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In , disproportionation, sometimes called dismutation, is a in which one compound of intermediate converts to two compounds, one of higher and one of lower oxidation state.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. .Holleman, A. F.; Wiberg, E. "Inorganic Chemistry" Academic Press: San Diego, 2001. . The reverse of disproportionation, such as when a compound in an intermediate oxidation state is formed from precursors of lower and higher oxidation states, is called comproportionation, also known as symproportionation.

More generally, the term can be applied to any desymmetrizing reaction where two molecules of one type react to give one each of two different types:

This expanded definition is not limited to redox reactions, but also includes some molecular autoionization reactions, such as the self-ionization of water. In contrast, some authors use the term redistribution to refer to reactions of this type (in either direction) when only ligand exchange but no redox is involved and distinguish such processes from disproportionation and comproportionation.
For example, the Schlenk equilibrium

is an example of a redistribution reaction.


History
The first disproportionation reaction to be studied in detail was:

This was examined using by in 1788. In the Swedish version of his paper he called it söndring.Gadolin Johan (1788) K. Sv. Vet. Acad. Handl. 1788, 186-197.Gadolin Johan (1790) Crells Chem. Annalen 1790, I, 260-273.''


Examples
  • Mercury(I) chloride disproportionates upon UV-irradiation:
:

:

  • Desymmetrizing reactions are sometimes referred to as disproportionation, as illustrated by the thermal degradation of bicarbonate:
:
The oxidation numbers remain constant in this acid-base reaction.

  • Another variant on disproportionation is radical disproportionation, in which two radicals form an alkene and an alkane.
:2CH3-\underset{^\bullet}CH2 -> {H2C=CH2} + H3C-CH3

  • Disproportionation of sulfur intermediates by microorganisms is widely observed in sediments.
:
:
:

:
The chlorine reactant is in 0. In the products, the chlorine in the Cl ion has an oxidation number of −1, having been reduced, whereas the oxidation number of the chlorine in the ion is +5, indicating that it has been oxidized.

  • Decomposition of numerous interhalogen compounds involve disproportionation. undergoes a disproportionation reaction to form bromine trifluoride and in non-aqueous media:
:

:
The oxidation state of oxygen is − in the superoxide free radical anion, −1 in hydrogen peroxide and 0 in dioxygen.

  • In the Cannizzaro reaction, an is converted into an alcohol and a . In the related Tishchenko reaction, the organic redox reaction product is the corresponding . In the Kornblum–DeLaMare rearrangement, a peroxide is converted to a and an alcohol.

  • The disproportionation of hydrogen peroxide into water and oxygen catalysed by either or the enzyme :
:

  • In the Boudouard reaction, carbon monoxide disproportionates to carbon and . The reaction is for example used in the method for producing ; high-pressure disproportionates when catalysed on the surface of an iron particle:
:

:

  • In and , each of the 3 nitrogen atoms of these very energetic linear polyatomic species has an oxidation state of −. These unstable and highly compounds will disproportionate in to form gaseous nitrogen () and , or , depending on pH conditions, as it can be conveniently verified by means of the for nitrogen:

Under acidic conditions, hydrazoic acid disproportionates as:
:

Under neutral, or basic, conditions, the azide disproportionates as:
:

:

  • Dithionite also undergoes alkaline hydrolysis to and :
:

  • is prepared on a larger scale by oxidizing a cooled aqueous solution of with manganese dioxide:J. Meyer and W. Schramm, Z. Anorg. Chem., 132 (1923) 226. Cited in: A Comprehensive Treatise on Theoretical and Inorganic Chemistry, by J.W. Meller, John Wiley
and Sons, New York, Vol. XII, p. 225.
:


Polymer chemistry
In free-radical chain-growth polymerization, chain termination can occur by a disproportionation step in which a hydrogen atom is transferred from one growing chain molecule to another one, which produces two dead (non-growing) chains.
(1991). 9780216929807, Blackie.
: Chain—CH2–CHX + Chain—CH2–CHX → Chain—CH=CHX + Chain—CH2–CH2X

in which, Chain— represents the already formed polymer chain, and indicates a reactive free radical.


Biochemistry
In 1937, Hans Adolf Krebs, who discovered the citric acid cycle bearing his name, confirmed the anaerobic dismutation of into , and by certain bacteria according to the global reaction:

The dismutation of pyruvic acid in other small organic molecules (ethanol + CO2, or lactate and acetate, depending on the environmental conditions) is also an important step in fermentation reactions. Fermentation reactions can also be considered as disproportionation or dismutation biochemical reactions. Indeed, the and acceptor of electrons in the supplying the in these complex biochemical systems are the same organic molecules simultaneously acting as or .

Another example of biochemical dismutation reaction is the disproportionation of into and . Biochemical basis of mitochondrial acetaldehyde dismutation in Saccharomyces cerevisiae

While in respiration electrons are transferred from substrate () to an electron acceptor, in fermentation part of the substrate molecule itself accepts the electrons. Fermentation is therefore a type of disproportionation, and does not involve an overall change in of the substrate. Most of the fermentative substrates are organic molecules. However, a rare type of fermentation may also involve the disproportionation of inorganic compounds in certain sulfate-reducing bacteria.


Disproportionation of sulfur intermediates
Sulfur isotopes of sediments are often measured for studying environments in the Earth's past (). Disproportionation of sulfur intermediates, being one of the processes affecting sulfur isotopes of sediments, has drawn attention from for studying the conditions in the oceans in the past.

Sulfate-reducing bacteria fractionate sulfur isotopes as they take in and produce . Prior to 2010s, it was thought that sulfate reduction could fractionate sulfur isotopes up to 46 ‰ and fractionation larger than 46 ‰ recorded in sediments must be due to disproportionation of sulfur intermediates in the sediment. This view has changed since the 2010s. As substrates for disproportionation are limited by the product of sulfate reduction, the isotopic effect of disproportionation should be less than 16 ‰ in most sedimentary settings.

Disproportionation can be carried out by microorganisms obligated to disproportionation or microorganisms that can carry out sulfate reduction as well. Common substrates for disproportionation include elemental (), () and ().


Claus reaction: a comproportionation reaction
The is an example of comproportionation reaction (the inverse of disproportionation) involving () and () to produce elemental sulfur and as follows:

The Claus reaction is one of the chemical reactions involved in the used for the of in the plants and leading to the formation of elemental sulfur (), which is easier to store, transport, reuse when possible, and dispose of.


See also

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