Sparingly soluble inorganic salts such as BaSO
4 and CaC
2O
4⋅2H
2O are dissolved by soaking with an aqueous suspension containing a strongly acidic ion exchange resin, hydrogen form (H-R). The dissolution proceeds by the cation exchange reaction and can be traced by monitoring pH, specific conductivity (k, mS/cm) and ion (s) concentration (s) in the eluent.
For the sake of simple operation and for avoiding contamination by foreign ions, the dissolution method, different from the conventional method in which mineral acid is used, may offer a promising technique to elucidate the reaction mechanism including cement hydration.
The present work was undertaken to find a clue on the cement hydration chemistry and dealt with the dissolution process of portland cement powders. The dissolution was studied by batchwise addition of H-R to aqueous suspensions of cement with different degrees of hydration. Changes in pH and k during dissolution were compared for three kinds of cement, and analyzed quantitatively to discuss the dissolution based on the variations of dissolved amounts of constituent species for a rapid hardening cement (RHC).
The results obtained are summerized as follows;
(1) Dissolved Ca(OH)
2 is exchanged preferentially with H-R accompanying steep decrease in both k and Ca
2+. Sulfuric acid libereated from gypsum results in a predominant increase in k at the complete dissolution.
(2) Changes in pH, k, Ca
2+(%) and SO
42-(%) are terminated by the addition of H-R of about ten times weight as much as cement powder used, then, a considerable solubility of molybdate reactive silicic (MRS) acid is observed.
(3) Complete dissolution of unhydrated cement is confirmed by 100% dissolution of MRS acid, whereas the dissolution decreases with increasing degree of hydration. White silica gel precipitates for hydrated RHC (80°C, 72-280h) after the complete dissolution, indicating that all of Ca in C-S-H gel is also adsorbed by H-R as cement minerals.
(4) Equivalent ionic conductivity of the MRS acid is estimated as low as 3.6S⋅cm
2/mol. The result indicates that the MRS acid does not contribute to the increase in k during the dissolution as mentioned in (1).
(5) This method is a useful technique for monitoring hydration characteristics and chemical changes taking place during early hydration of cement.
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