The enthalpies of hydration of d-metal complexes
The trend in observed hydration enthalpies of the
hexa-aquo transition metal complexes of the first row transition
metals can be explained in terms of the ligand field stabilization
energy.
|
 |
The enthalpies
of hydration for [M(H2O)6]2+
The arrow denotes the LFSE for the hexa-aquo VII complex. |
In the plot, the dashed line is the enthalpy of
hydration expected on the basis of its being proportional to
z2/r, where z is the effective nuclear charge and
r is the ionic radius. The number of d electrons changes as
the period is crossed, and the enthalpy of hydration changes
also.
The extra hydration enthalpy of some of the complexes compared
to that predicted on a purely electrostatic basis corresponds
to the ligand field stabilization energy for that configuration.
On going from the gas phase to the condensed phase, the
symmetry of the ion changes from spherical in the free ion
to octahedral in the complex, and so the energies of the d-orbitals
split, and the number of electrons determines the total LFSE
that arises. Hence certain configurations have extra stability
in the octahedral hexa-aquo complex.
In [Mn(H2O)6]2+,
there are 5 d-electrons, and so zero LFSE, and we can see that
the hydration energy is that predicted on a purely electrostatic
basis.
The structure of Spinels
Spinels are metallic oxides with the formula AB2O4,
such as Fe3O4, Co3O4,
and Mn3O4. They have the structure of spinel
itself, MgAl2O4 (Mg = A, Al = B), which
is based on a face-centered cubic array of oxide anions with A
cations occupying one eighth of the tetrahedral holes and B cations
occupying half the octahedral holes.
However, some spinels crystallize with the inverse
spinel structure B(AB)O4. The reason for this
is the variation in the ligand field stabilization energy between
the two arrangements.
If we consider AB2O4, we see
that the stoichiometry of the compound requires that one of the
cations (A) have a charge of +2, and the other two cations (B)
have a charge of +3. The normal spinel has the A cations in tetrahedral
holes and the B cations in the octahedral holes, whereas the inverse
spinel has the A cations in octahedral holes, and the B cations
with half in octahedral holes and half in tetrahedral holes. We
investigate why this is so by considering the structure of Fe3O4.
| The Structure
of Fe3O4 |
| Normal Spinel |
Inverse Spinel |
| Fe2+[Fe3+]2O4 |
Fe3+[Fe2+Fe3+]O4 |
| Fe (1): d6
in Td hole LFSE = 0 |
Fe (1): d5
in Td hole LFSE = +0.4Δt |
| Fe (2): d5
in Oh hole LFSE = -2Δo |
Fe (2): d6
in Oh hole LFSE = -2.4Δo |
| Fe (3): d5
in Oh hole LFSE = -2Δo |
Fe (3): d5
in Oh hole LFSE = -2Δo |
| Total LFSE =
(0) + (-2Δo) +
(-2Δo)
= -4Δo |
Total LFSE =
(+0.4Δt) + (-2.4Δo)
+ (-2Δo)
= -4Δo + 0.4(Δt
- Δo) |
Δt
< Δo, and the
ligands in the tetrahedral orientation are always in the
weak-field limit, and so the inverse spinel structure
has a greater ligand field stabilization energy than the
normal spinel structure. |
| So, Fe3O4
is predicted to have the inverse spinel structure, and
this is as observed. |
In general if the sum of the ligand field stabilization
energies for (A2+)tet(B3+)oct
is greater than those for (B3+)tet(A2+)oct,
then the normal spinel structure will be adopted, and vice versa.
The crystal structure adopted by a given compound is that
which has the largest lattice enthalpy, and so we can see
that the ligand field stabilization energy has an effect on
the value of the lattice enthalpies, with the LFSE being large
enough to change the lattice enthalpy so as to drive the conversion
of a spinel to an inverse spinel, as in the case of Fe3O4,
for example.
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