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Essentials of Computational Chemistry

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372 10 THERMODYNAMIC PROPERTIES<br />

10.4.3 Isodesmic Equations<br />

An alternative method for computing heats (or free energies) <strong>of</strong> formation involves<br />

consideration <strong>of</strong> a balanced chemical equation, e.g.,<br />

mA + nB −−−→ rC + sD (10.34)<br />

whereA,B,C,andDaremoleculesandm, n, r, ands indicate the number <strong>of</strong> moles <strong>of</strong><br />

each in the balanced equation. The heat <strong>of</strong> reaction for a chemical transformation is defined<br />

as the difference between the heats <strong>of</strong> formation <strong>of</strong> the products and those <strong>of</strong> the reactants<br />

when these are defined relative to consistent standard states. For the reaction <strong>of</strong> Eq. (10.34),<br />

we would have<br />

H o<br />

o<br />

o<br />

rxn,298 = [rHo f,298 (C) + sHo f,298 (D)] − [mHf,298 (A) + nHf,298 (B)] (10.35)<br />

where we have arbitrarily selected 298 K as the temperature <strong>of</strong> interest. Note that the<br />

standard-state symbol on the heat <strong>of</strong> reaction (as opposed to the heats <strong>of</strong> formation) does not<br />

imply the use <strong>of</strong> elemental standard states to assign a zero <strong>of</strong> enthalpy. Because the reaction<br />

is balanced, the standards used to define the zeroes for the heats <strong>of</strong> formation must cancel<br />

out on the two sides <strong>of</strong> the equation. So it is equally valid to write<br />

H o<br />

rxn,298 = [rH298(C) + sH298(D)] − [mH298(A) + nH298(B)] (10.36)<br />

where H298 is the quantity typically addressed theoretically, i.e., the enthalpy relative to all<br />

nuclei and electrons infinitely separated and at rest.<br />

Ins<strong>of</strong>ar as the r.h.s. <strong>of</strong> Eq. (10.35) must then be equal to the r.h.s. <strong>of</strong> Eq. (10.36), if the<br />

experimental heats <strong>of</strong> formation for all but one <strong>of</strong> the species in Eq. (10.34) are known (say<br />

B), we may rearrange our equality to determine this quantity as<br />

H o<br />

f,298 (B) =−1<br />

n {[rH298(C) + sH298(D)] − [mH298(A) + nH298(B)]<br />

− [rH o<br />

f,298 (C) + sHo<br />

f,298<br />

o<br />

(D)] + mHf,298 (A)} (10.37)<br />

This technique at first seems rather cumbersome, since we must perforce compute H298 for<br />

four different species in this example, but it has one great advantage over the apparently<br />

simpler apriori calculation <strong>of</strong> a single heat <strong>of</strong> formation, and that is that the difficulty<br />

in computing heats <strong>of</strong> atomization can be avoided. As noted above, computed heats <strong>of</strong><br />

atomization tend to be highly inaccurate unless heroic levels <strong>of</strong> theory are employed, because<br />

the correlation energies for the electrons in the atoms and in the molecule are so enormously<br />

different. However, assuming experimental data are available, we may select our balanced<br />

chemical Eq. (10.34) in such a way that the various bonds on the left- and right-hand<br />

sides are essentially identical. That being the case, we would expect bond-by-bond errors<br />

in correlation energy to largely cancel in the computed heat <strong>of</strong> reaction (the top line on the

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