three-...
A method of determining the boundary conditions for the Navier-Stokes equations in stream function-v...
Accurate field data have been collected along the Febbraro River (central Italian Alps) during quasi...
In this paper it is shown how the analysis of Came and Marsh ( I) can be extended to provide estima...
AbstractLet S be a stream surface in a flow. Let ω3 be the vertical component of the vorticity on S....
The vortex is a common phenomenon in fluid field. In this paper, vortex can be represented by curvat...
By means of the solution of the linearized equation for the vertical components of the vorticity, th...
The complete form of the vertical vorticity tendency equation (the complete-form vorticity equation)...
<p>Changes of cross-sectional mean vorticity from the bottom of the river to 1.3 meters above the ri...
© 2019 Rina PervenStreamline geometry has been studied in case of turbulent wall flows. Complex but ...
Turbulence has a significant influence on fluvial processes. Especially in the sharp bends of geomet...
Abstract A theory is developed for the vorticity and its substantial derivative just downstream of a...
In this paper we suppose that the initial datum for the 2D Navier–Stokes equations are of the vortex...
The development of streamwise vortices and transition of the three-dimensional boundary layer flow o...
The mechanism of the flow resistance in open channels and pipelines is of vital importance for vario...
In this paper the gradients of flow parameters and the expression for vorticity vector behind three-...
A method of determining the boundary conditions for the Navier-Stokes equations in stream function-v...
Accurate field data have been collected along the Febbraro River (central Italian Alps) during quasi...
In this paper it is shown how the analysis of Came and Marsh ( I) can be extended to provide estima...