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Valence-Bond Theory
The Valence-Bond (Heitler-London) wavefunction for H2 is
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(38) |
Compare it to the molecular orbital wavefunction
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(39) |
We see that the VB wavefunction likes to have one electron near A
and one electron near B, whereas the MO wavefunction allows the possibility
for 2 electrons on A. The VB wavefunction will therefore describe the dissociation
of H2 into H+H, unlike the MO wavefunction. We say that the
VB wavefunction has covalent structures and the MO wavefunction has covelent
and ionic structures.
We also introduce the concept of hybrid orbitals, particularly relevant
for the C atom where the 2s and 2p orbitals lie close in energy. In particular
sp3 orbitals, defined as
Each hybrid orbital points towards one of the corners of the cube.
Hence one can write down a VB wavefunction for CH4:
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(44) |
and even for H2O
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(45) |
In this case there are two electrons in each of the sp3
orbitals
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which constitute the lone pairs, or `rabbit ears'.
VB theory predates MO theory. It gives a more pleasing description
because it maintains the atomic nature of the atoms in a molecule. However
it is much more difficult to work with, because atomic orbitals on different
atoms are not orthogonal, whereas molecular orbitals being eigenfunctions,
are orthogonal. The essential difference between VB and MO is that the
former is a localised picture (ie atomic) and the latter is a delocalised
picture (electrons shared between atoms).
But it is important to realise that although the MO picture gives delocalised
orbitals it is possible to construct linear combinations of them (eq
)
which do not change the electron density or the wavefunction, and become
localised. In H2CO, instead of having the a1
and b2 bonding CH2 orbitals, doing the above
constructs two localised orbitals, one along each CH bond. Of course they
no longer carry a symmetry label, but symmetry has been used to construct
them. The organic chemistry interpretations use such localised orbitals,
and computer programs can construct localised orbitals at the end of calculations..
However, because the MO wavefunction is a determinant, it is possible
to add and subtract rows (ie orbitals) to construct functions which are
localised.
Next: Symmetry
Up: Contents
- Previous: The
Equations for the orbitals
Nicholas Handy
1998-09-23