Andere Kunden interessierten sich auch für
![Coherent structures and secondary motions in open duct flow]( "Coherent structures and secondary motions in open duct flow")
Coherent structures and secondary motions in open duct flow57,00 €![A hydrodynamical perspective on the turbulent transport of bacteria in rivers]( "A hydrodynamical perspective on the turbulent transport of bacteria in rivers")
A hydrodynamical perspective on the turbulent transport of bacteria in rivers51,00 €![Strategies to reduce friction losses and their implications for the energy efficient design of internal flow domains]( "Strategies to reduce friction losses and their implications for the energy efficient design of internal flow domains")
Strategies to reduce friction losses and their implications for the energy efficient design of internal flow domains42,00 €![Numerical Study on the Propagation of Turbulent Fronts in Dilute Polymer Solutions]( "Numerical Study on the Propagation of Turbulent Fronts in Dilute Polymer Solutions")
Numerical Study on the Propagation of Turbulent Fronts in Dilute Polymer Solutions41,00 €![Turbulence, Coherent Structures, Dynamical Systems and Symmetry]( "Turbulence, Coherent Structures, Dynamical Systems and Symmetry")
Turbulence, Coherent Structures, Dynamical Systems and Symmetry114,99 €![The Role of Coherent Structures in Modelling Turbulence and Mixing]( "The Role of Coherent Structures in Modelling Turbulence and Mixing")
The Role of Coherent Structures in Modelling Turbulence and Mixing83,99 €![Turbulent Shear Flows 7]( "Turbulent Shear Flows 7")
Turbulent Shear Flows 774,99 €
The origin of secondary currents and subaqueous sediment patterns in natural rivers is analysed from first principles. For this purpose, simulations of sediment transport in canonical turbulent open channel flows are performed using a numerical technique that resolves all relevant flow scales and the dynamics of the individual sand grains. The high-fidelity datasets reveal the fundamental importance of individual coherent structures for the development of sediment patterns and secondary flows.