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A glutamic acid was buried in the hydrophobic core of staphylococcal nuclease by replacement of Val-66. Its pK(a) was measured with equilibrium thermodynamic methods. It was 4.3 units higher than the pK(a) of Glu in water. This increase was comparable to the DeltapK(a) of 4.9 units measured previously for a lysine buried at the same location. According to the Born formalism these DeltapK(a) are energetically equivalent to the transfer of a charged group from water to a medium of dielectric constant of 12. In contrast, the static dielectric constants of dry protein powders range from 2 to 4. In the crystallographic structure of the V66E mutant, a chain of water molecules was seen that hydrates the buried Glu-66 and links it with bulk solvent. The buried water molecules have never previously been detected in >20 structures of nuclease. The structure and the measured energetics constitute compelling and unprecedented experimental evidence that solvent penetration can contribute significantly to the high apparent polarizability inside proteins. To improve structure-based calculations of electrostatic effects with continuum methods, it will be necessary to learn to account quantitatively for the contributions by solvent penetration to dielectric effects in the protein interior.

To quantitate the contributions of the large hydrophobic residues in staphylococcal nuclease to the stability of its native state, single alanine and glycine substitutions were constructed by site-directed mutagenesis for each of the 11 leucine, 9 valine, 7 tyrosine, 5 isoleucine, 4 methionine, and 3 phenylalanine residues. In addition, each isoleucine was also mutated to valine. The resulting collection of 83 mutant nucleases was submitted to guanidine hydrochloride denaturation using intrinsic tryptophan fluorescence to monitor the equilibrium constant between the native and denatured states. From analysis of these data, each mutant protein's stability to reversible denaturation (delta GH2O) and sensitivity to guanidine hydrochloride (mGuHCl or d(delta G)/d[GuHCl]) were obtained. Four unexpected trends were observed. (1) A striking bipartite distribution was found for sites of mutations that altered mGuHCl: mutations that increased this parameter only involved residues that contribute side chains to the major hydrophobic core centered around a five-strand beta-barrel, whereas mutations that caused mGuHCl to decrease clustered around a second, smaller and less well-defined hydrophobic core. (2) The average stability loss for mutants in each of the six residue classes was 2-3 times greater than that estimated on the basis of the free energy of transfer of the hydrophobic side chain from water to n-octanol. (3) The magnitude of the stability loss on substituting Ala or Gly for a particular type of amino acid varied extensively among the different sites of its occurrence in nuclease, indicating that the environment surrounding a specific residue determines how large a stability contribution its side chain will make.(ABSTRACT TRUNCATED AT 250 WORDS)

Lys-66 and Glu-66, buried in the hydrophobic interior of staphylococcal nuclease by mutagenesis, titrate with pK(a) values of 5.7 and 8.8, respectively (Dwyer et al., Biophys. J. 79:1610-1620; García-Moreno E. et al., Biophys. Chem. 64:211-224). Continuum calculations with static structures reproduced the pK(a) values when the protein interior was treated with a dielectric constant (epsilon(in)) of 10. This high apparent polarizability can be rationalized in the case of Glu-66 in terms of internal water molecules, visible in crystallographic structures, hydrogen bonded to Glu-66. The water molecules are absent in structures with Lys-66; the high polarizability cannot be reconciled with the hydrophobic environment surrounding Lys-66. Equilibrium thermodynamic experiments showed that the Lys-66 mutant remained folded and native-like after ionization of the buried lysine. The high polarizability must therefore reflect water penetration, minor local structural rearrangement, or both. When in pK(a) calculations with continuum methods, the internal water molecules were treated explicitly, and allowed to relax in the field of the buried charged group, the pK(a) values of buried residues were reproduced with epsilon(in) in the range 4-5. The calculations show that internal waters can modulate pK(a) values of buried residues effectively, and they support the hypothesis that the buried Lys-66 is in contact with internal waters even though these are not seen crystallographically. When only the one or two innermost water molecules were treated explicitly, epsilon(in) of 5-7 reproduced the pK(a) values. These values of epsilon(in) > 4 imply that some conformational reorganization occurs concomitant with the ionization of the buried groups.

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