Instantaneous transport of a passive scalar in a turbulent separated flow

• Published in: Environmental fluid mechanics (Dordrecht, Netherlands : 2001) Netherlands : 2001), 2018-04, Vol.18 (2), p.487-513
• Main Authors: Ouro, P., Fraga, B., Viti, N., Angeloudis, A., Stoesser, T., Gualtieri, C.
• Format: Article
• Language: English
• Subjects: Advection; Classical Mechanics; Covariance; Dispersion; Dye dispersion; Earth and Environmental Science; Earth Sciences; Environmental Physics; Flow separation; Fluid dynamics; Fluid flow; Fluid mechanics; Hydrodynamics; Hydrogeology; Hydrology/Water Resources; Large eddy simulation; Large eddy simulations; Mass flux; Mass transport; Oceanic eddies; Oceanography; Original; Original Article; Residence time; Residence time distribution; Residential density; Simulation; Solute transport; Solutes; Tracer transport; Tracers; Transport; Turbulence; Turbulent flow; Turbulent mixing; Velocity; Vortices
• ISSN: 1567-7419; 1573-1510
• DOI: 10.1007/s10652-017-9567-3

The results of large-eddy simulations of flow and transient solute transport over a backward facing step and through a 180° bend are presented. The simulations are validated successfully in terms of hydrodynamics and tracer transport with experimental velocity data and measured residence time distribution curves confirming the accuracy of the method. The hydrodynamics are characterised by flow separation and subsequent recirculation in vertical and horizontal directions and the solute dispersion process is a direct response to the significant unsteadiness and turbulence in the flow. The turbulence in the system is analysed and quantified in terms of power density spectra and covariance of velocity fluctuations. The injection of an instantaneous passive tracer and its dispersion through the system is simulated. Large-eddy simulations enable the resolution of the instantaneous flow field and it is demonstrated that the instabilities of intermittent large-scale structures play a distinguished role in the solute transport. The advection and diffusion of the scalar is governed by the severe unsteadiness of the flow and this is visualised and quantified. The analysis of the scalar mass transport budget quantifies the mechanisms controlling the turbulent mixing and reveals that the mass flux is dominated by advection.