The dissolution of soda lime silicate glass was studied in sodium bera
te buffer solutions (pH 8.1) containing varying concentrations of Mg.
The experimental data were expressed in terms of the equation Q=kt(alp
ha). In the absence of Mg, at pH 8.1, alpha was found to be I and chan
ging the concentration of Na in the solution did not influence a Howev
er, Na concentration did alter the rate constant (k). The higher the N
a concentration in the buffer the faster the dissolution. Under condit
ions of constant concentration of sodium in the buffet; increasing Mg
concentrations in the leachant reduced the glass leach rate and change
d the kinetics of glass leaching. At the lower Mg concentration range,
alpha approximate to 1, the leach rates are high; at the higher Mg co
ncentration range, alpha approximate to 0.5, the leach rates are low.