11462 J. Phys. Chem. A, Vol. 104, No. 49, 2000
Letters
to 1 atm, whereas the equilibrium constant is far too small to
allow direct Raman measurements of the hemiketal concentra-
tion.
namic results which we have presented, serve as an experimental
bench-mark against which to test both fundamental solvation
theories and semiempirical solvation modeling strategies.9,22-24
A further important feature of the results is the similarity of
the 1 atm ∆H° and ∆U° values, which also requires that ∆G°
and ∆A° must be the nearly equal.14 However, when the pressure
is increased to 2 GPa, the values of ∆H° and ∆U° (or ∆G° and
∆A°) diverge as a result of the increasing magnitude of P∆V°.
This behavior beautifully illustrates the importance of ∆V° in
dictating the pressure dependence of reaction thermodynamic
values. Although ∆V° typically plays a negligible role for reac-
tions carried out under ambient conditions, it may become a
dominant contribution to some high-pressure industrial pro-
cesses, or even for exotic biological processes occurring in deep
ocean hydrothermal vents or extraterrestrial environments.15,16
The difference between the liquid and gas-phase reaction
thermodynamic functions represents the solvent contribution to
the chemical equilibrium (see the last few columns of Table
1). The excess potential energy of reaction, ∆Ux, indicates that
the solvation energy of the reactants (acetone + methanol) and
product (hemiketal) differ by about 20 kJ/mol in THF at both
1 atm. and 2 GPa. The large excess entropy of reaction, ∆Sx,
implies that solvent structural rearrangement plays a significant
role in solvation thermodynamics (an effect which is difficult
to reproduce using dielectric continuum solvation models).17,18
Like ∆Ux and ∆Sx, the excess reaction volume, ∆Vx, is also
approximately pressure independent. The constancy of these
functions implies that there is little change in solvent structure
with pressure. On the other hand, because our experiments span
more than a 10 000-fold increase in pressure, the associated
change in P∆Vx produces dramatic changes in ∆Hx and ∆Gx.
A further interesting feature of the excess thermodynamic results
is the very small, and nearly pressure independent, value of the
excess Helmholtz free energy, ∆Ax. This implies a nearly perfect
cancellation of the large ∆Ux and T∆Sx, reminiscent of the well-
known enthalpy-entropy compensation phenomena.19-21 Our
results suggest that although both ∆Hx - T∆Sx and ∆Ux -
T∆Sx are nearly zero at 1 atm, only the latter cancellation
continues into the high-pressure regime, which may warrant a
theoretical reexamination of such compensation phenomena.
More generally, the sort of global excess reaction thermody-
Acknowledgment. This work was supported by the National
Science Foundation (CHE-9530595).
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