Compared
with univalent cationic diffusion, little is known about
the diffusion behavior of multivalent cations let alone the diffusion
of water in their first hydration shell. Here, we show that all published
translational diffusion coefficients of multivalent cations and water
measured at room temperature exhibit the same concentration dependence
when plotted as a function of the mass fraction of free water or of
hydrated solute. This behavior is held until only hydration and confined
water remain in solutions, wherein their concentration dependences
become cationic charge number-dependent. We also found that the iceberg
model can well describe the diffusions of multivalent cations with
decreasing water content until only hydration water is present. However, 1H-pulsed-field-gradient nuclear magnetic resonance measurements
confirmed that 1H in the first hydration shell diffuses
faster than Al3+ at room temperature and they have the
same diffusion coefficient only with decreasing the temperature down
to about 243 K. Therefore, iceberg model only equivalently describes
the effect of strong ion–water interaction on multivalent cationic
diffusion. These results will also help us reconceive our current
understanding of the pathway for hydration water affecting the diffusion
behavior of solutes with relatively weak solute–water interactions.