“…Figure 1B shows that the measured dissolution rate of all the fly ashes in this study decreases exponentially with the number of constraints, n c , for a given pH. 11,13,40 When the fly ash dissolution rates shown in Figure 1B are plotted along with additional dissolution rate data for glassy silica, quartz, and several aluminosilicate glasses including albite, jadeite, nepheline, and sodium silicate glass (denoted as "Natural" glass; see Figure 1C 18,35,36 )the exponential dependence of dissolution rate on n c is preserved § . It should be noted that decreases in dissolution rate generally correspond to lower concentrations of calcium in the fly ash, but this is not true in all cases.…”