There are two main forms of the oxides of Carbon: Carbon
Monoxide (CO) and Carbon Dioxide
(CO2).
Carbon Monoxide
This is formed when carbon is burned
with a deficiency of oxygen. There is a formal triple bond thereby
completing the octet around each of the atoms, and this results
in formal charges of -1 for C and +1 for O, and the presence
of lone electron pairs on both atoms.
Carbon monoxide is a valuable ligand for the stabilization
of metals in low oxidation states, as it forms synergic
bonds. The lone pair on the C atom forms a σ-bond
to the metal, but the electrons in the d-orbitals on the metals
are delocalized into the antibonding π-orbitals
of the CO ligand by the formation of dπ(metal)-pπ(CO)
bonds. (This weakens the CO bond, and so the extent of backbonding
in a complex can often be obtained from vibrational spectroscpy,
which measures the wavenumber of the CO bond.)
This combination of σ-donor and
π-acceptor is the definition of synergic
bonding, and the main interaction is the acid-base interaction
between the electron donor metal and the electron acceptor CO
molecule. These interactions mean that the high electron
density on the metal in its low oxidation state is delocalized
over the CO ligands, and so the metal is stabilized. Examples
of metals in the 0 oxidation state are Ni(CO)4, Fe(CO)5,
and Mn2(CO)10. The role of CO in bonding
with transition metals is very important.
Carbon Dioxide
This contains two C=O double
bonds, which are each longer and have smaller force constants
than the bond in CO, reflecting the presence of a triple bond
in CO. It is formed by heating carbonates, giving CO2
and the metal oxide.
Carbon dioxide is the thermodynamically most stable oxide of
carbon, though in the presence of carbon an equilibrium is set
up, governed by the entropic favourability of the formation
of two molecules of CO(g) from one molecule of CO2(g).
Carbon dioxide is weakly acidic in aqueous solution, forming
Carbonic acid, H2CO3, but in alkaline
solution the basic hydrogencarbonate ion, HCO3-,
is formed.
Carbon Dioxide is one of the main gases contributing to the
Greenhouse effect. The CO2
in the atmosphere allows visible light to pass through to the
earth, but it absorbs the waves which are reradiated by the
earth at longer wavelengths, resulting in a gradual warming
of the earth.
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