Large-eddy simulation has been shown to be able to faithfully reproduce observed turbulent statistics and the 3-D details and time evolutions of important coherent flow structures (scalar microfront, sweep/ejection cycles), which dominates the transport and diffusion processes in a range of plant canopies. The scales of such coherent eddies are important in defining the so-called near-field and far-field diffusion characteristics.
In this study, a large-eddy simulation is performed to simulate diffusion from/to line/point sources/sinks inside a horizontally homogeneous forest with an observed vertical profile of plant area density and under neutral stratification. The source (water vapor) and sink (carbon dioxide) strengths are prescribed from a coupled plant model with values close to midday observations in the field during the growing season. Both concentrations and fluxes distributions (footprint) will be presented for each source/sink configuration (line, point), as well as important diffusion properties such as eddy-diffusivity and Lagrangian time scales. While the lateral line source/sink allows assessment of diffusion properties in the streamwise and vertical directions, the point source/sink permits study of diffusion in the spanwise direction. Even though the domain size in this study is greater than in previous simulations, our emphasis here is on the near-field diffusion processes.
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