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On the Stability of the AlOSi(OH)32+ Complex in Aqueous Solution
Authors:Lorenzo?Spadini  author-information"  >  author-information__contact u-icon-before"  >  mailto:lorenzo.spadini@ujf-grenoble.fr"   title="  lorenzo.spadini@ujf-grenoble.fr"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author,Paul?W.?Schindler,Staffan?Sj?berg
Affiliation:1.Environmental Geochemistry Group, LGIT,University of Grenoble I,Grenoble Cedex 9,France;2.Department of Inorganic Chemistry,University of Bern,Bern,Switzerland;3.Department of Inorganic Chemistry,University of Ume?,Ume?,Sweden
Abstract:Summary The complexation of aluminium(III) and silicon(IV) was studied in a simplified seawater medium (0.6 M Na(Cl)) at 25 °C. The measurements were performed as potentiometric titrations using a hydrogen electrode with OH ions being generated coulometrically. The total concentrations of Si(IV) and Al(III) respectively [Si tot ] and [Al t ot], and −log[H +] were varied within the limits 0.3 < [Si tot ] < 2.5 mM, 0.5 < [Al tot ] < 2.6 mM, and 2 ≤ -log[H +] ≤ 4.2. Within these ranges of concentration, evidence is given for the formation of an AlSiO(OH) 3 2+ complex with a formation constant log β1,1-1 = −2.75 ± 0.1 defined by the reaction Al 3++Si (OH)4AlOSi(OH) 3 2+ +H + An extrapolation of this value to I=0 gives log β1,1-1 = −2.30. The calculated value of logK (Al 3++SiO(OH) 3 AlOSi(OH) 3 2+ ) = 6.72 (I=0.6 M) can be compared with corresponding constants for the formation of AlF 2+ and AlOH 2+ , which are equal to 6.16 and 8.20. Obviously, the stability of these Al(III) complexes decreases within the series OH >SiO(OH) 3  > F
Keywords:aluminium  equilibrium analysis  silica  solution chemistry  speciation
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