A molecular dynamics simulation method for the first hydration shell e
xchange kinetics is described and is illustrated for Na+ in water. The
exchange process is found to have a complex character. A calculated s
mall transmission coefficient, K approximate to 0.21, indicates that t
ransition-state theory seriously overestimates the rate. Grote-Hynes t
heory is unsuccessful in accounting for the kappa value. This is trace
d to trajectory mechanistic aspects for which the theory's assumptions
break down. Inclusion of anharmonicity via the theory of Voth provide
s an improved estimate.