For the first time, self-diffusion of silicate species in a highly condensed silicate solution has been investigated. Self-diffusion coefficients in the range of 5.8×10 -11 m2 s -1 (for the Q 4 units) to 1.9×10 -10 m2 s -1 (for the Q 1 units) were obtained. Upper limits to chemical-exchange rates between silicate units have been determined. The exchange processes are not fast enough to average the self-diffusion coefficients between the various units on the timescale of the relevant stimulated echo experiment, though they may reduce the observed differences in D self .
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Bahlmann et al. (1997) studied this question.
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