Wh. Casey et Bl. Phillips, Kinetics of oxygen exchange between sites in the GaO4Al12(OH)(24)(H2O)(12)(7+)(aq) molecule and aqueous solution, GEOCH COS A, 65(5), 2001, pp. 705-714
Rates of steady exchange of oxygens between bulk solution and sites in the
GaO4Al12(OH)(12)(7+)(aq) (GaAl12) aqueous complex were determined over the
temperature range of 301 to 317 K and 4.1 < pH < 4.9 using O-17-nuclear mag
netic resonance (NMR). The GaAl12 molecule, like the AlO4Al12(OH)(24)(H2O)(
12)(7+)(aq) (Al-13) molecule studied previously, has 12 equivalent bonded w
ater molecules (eta (1)-OH2 sites), two structurally distinct sets of 12 hy
droxyl bridges (mu (2)-OH; mu (2)-OH' sites), and four four-coordinated oxo
gropups (mu (4)-O sites).
The GaAl12 molecule is much less reactive than the Al-13 molecule, and this
decreased reactivity is not associated with any clear changes in the struc
tural chemistry at the sites of exchange. The rate coefficients for exchang
e of the water molecules bonded to the complex with bulk water are as follo
w: k(ex)(298) = 227(+/-40) s(-1), DeltaH(double dagger) = 63(+/-7) kJ mol(-
1), and DeltaS(double dagger) = 13(+/-21) J mol(-1) K-1. The rate at 298 K
is approximate to 5 times slower than the corresponding exchange reaction o
n the Al-13 molecule, but it falls within the range measured for dissolved
aluminum monomers. These data support our earlier speculation that rates of
exchange of eta (1)-OH2 sites at fully charged aluminum (hydr)oxide minera
l surfaces are similar to rates for aqueous aluminum complexes in acids.
The rates of isotopic exchange of the two hydroxyl bridges in the GaAl12 co
mplex differ from one another, as we also observed for the Al-13 complex, b
ut to a much smaller extent. Likewise, the activation parameters for exchan
ge at the two sites are much more similar to one another in the GaAl12 mole
cule than in the Al-13. The rate coefficients for exchange of the more reac
tive hydroxyl bridge are as follows: k(ex)(298) = 1.8(+/-0.1) . 10(-5) s(-1
), DeltaH(1)(double dagger) = 98(+/-3) kJ mol(-1), DeltaS(1)(double dagger)
= -8(+/-9) J mol(-1) K-1, and for the less labile bridge, they are k(ex)(2
98) = 4.1(+/-0.2) . 10(-7) s(-)1, with DeltaH(2)(double dagger) = 125(+/-4)
kJ mol(-1) and DeltaS(2)(double dagger) = 54(+/-12) J mol(-1) K-1. There i
s no strong pH dependence to rates. Copyright (C) 2001 Elsevier Science Ltd
.