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| | Diffusion |
 | | Diffusion fluxes can cause changes in the concentration distribution of the diffusing molecules, and to deal with these we need the full differential equation for diffusion, which can be written |
 | | Let's assume that the atmosphere is well-mixed by wind and turbulance at a height of 100 meters, and that diffusion is called upon to move CO from 100 meters to the ground. |
 | | In the steady state, we assume that all of the molecules reaching the surface of the cell at radius a are adsorbed, resulting in C=0 at r=a, and a constant rate, Q, of uptake of nutrient molecules. |
| www.cco.caltech.edu /~brokawc/Bi145/Diffusion.html (1796 words) |
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