Analytical motional models are described for the interpretation of NMR
cross relaxation between protein protons and water protons, treating
bulk water as a self-diffusing continuum. Using intermolecular dipolar
relaxation theory, scaling arguments, and numerical calculations, the
distance dependence of the cross-relaxation rate constant between the
protein proton and the first hydration shell is discussed for planar
and spherical surface geometries. It is found that differential effect
s between NOESY and ROESY rate constants depend strongly on geometrica
l factors and do not directly reflect residence times of individual wa
ter molecules on the protein surface. Restriction of water diffusion t
o a coarse lattice leads qualitatively to the same NMR relaxation beha
vior, but X-ray crystallography would display well-ordered water struc
ture, illustrating the complementary views of the two techniques on pr
otein hydration.