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the diffusion of light.
Thus, the longitudinal diffusion and the length of striations are reduced significantly.
Selection and drift in subdivided populations : a straightforward method for deriving diffusion approximations and applications involving dominance, selfing and local extinctions.
A mechanism is studied of the heterogeneity coefficient dissipation due to molecular diffusion.
Other elements of spatial diffusion, however, also emerge in this research.
The turbulence energy balance is examined, including the separate effects of vertical diffusion of pressure and local kinetic energy.
This would again suggest turbulent diffusion times of around 3000 years, which would then be the time required for achieving global homochirality in the ocean.
A commonly used procedure to estimate turbulent diffusion times is in terms of enhanced turbulent (eddy) diffusivities.
Here we have made the additional assumption that vertical diffusion of solute is negligible.
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