Abstract

As part of ongoing studies to evaluate relationships between structure and rates of dissolution of silicate glasses in aqueous media, sodium borosilicate glasses of composition Na 2O·xB 2O 3·(3 − x)SiO 2, with x ≤ 1 (Na 2O/B 2O 3 ratio ≥ 1), were analyzed using deep-UV Raman spectroscopy. Results were quantified in terms of the fraction of SiO 4 tetrahedra with one non-bridging oxygen (Q 3) and then correlated with Na 2O and B 2O 3 content. The Q 3 fraction was found to increase with increasing Na 2O content, in agreement with studies on related glasses, and, as long as the value of x was not too high, this contributed to higher rates of dissolution in single pass flow-through testing. In contrast, dissolution rates were less strongly determined by the Q 3 fraction when the value of x was near unity, and appeared to grow larger upon further reduction of the Q 3 fraction. Results were interpreted to indicate the increasingly important role of network hydrolysis in the glass dissolution mechanism as the BO 4 tetrahedron replaces the Q 3 unit as the charge-compensating structure for Na + ions. Finally, the use of deep-UV Raman spectroscopy was found to be advantageous in studying finely powdered glasses in cases where visible Raman spectroscopy suffered from weak Raman scattering and fluorescence interference.

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