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Essentials of Computational Chemistry

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15.1 REACTION KINETICS AND RATE CONSTANTS 521<br />

sides from time 0 to time τ leads to<br />

<br />

[A]0<br />

ln = k1τ (15.8)<br />

[A]τ<br />

Thus, experimentally, one plots the logarithm <strong>of</strong> the concentration ratio against time under<br />

conditions where Eq. (15.7) holds in order to determine k1. The reverse rate constant k−1<br />

may either be determined analogously, or from Eq. (15.5) once k1 is known.<br />

Note that for a first-order reaction, the time required for the reactant concentration to drop<br />

by some constant factor is a simple function <strong>of</strong> the rate constant. Thus, for instance, the half-<br />

life τ1/2, which is the time required such that [A]τ1/2<br />

= 1<br />

2 [A]0 for any starting concentration,<br />

may be determined from Eq. (15.8) to be k −1<br />

1 ln 2.<br />

Fragmentation is another possible unimolecular reaction. A fragmentation reaction may<br />

be expressed as<br />

A k1<br />

−−−⇀ ↽−−− B + C (15.9)<br />

k−1<br />

(in principle, fragmentations involving more than two products all <strong>of</strong> which are produced<br />

simultaneously are possible, but examples are very rare). The rate for disappearance <strong>of</strong> A<br />

when in excess <strong>of</strong> its equilibrium value is<br />

− d[A]<br />

dt = k1[A] − k−1[B][C] (15.10)<br />

The only difference from an experimental viewpoint between Eqs. (15.6) and (15.10) is that<br />

Eqs. (15.7) and (15.8) can now be made to apply by ensuring that either one (or both) <strong>of</strong> B<br />

and C have vanishingly small concentrations over the course <strong>of</strong> the rate measurement.<br />

15.1.2 Bimolecular Reactions<br />

The opposite <strong>of</strong> a fragmentation reaction is a condensation reaction, i.e.,<br />

A + B k1<br />

−−−⇀ ↽−−− C (15.11)<br />

Note that in practice the abstract species A and B may themselves already be molecules<br />

or supermolecules formed from prior condensations, but simple probability arguments make<br />

condensation reactions simultaneously involving more than two species impossible under<br />

most sets <strong>of</strong> experimental conditions. The rate law associated with eq. 15.11 is<br />

k−1<br />

− d[A]<br />

dt = k1[A][B] − k−1[C] (15.12)<br />

where k1 is a second-order rate constant because it multiplies a set <strong>of</strong> concentrations whose<br />

exponents sum to 2. The simplest evaluation <strong>of</strong> k1 proceeds by arranging for a vanishingly

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