Many geological and technological processes depend on diffusion in cry
stalline silicates and oxides, but models of the dynamics of diffusion
have only rarely been based on relatively direct microscopic informat
ion on the rates and energetics of the hopping of cations from site to
site. Two-dimensional nuclear magnetic resonance (NMR) exchange spect
ra for lithium-6 in lithium orthosilicate (Li(4)SiO4) provided a detai
led picture of the hopping rates of Li+ ions among structurally distin
ct sites and helped to define the diffusion pathway. Rates and activat
ion energies depended measurably on site geometry, and bulk electrical
conductivity was accurately predicted.