The effect of pressure on the capture of a substrate alcohol by yeast alcoh
ol dehydrogenase is biphasic. Solvent isotope effects accompany both phases
and are expressed differently at different pressures. These differences al
low the extraction of an inverse intrinsic kinetic solvent isotope effect o
f 1.1 (i.e., V-D2O/K = 0.9) accompanying hydride transfer and an inverse eq
uilibrium solvent isotope effect of 2.6 (i.e., K-D2O(S) = 0.4) accompanying
the binding of nucleotide, NAD(+). The Value of the kinetic effect is cons
istent with a reactant-state E-NAD(+)-Zn-OH2 having a fractionation factor
of phi approximate to 0.5 for the zinc-bound water in conjunction with a tr
ansition-state proton exiting a low-barrier hydrogen bond with a fractionat
ion factor between 0.6 and 0.9. The value of the equilibrium effect is cons
istent with restrictions of torsional motions of multiple hydrogens of the
enzyme protein during the conformational change that accompanies the bindin
g of NAD(+). The absence of significant commitments to catalysis accompanyi
ng the kinetic solvent isotope effect means that this portion of the proton
transfer occurs in the same reactive step as hydride transfer in a concert
ed chemical mechanism. The success of this analysis suggests that future me
asurements of solvent isotope effects as a function of pressure, in the pre
sence of moderate commitments to catalysis, may yield precise estimates of
intrinsic solvent isotope effects that are not fully expressed on capture a
t atmospheric pressure.