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'''Dispersive mass transfer''', in [[fluid dynamics]], is the spreading of mass from highly concentrated areas to less concentrated areas. It is one form of [[mass transfer]].


Dispersive mass flux is analogous to [[diffusion]], and it can also be described using [[Fick's law|Fick's first law]]:
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:<math>J = -E \frac{dc}{dx}, </math>
 
where c is mass concentration of the species being dispersed, E is the dispersion coefficient, and x is the position in the direction of the concentration gradient. Dispersion can be differentiated from diffusion in that it is caused by non-ideal flow patterns (i.e. deviations from [[plug flow]]) and is a macroscopic phenomenon, whereas diffusion is caused by random molecular motions (i.e. [[Brownian motion]]) and is a microscopic phenomenon. Dispersion is often more significant than diffusion in [[convection]]-diffusion problems. The dispersion coefficient is frequently modeled as the product of the fluid velocity, ''U'', and some characteristic length scale, ''α'':
 
:<math>E = \alpha U.</math>
 
{{DEFAULTSORT:Dispersive Mass Transfer}}
[[Category:Chemical engineering]]
 
 
{{Physics-stub}}

Latest revision as of 14:44, 27 October 2014

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