Orbital hybridisation
In chemistry,
hybridisation (or
hybridization) is the concept of mixing atomic orbitals to form new
hybrid orbitals
suitable for the qualitative description of atomic bonding properties.
Hybridised orbitals are very useful in the explanation of the shape of molecular orbitals for molecules. It is an integral part of valence bond theory. Although sometimes taught together with the valence shell electron-pair repulsion (VSEPR) theory, valence bond and hybridization are in fact not related to the VSEPR model.
[1]
The hybrids are named based on the atomic orbitals that are involved
in the hybridization, and the geometries of the hybrids are also
reflective of those of the atomic-orbital contributors. For example, in
the methane (CH
4) a set of
sp3 orbitals are formed by mixing one
s and three
p orbitals on the carbon atom, and are directed towards the four hydrogen atoms which are located at the vertices of a regular tetrahedron.
Historical development
Chemist Linus Pauling first developed the hybridisation theory in order to explain the structure of molecules such as methane (CH
4).
[2]
This concept was developed for such simple chemical systems, but the
approach was later applied more widely, and today it is considered an
effective heuristic for rationalizing the structures of organic compounds.
For quantitative calculations of electronic structure and molecular properties, hybridisation theory is not as practical as molecular orbital theory. Problems with hybridisation are especially notable when the
d orbitals are involved in bonding, as in coordination chemistry and organometallic chemistry. Although hybridisation schemes in transition metal chemistry can be used, they are not generally as accurate.
Orbitals are a model representation of the behaviour of electrons
within molecules. In the case of simple hybridisation, this
approximation is based on atomic orbitals, similar to those obtained for
the hydrogen atom, the only atom for which an exact analytic solution
to its Schrödinger equation
is known. In heavier atoms, like carbon, nitrogen, and oxygen, the
atomic orbitals used are the 2s and 2p orbitals, similar to excited
state orbitals for hydrogen. Hybridised orbitals are assumed to be
mixtures of these atomic orbitals, superimposed on each other in various
proportions. The theory of hybridisation is most applicable under these
assumptions. It gives a simple orbital picture equivalent to Lewis structures. Hybridisation is not required to describe molecules, but for molecules made up from carbon, nitrogen and oxygen (and to a lesser extent, sulfur and phosphorus) the hybridisation theory/model makes the description much easier.
The hybridisation theory finds its use mainly in organic chemistry. Its explanation starts with the way bonding is organized in methane.
Types of hybridisation
sp3 hybrids
Hybridisation describes the bonding atoms from an atom's point of view. That is, for a tetrahedrally coordinated carbon (e.g., methane, CH
4),
the carbon should have 4 orbitals with the correct symmetry to bond to
the 4 hydrogen atoms. The problem with the existence of methane is now
this: carbon's ground state configuration is 1
s2 2
s2 2
px1 2
py1 or more easily read:
The valence bond theory would predict, based on the existence of two half-filled
p-type orbitals (the designations
px py or
pz are meaningless at this point, as they do not fill in any particular order), that C forms two covalent bonds, i.e., CH
2 (methylene). However, methylene is a very reactive molecule (see also: carbene) and cannot exist outside of a molecular system. Therefore, this theory alone cannot explain the existence of CH
4.
Furthermore, ground state orbitals cannot be used for bonding in CH
4. While exciting a 2
s electron into a 2
p
orbital would, in theory, allow for four bonds according to the valence
bond theory, (which has been proved experimentally correct for systems
like O
2) this would imply that the various bonds of CH
4 would have differing energies due to differing levels of orbital overlap. Once again, this has been experimentally disproved: any hydrogen can be removed from a carbon with equal ease.
To summarise, to explain the existence of CH
4 (and many other molecules) a method by which as many as 12 bonds (for transition metals) of equal strength (and therefore equal length) may be explained was required.
The first step in hybridisation is the excitation of one (or more)
electrons (we consider the carbon atom in methane, for simplicity of the
discussion):
The proton that forms the nucleus of a hydrogen atom attracts one of
the lower-energy valence electrons on carbon. This causes an excitation,
moving a 2s electron into a 2p orbital. This, however, increases the
influence of the carbon nucleus on the valence electrons by increasing
the effective core potential (the amount of charge the nucleus exerts on
a given electron = Charge of Core − Charge of all electrons closer to
the nucleus). The effective core potential is also known as the
effective nuclear charge, or Z
eff.
The solution to the Schrödinger equation for this configuration is a
linear combination of the s and p wave functions, or orbitals, known as a
hybridized orbital.
[3]
In the case of carbon attempting to bond with four hydrogens, four
valence-shell orbitals are required. (Core orbitals are almost never
involved in bonding.) Therefore, the 2
s orbital "mixes" with the three 2
p orbitals to form four
sp3 hybrids (read as
s-p-three). See graphical summary below.
becomes
In CH
4, four
sp3 hybridised orbitals are overlapped by hydrogen's 1
s orbital, yielding four σ (sigma) bonds (that is, four single covalent bonds). The four bonds are of the same length and strength. This theory fits our requirements.
translates into
An alternative view is: View the carbon as the C
4− anion. In this case all the orbitals on the carbon are filled:
If we now recombine these orbitals with the empty
s-orbitals of 4 hydrogens (4 protons, H
+)
and then allow maximum separation between the 4 hydrogens (i.e.,
tetrahedral surrounding of the carbon), we see that at any orientation
of the
p-orbitals, a single hydrogen has an overlap of 25% with the
s-orbital of the C, and a total of 75% of overlap with the 3
p-orbitals (see that the relative percentages are the same as the character of the respective orbital in an
sp3-hybridisation model, 25%
s- and 75%
p-character).
According to the orbital hybridisation theory, the valence electrons in methane should be equal in energy but its photoelectron spectrum
[4] shows two bands, one at 12.7 eV
(one electron pair) and one at 23 eV (three electron pairs). This
apparent inconsistency can be explained when one considers additional
orbital mixing taking place when the
sp3 orbitals mix with the 4 hydrogen orbitals.
sp2 hybrids
Other carbon based compounds and other molecules may be explained in a similar way as methane. Take, for example, ethene (C
2H
4). Ethene has a double bond between the carbons.
For this molecule, carbon will
sp2 hybridise, because one π (pi) bond is required for the double bond between the carbons, and only three σ bonds are formed per carbon atom. In
sp2 hybridisation the 2
s orbital is mixed with only two of the three available 2
p orbitals:
forming a total of 3
sp2 orbitals with one p-orbital remaining. In ethylene (ethene) the two carbon atoms form a σ bond by overlapping two
sp2 orbitals and each carbon atom forms two covalent bonds with hydrogen by
s–
sp2 overlap all with 120° angles. The π bond between the carbon atoms perpendicular to the molecular plane is formed by 2
p–2
p overlap. The hydrogen–carbon bonds are all of equal strength and length, which agrees with experimental data.
The amount of
p-character is not restricted to integer values; i.e., hybridisations like
sp2.5
are also readily described. In this case the geometries are somewhat
distorted from the ideally hybridised picture. For example, as stated in
Bent's rule, a bond tends to have higher
p-character when directed toward a more electronegative substituent.
sp hybrids
A schematic presentation of hybrid orbitals sp
The chemical bonding in compounds such as alkynes with triple bonds is explained by
sp hybridization.
In this model, the 2
s orbital mixes with only one of the three
p-orbitals resulting in two
sp orbitals and two remaining unchanged
p orbitals. The chemical bonding in acetylene (ethyne) (C
2H
2) consists of
sp–
sp overlap between the two carbon atoms forming a σ bond and two additional π bonds formed by
p–
p overlap. Each carbon also bonds to hydrogen in a sigma
s–
sp overlap at 180° angles.
Hybridisation and molecule shape
Hybridisation, along with the VSEPR theory, helps to explain molecule shape:
- AX1 (e.g., LiH): no hybridisation; trivially linear shape
- AX2 (e.g., BeCl2): sp hybridisation; linear or digonal shape; bond angles are cos−1(−1) = 180°
- AX3 (e.g., BCl3): sp2 hybridisation; trigonal planar shape; bond angles are cos−1(−1/2) = 120°
- AX2E (e.g., GeF2): bent / V shape, < 120°
- AX4 (e.g., CCl4): sp3 hybridisation; tetrahedral shape; bond angles are cos−1(−1/3) ≈ 109.5°
- AX3E (e.g.,NH3): trigonal pyramidal, 107°
(Note: The existence of a lone pair of electrons distorts bond angles
slightly due to increased s-orbital character in the lone pair and
increased p-orbital character in the orbitals used to make the bond
pairs. It is not due to increased electron repulsion which is a very
common misconception.[citation needed])
- AX5 (e.g., PCl5): sp3d hybridisation; trigonal bipyramidal shape
- AX6 (e.g., SF6): sp3d2 hybridisation; octahedral (or square bipyramidal) shape
This holds if there are no lone electron pairs on the central atom. If there are, they should be counted in the X
i number, but bond angles become smaller due to increased repulsion. For example, in water (H
2O), the oxygen
atom has two bonds with H and two lone electron pairs (as can be seen
with the valence bond theory as well from the electronic configuration
of oxygen), which means there are four such 'elements' on O. The model
molecule is, then, AX
2E
2:
sp3 hybridisation is utilized, and the electron arrangement of H
2O
is tetrahedral. This agrees with the experimentally-determined shape
for water, a non-linear, bent structure, with a bond angle of 104.5
degrees (the two lone-pairs are not visible).
In general, for an atom with s and p orbitals forming hybrids h
i and h
j with included angle
, the following holds: 1 +
ij cos(
) = 0. The p-to-s ratio for hybrid i is
i2, and for hybrid j it is
j2. In the special case of equivalent hybrids on the same atom, again with included angle
, the equation reduces to just 1 +
2 cos(
) = 0. For example, BH
3 has a trigonal planar geometry, three 120° bond angles, three equivalent hybrids about the boron atom, and thus 1 +
2 cos(
) = 0 becomes 1 +
2 cos(120°) = 0, giving
2 = 2 for the p-to-s ratio. In other words, sp
2 hybrids, just as expected from the list above.
Explanation of the shape of water
Commonly, the hybridization of the oxygen in water is described as sp
3 following the guidelines of VSEPR and the tetrahedral electron geometry it implies.
[5] In order for this to be true, the two electron pairs would be in equal-energy, symmetrical, sp
3 hybridised orbitals (two electron-pairs and two hydrogen atoms making the tetrahedron). However, molecular orbitals calculations give orbitals which reflect the symmetry of the molecule.
[6] One of the two lone pairs is in a pure p-type orbital, with its electron density perpendicular to the H-O-H framework.
[6] The other lone pair is an orbital that is close to an sp
2-type orbital that is in the same plane as the H-O-H bonding. It is not a purely sp
2-type orbital, but is extra rich in s-character.
[6] Photoelectron spectra confirm the presence of two different energies for the nonbonded electrons.
[7]
In contrast, the orbitals used to make the O-H bonds are close to sp
2 hybrids, but are extra p-rich.
[8]
However, molecular orbital theory does not give two equivalent bonds,
but two delocalised orbitals which are in-phase and out-of-phase
combinations of the H-O bond orbitals.
[6]
It has been argued that it is this change in the mixing of the orbitals
that is responsible for the compression of the H-O-H angle down to the
experimental 104.5 degrees, not some change in the repulsion of
electrons.
[8] However, if the molecular orbitals are localised, leaving the total wave function unaltered, one obtains two equivalent lone pairs and two equivalent bonds.
[9]
An accurate prediction of the bond angle requires however that
polarisation d functions be added to the molecular orbital calculation.
[10]
Thus while VSEPR and its application to hybridisation predicts the
correct atomic framework for water, it may do so for the wrong reason.
Controversy regarding d-orbital participation
Hybridisation theory has failed in a few aspects, notably in
explaining the energy considerations for the involvement of d-orbitals
in chemical bonding (See above for sp
3d and sp
3d
2
hybridisation). This can be well-explained by means of an example.
Consider, for instance, how the theory in question accounts for the
bonding in phosphorus pentachloride (PCl
5).
The d-orbitals are large, comparatively distant from the nucleus and
high in energy. Radial distances of orbitals from the nucleus seem to
reveal that d-orbitals are far too high in energy to 'mix' with s- and
p-orbitals. 3s – 0.47, 3p – 0.55, 3d – 2.4 (in angstroms). Thus, at first glance, sp
3d hybridisation seems improbable.
However, a closer examination of the factors that affect orbital size (and energy) reveals more. Formal charge on the central atom is one such factor, and it is obvious that the P atom in PCl
5
carries quite a large partial positive charge. Thus the 3d orbital
contracts in size to such an extent that hybridisation with s and p
orbitals may occur. Further, note the cases in which d-orbital
participation was proposed in hybridisation: SF
6(sulfur hexafluoride), IF
7, XeF
6; in all these molecules, the central atom is surrounded by the highly electronegative fluorine
atom, thus making hybridisation probable among s, p and d orbitals. A
further study reveals that orbital size also depends on the number of
electrons occupying it. And, even further, coupling of d orbital
electrons also results in contraction, albeit to a lesser extent.
The molecular orbital theory, however, offers a clearer insight into the bonding in these molecules.
Hybridisation theory vs. MO theory
Hybridisation theory is an integral part of organic chemistry and in general discussed together with molecular orbital theory
in advanced organic chemistry textbooks although for different reasons.
One textbook notes that for drawing reaction mechanisms sometimes a
classical bonding picture is needed with two atoms sharing two
electrons.
[11]
It also comments that predicting bond angles in methane with MO theory
is not straightforward. Another textbook treats hybridisation theory
when explaining bonding in alkenes
[12] and a third
[13] uses MO theory to explain bonding in hydrogen but hybridisation theory for methane.
Although the language and pictures arising from hybridisation theory, more widely known as valence bond theory, remain widespread in synthetic organic chemistry,
this qualitative view of bonding has been largely superseded by
molecular orbital theory when a more detailed analysis is required.
Advanced texts often stress that while hybrid orbital theory is still
useful for problems requiring a rough approximation, it provides an
incomplete picture that cannot account for many chemical phenomena.
[14][15]
One specific problem with hybridisation is that it incorrectly predicts
the photoelectron spectra of many molecules, including such fundamental
species such as methane and water. From a pedagogical perspective,
hybridisation approach tends to over-emphasize localisation of bonding
electrons and does not effectively embrace molecular symmetry as does MO theory.
Bonding orbitals formed from hybrid atomic orbitals may be considered as localized molecular orbitals,
which can be formed from the delocalized orbitals of molecular orbital
theory by an appropriate mathematical transformation. For molecules with
a closed electron shell in the ground state, this transformation of the
orbitals leaves the total many-electron wave function unchanged. The
hybrid orbital description of the ground state is therefore
equivalent
to the delocalized orbital description for explaining the ground state
total energy and electron density, as well as the molecular geometry
which corresponds to the minimum value of the total energy.
There is no such equivalence, however, for ionized or excited states
with open electron shells. Hybrid orbitals cannot therefore be used to
interpret photoelectron spectra, which measure the energies of ionized
states, identified with delocalized orbital energies using Koopmans' theorem. Nor can they be used to interpret UV-visible spectra which correspond to electronic transitions between delocalized orbitals.
See also
- Linear combination of atomic orbitals molecular orbital method
- MO diagrams
References
- ^ Gillespie, R.J. (2004), "Teaching molecular geometry with the VSEPR model", Journal of Chemical Education 81 (3): 298–304, DOI:10.1021/ed081p298
- ^ Pauling,
L. (1931), "The nature of the chemical bond. Application of results
obtained from the quantum mechanics and from a theory of paramagnetic
susceptibility to the structure of molecules", Journal of the American Chemical Society 53 (4): 1367–1400, DOI:10.1021/ja01355a027
- ^ McMurray, J. (1995). Chemistry Annotated Instructors Edition (4th ed.). Prentice Hall. p. 272. ISBN 0-13-140221-8
- ^ photo electron spectrum of methane 1 photo electron spectrum of methane 2
- ^ Petrucci
R.H., Harwood W.S. and Herring F.G. "General Chemistry. Principles and
Modern Applications" (Prentice-Hall 8th edn 2002) p.441
- ^ a b c d Levine I.N. “Quantum chemistry” (4th edn, Prentice-Hall) p.470-2
- ^ Levine p.475
- ^ a b Laing, Michael J. Chem. Educ. (1987) 64, 124–128 "No rabbit ears on water. The structure of the water molecule: What should we tell the students?"
- ^ Levine p.481-2
- ^ A.Szabo
and N.S.Ostlund, "Modern Quantum Chemistry: Introduction to Advanced
Electronic Structure Theory" (MacMillan 1982) p.202 quotes calculated
bond angles of 111.2° for a 4-31G basis set without d functions, and 105.5° for a 6-31G* basis set with d functions, compared to the expermimental 104.5°.
- ^ Clayden, Jonathan; Greeves, Nick; Warren, Stuart; Wothers, Peter (2001). Organic Chemistry (1st ed.). Oxford University Press. p. 105. ISBN 978-0-19-850346-0.
- ^ Organic Chemistry, Third Edition Marye Anne Fox James K. Whitesell 2003 ISBN 978-0-7637-3586-9
- ^ Organic Chemistry 3rd Ed. 2001 Paula Yurkanis Bruice ISBN 0-13-017858-6
- ^ G. L. Miessler and D. A. Tarr “Inorganic Chemistry” 3rd Ed, Pearson/Prentice Hall publisher, 2003. ISBN 0-13-035471-6.
- ^ Shriver,
D. F.; Atkins, P. W.; Overton, T. L.; Rourke, J. P.; Weller, M. T.;
Armstrong, F. A. “Inorganic Chemistry” W. H. Freeman, New York, 2006. ISBN 0-7167-4878-9.