Jy. Tilquin et al., EFFECT OF BASICITY ON REDOX EQUILIBRIA IN SODIUM-SILICATE MELTS - AN IN-SITU ELECTROCHEMICAL INVESTIGATION, Journal of non-crystalline solids, 211(1-2), 1997, pp. 95-104
Redox ratios of chromium and antimony were directly measured at 1000 d
egrees C in sodium silicate melts by electrochemical methods. The redo
x ratios were found to increase while increasing the sodium oxide cont
ent, i.e. the liquid basicity. It was shown that the logarithm of the
redox ratio is a linear function of the logarithm of the sodium oxide
activity. Our results differ systematically from those obtained on que
nched samples. The results are discussed in the light of a thermodynam
ic model considering activities of molecular species. We suggest that,
when dissolved in silicate melts, multivalent ions form oxocomplexes
which are not fully discrete species because non-bridging oxygens can
intervene in their coordination sphere. We also concluded that there a
re rapid exchanges of oxygen atoms between the oxocomplexes and the so
lvent.