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Untitled - Aerobib - Universidad Politécnica de Madrid

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1.8. CHEMICAL KINETICS 33<br />

This structure can be obtained from Quantum Mechanics or be postulated from the<br />

structure of the molecules. The Absolute Reaction Rate Theory has been successfully<br />

applied to the study of a great number of reactions well as to many other physical<br />

and physicochemical phenomena. A full <strong>de</strong>velopment of the theory can be found, for<br />

instance, in the works mentioned in Refs. [24] and [25].<br />

In the previous study it has been assumed that a single one directional reaction<br />

takes place within the mixture. Generally, all reactions proceed simultaneously in both<br />

senses at different rates. Thus, reaction (1.112) must be substituted by the following<br />

∑<br />

ν iA ′ i ⇄ ∑<br />

i<br />

i<br />

ν ′′<br />

i A i , (1.134)<br />

and the rate w i of production of species A i is given by the expressions<br />

(<br />

)<br />

∏ ∏<br />

w i = M i (ν i ′′ − ν i)<br />

′ k f c ν′ i<br />

− k b c ν′′ i<br />

. (1.135)<br />

Here k f and k b are the specific rates corresponding to the forward and backward reactions<br />

respectively.<br />

i<br />

On the other hand to be able to form the products, the reacting molecules must<br />

contact one another. This reduces the molecularity of a single elementary reaction to<br />

1, 2 or 3, since the probability of a collision of more than three molecules is practically<br />

nil. Consequently, when the reaction rate <strong>de</strong>pends in a complicated way on the<br />

concentrations, it can be assured that it proceeds from the combination of several elementary<br />

reactions. The basic problem of Chemical Kinetics is then the establishment<br />

of the set of elementary reactions that produce within the mixture. For example, the<br />

stoichiometric equation for the <strong>de</strong>composition of ozone is<br />

While the following is the actual system of reactions [28]:<br />

i<br />

i<br />

i<br />

2O 3 ⇄ 3O 2 . (1.136)<br />

O 3 +G k fi<br />

⇄<br />

k b1<br />

O+O 2 +G, (1.137)<br />

O+O 3<br />

k f2<br />

⇄<br />

k b2<br />

2O 2 , (1.138)<br />

O 2 +G k f3<br />

⇄<br />

k b3<br />

2O+G. (1.139)<br />

Here G is one of the atoms or molecules of the mixture. Each one of these reactants<br />

acts at its own reaction rate and the rate of consumption of the ozone results from

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