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Essentials of Computational Chemistry

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11.4 STRENGTHS AND WEAKNESSES OF CONTINUUM SOLVATION MODELS 413<br />

One approach for reducing the errors associated with the prediction <strong>of</strong> pKa values is to<br />

employ an isodesmic reaction. To illustrate with a specific example, it may be very hard to<br />

correctly predict the free energy change for the aqueous reaction<br />

+<br />

NH3 F<br />

NH 2<br />

F<br />

+<br />

+<br />

H<br />

(11.26)<br />

However, if the theoretical target is instead the free energy change for the isodesmic equation<br />

+<br />

NH3 F<br />

+<br />

NH 2<br />

NH 2<br />

F<br />

+<br />

+<br />

NH3 (11.27)<br />

one may well expect this to be computed far more accurately, since errors in levels <strong>of</strong> theory<br />

should largely cancel from left to right. Provided experimental data are available for the<br />

unsubstituted case<br />

NH 2<br />

+<br />

+ H<br />

+<br />

NH3 (11.28)<br />

then the free energy change for Eq. (11.26) may be estimated from the difference between<br />

the computed value for Eq. (11.27) and the experimental value for Eq. (11.28). Chen and<br />

MacKerell (2000) have provided a more detailed demonstration <strong>of</strong> the utility <strong>of</strong> this approach<br />

for a series <strong>of</strong> substituted pyridines using a variety <strong>of</strong> different levels <strong>of</strong> theory for the gas<br />

phase and computed solvation free energies.<br />

An alternative approach for improving predicted pKa values has been suggested by Klicic<br />

et al. (2002), who developed functional-group-specific linear regression corrections for pKa<br />

values computed from a particular DFT SCRF PB formalism. Correction <strong>of</strong> the raw computed<br />

pKas increases the model’s accuracy to about 0.5 pK units for those acidic functional groups<br />

well represented in their parameterization set.<br />

11.4.1.2 Redox potentials<br />

Oxidation and reduction potentials in solution are also computed via reference to<br />

particular thermodynamic cycles as illustrated in Figure 11.10. In this case, however, the

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