Proton mobility is traditionally thought to be governed by water molec
ule rotation. Water rotation times from D2O NMR spin-lattice relaxatio
n measurements are compared with proton hopping times from mobility da
ta with and without subtraction of the estimated hydrodynamic mobility
. In the latter case the two data agree nicely at high temperatures. I
t is concluded that the hydrodynamic proton mobility is considerably s
maller than previously believed because H3O+ is nearly immobilized by
extra-strong hydrogen-bonds to first-shell water ligands, estimated to
be about 2 kcal/mol stronger than bulk hydrogen-bonds. Water rotation
is slower than proton hopping below 20 degrees C and has a hydrodynam
ic component to its activation energy. Therefore, proton mobility is n
ot governed by water rotation but rather both processes are controlled
by hydrogen-bond dynamics. Comparison with hydrogen-bond lifetimes fr
om depolarized light scattering suggests that two consecutive cleavage
events of ordinary hydrogen bonds constitute a single proton hop. Thi
s agrees with a recent molecular model for the Grotthuss mechanism.