An assessment of complex formation between aluminium and silicic acid in acidic solutions

Physics

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Scientific paper

The extent of the reaction A1 3+ + Si(OH) 4 AlOSi(OH) 3 2+ + H + has been assessed by measuring the shift in log[H + ] between solutions containing A1(ClO 4 ) 3 , HClO 4 , and NaClO 4 with and without added silicic acid. The observed shifts of 0.018-0.027 units are about one tenth of those predicted from the formation constant ( pK 110 = 1.07 ± 0.06) proposed for the monomeric aluminosilicate species by and (1992). An estimate of this formation constant on the basis of the shifts in log[H + ] ( pK 110 = 2.50 ± 0.05) indicates that the concentration of aluminosilicate species can be neglected in many natural waters.

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