Large eddy simulation of turbulence and solute transport in a forested headwater stream

• Published in: Journal of geophysical research. Earth surface Vol. 121; no. 1; pp. 146 - 167
• Main Authors: Khosronejad, A., Hansen, A. T., Kozarek, J. L., Guentzel, K., Hondzo, M., Guala, M., Wilcock, P., Finlay, J. C., Sotiropoulos, F.
• Format: Journal Article
• Language: English
• Published: Washington Blackwell Publishing Ltd 01-01-2016
• Subjects: Computer simulation; Concentration time; Creeks & streams; Debris; Detritus; Flow pattern; forested stream; Geophysics; Large eddy simulation; Marine; Mathematical models; Metropolitan areas; Natural streams; Roughness; Simulation; Solute transport; Solutes; Streambeds; Streams; Time series; Tracers; Transport; Transport processes; Turbulence; USA, Minnesota
• ISSN: 2169-9003; 2169-9011
• DOI: 10.1002/2014JF003423

The large eddy simulation (LES) module of the Virtual StreamLab (VSL3D) model is applied to simulate the flow and transport of a conservative tracer in a headwater stream in Minnesota, located in the south Twin Cities metropolitan area. The detailed geometry of the stream reach, which is ∼135 m long, ∼2.5 m wide, and ∼0.15 m deep, was surveyed and used as input to the computational model. The detailed geometry and location of large woody debris and bed roughness elements up to ∼0.1 m in size were also surveyed and incorporated in the numerical simulation using the Curvilinear Immersed Boundary approach employed in VSL3D. The resolution of the simulation, which employs up to a total of 25 million grid nodes to discretize the flow domain, is sufficiently fine to directly account for the effect of large woody debris and small cobbles (on the streambed) on the flow patterns and transport processes of conservative solutes. Two tracer injection conditions, a pulse and a plateau release, and two cross sections of measured velocity were used to validate the LES results. The computed results are shown to be in good agreement with the field measurements and tracer concentration time series. To our knowledge, the present study is the first attempt to simulate via high‐resolution LES solute transport in a natural stream environment taking into account a range of roughness length scales spanning an order of magnitude: from small cobbles on the streambed (∼0.1 m in diameter) to large woody debris up to ∼3 m long.
Key Points
Large eddy simulation of flow and solute transport in a forested stream
Simulation results for time series of solute transport are validated using field data
Simulations revealed details of mechanisms by which tracer are trapped in local areas