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Untitled - Aerobib - Universidad Politécnica de Madrid

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224 CHAPTER 8. IGNITION, FLAMMABILITY AND QUENCHING<br />

A correct stating of the problem would require first an a<strong>de</strong>quate formulation of<br />

the same, in an analogous way to the one used in Chap. 6 for the stationary wave. In<br />

the second place it would be necessary to perform an analysis of the type of solutions<br />

for the system of equations obtained un<strong>de</strong>r the set of initial and boundary conditions<br />

corresponding to the mo<strong>de</strong>l previously <strong>de</strong>scribed.<br />

If we consi<strong>de</strong>r the more simple case of an in<strong>de</strong>finite plane wave corresponding<br />

to a one-dimensional problem, in which case the initial energy must be stored between<br />

two parallel layers, it may be easily verified that the system of equations of Chap. 6,<br />

corresponding to a stationary wave, keeping the same notation, must be substituted by<br />

the following:<br />

a) Continuity equation.<br />

b) Energy equation.<br />

c) Diffusion equation.<br />

∂ρ<br />

∂t + ∂(ρv) = 0. (8.7)<br />

∂x<br />

( ∂T<br />

ρc p<br />

∂t + v ∂T )<br />

= ∂ (<br />

λ ∂T )<br />

+ qw. (8.8)<br />

∂x ∂x ∂x<br />

ρ<br />

( ∂Y<br />

∂t + v ∂Y )<br />

= ∂ (<br />

ρD ∂Y )<br />

+ w. (8.9)<br />

∂x ∂x ∂x<br />

Thus we obtain a system of three equations for the three unknowns T , v and Y .<br />

Since the process takes place at constant pressure, ρ is already <strong>de</strong>termined, as function<br />

of T .<br />

With reference to initial and boundary conditions corresponding to the mo<strong>de</strong>l<br />

un<strong>de</strong>r consi<strong>de</strong>ration, if 2d is the width of the heated slab and the origin of coordinates<br />

is fixed at the central point of the slab, we will have:<br />

a) Initial conditions (t = 0).<br />

0 < x < d : T = T f ,<br />

d < x < ∞ : T = T 0 ,<br />

(8.10)<br />

b) Boundary conditions (by symmetry).<br />

0 < x < ∞ : v = Y = 0.<br />

x = 0 :<br />

∂T<br />

∂x = v = ∂Y<br />

∂x = 0.<br />

Furthermore an additional condition must be introduced expressing that w must<br />

be zero for T = T 0 , as it was done for the case of a stationary wave.

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