As a series of studies on the dissolution of sparingly soluble inorganic compound with a strongly acidic ion exchange resin (H-R), alkaline earth carbonate (MCO
3) compounds were chosen by considering from a viewpoint of bicarbonate formation as an intermediate. Experiments were carried out by batchwise addition of H-R and by continuous feeding of H-R suspension into an aqueous suspension containing MCO
3 powder such as 4MgCO
3·Mg (OH)
2·4H
2O (BMC), CaCO
3, SrCO
3, BaCO
3 and those binary mixtures.
The pH, specific conductivity (k : mS/cm) and dissolved amount of M
2+ ion against H-R (g) added were measured, and the results obtained were analyzed for the dissolution mechanism.
The results obtained were summerized as follows;
1) In an initial stage of H-R addition, increases in M
2+ concentration and k value were observed. Linear relationship between [M
2+] (mmol/l) and k, the correlation between the slop and equivalent ionic conductivity of M
2+ ion, and pH dependence on the stability of HCO
3- ion indicate the formation of bicarbonate compound, M (HCO
3)
2.
2MCO
3 + 2 (H-R) →M (HCO
3)
2 + M-R2
2) As more is added, secondary ion exchange reaction between M
2+ and H-R leads to decrease in [M
2+] and k with evolution of CO
2 gas.
M (HCO
3)
2 + 2 (H-R) →M-R2 + 2CO
2 + 2H
2O
3) In general, the reactivity to produce the bicarbonate is proportional to the solubility product, i.e. Mg (HCO
3)
2>> Ba (HCO
3)
2 > Ca (HCO
3)
2> Sr (HCO
3)
2; the result will be applied to a separation technique.
View full abstract