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Untitled - Aerobib - Universidad Politécnica de Madrid

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48 CHAPTER 2. TRANSPORT PHENOMENA IN GAS MIXTURES<br />

Making use of relations (1.33) and (1.36) in chapter 1, it is obtained<br />

∑<br />

Y j<br />

D ij<br />

j≠i<br />

M j<br />

[<br />

¯vdi − ¯v dj<br />

+ ∇Y i<br />

− 1 ρ<br />

− ∇Y j<br />

Y j<br />

Y i<br />

(<br />

DT j<br />

Y j<br />

+ M j − M i ∇p<br />

M m p<br />

]<br />

= ¯0, (i = 1, 2, . . . , l).<br />

− D T i<br />

Y i<br />

) ∇T<br />

T<br />

(2.29)<br />

Diffusion of a species whose mass fraction is very small is particularly important<br />

in certain problems. For example, diffusion of active particles which propagate<br />

chemical reactions through a combustion wave. Then it becomes possible to give an<br />

explicit approximate expression for the diffusion flux of such species. For diffusion<br />

arising from differences in composition this expression is<br />

(<br />

∑ Y j ∇Yj<br />

− ∇Y )<br />

i<br />

j≠iM j Y j Y i<br />

¯f i = ρY i¯v di = ρY i<br />

∑ Y j<br />

. (2.30)<br />

M j D ij<br />

j≠i<br />

System (2.29) is, generally, too complicated to be used in the solution of many<br />

of the Aerothermochemistry problems. Therefore, in some of its applications, diffusion<br />

fluxes of the species are substituted by approximate expressions un<strong>de</strong>r the assumption<br />

that diffusion flux due to differences in composition ¯f iY of each species is<br />

proportional to its gradient of molar fraction. That is, by adopting for such flux an<br />

expression of the form<br />

¯f iY = −ρ M i<br />

M m<br />

D im ∇X i . (2.31)<br />

Here D im is a binary diffusion coefficient of the species through the mixture formed<br />

by the rest. This expression is exact only when binary diffusion coefficients and molar<br />

masses of the species are all equal. If mean molar mass of the mixture is also constant,<br />

one has<br />

¯f iY = −ρD im ∇Y i , (2.32)<br />

by virtue of Eqs. (1.33) and (1.36) in chapter 1. This expressions will be used in<br />

chapter 13. In aerothermochemical problems diffusion fluxes arising from differences<br />

in pressure and temperature are, in general, negligible. C. R. Wilke [14] has given an<br />

explicit approximate expression, empirically <strong>de</strong>duced, similar to (2.31) for fluxes due<br />

to differences in composition.

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