“…Results are described in detail in ref 79. This has indeed been demonstrated: bulk viscosity can be directly calculated from species exchange rates measured by NMR. 79 The exchange among Si sites is mirrored by that among 0 sites: 170 NMR has shown that bridging and nonbridging oxygens interchange at rates comparable to that of the Si sites.89 This kind of study has been extended to temperatures just above T" by two dimensional exchange spectroscopy. 90 This kina of structural exchange is in marked contrast to the behavior of a mixture of molten alkali nitrate and sulfate, where no exchange among the oxygens bound to these molecular anions was observed.1 A few relaxation time studies of network forming species in oxide glasses and liquids have been made, with some early high-temperature relaxation time results, on UB in B203.91'92 "Si data in glassy and liquid silicates have proven difficult to understand in complete detail, in part because of the sensitivity to paramagnetic impurities.79,88 However, relaxation mechanisms change abruptly near the bulk glass transition temperature, probably because of the structural mobility that begins at that point.79,88 Apparent activation energies in the liquid region are similar to those for viscosity.…”