The first disproportionation reaction to be studied in detail was:

2 Sn²⁺ → Sn⁴⁺ + Sn

This was examined using tartrates by Johan Gadolin in 1788. In the Swedish version of his paper he called it söndring.^[4][5]

• Mercury(I) chloride disproportionates upon UV-irradiation:^{[clarification needed]}

Hg₂Cl₂ → HgCl₂ + Hg

• Phosphorous acid disproportionates upon heating to 200°C to give phosphoric acid and phosphine:

4 H₃PO₃ → 3 H₃PO₄ + PH₃

• Desymmetrizing reactions are sometimes referred to as disproportionation, as illustrated by the thermal degradation of bicarbonate:

2 HCO−3 → CO2−3 + H₂CO₃

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.

${\displaystyle {\ce {2CH3-{\underset {^{\bullet }}{C}}H2->{H2C=CH2}+H3C-CH3}}}$ 

• Disproportionation of sulfur intermediates by microorganisms is widely observed in sediments.^[6][7][8][9]

4 S⁰ + 4 H₂O → 3 H₂S + SO2−4 + 2 H⁺

3 S⁰ + 2 FeOOH → SO2−4 + 2 FeS + 2 H⁺

4 SO2−3 + 2 H⁺ → H₂S + SO2−4

• Chlorine gas reacts with concentrated sodium hydroxide to form sodium chloride, sodium chlorate and water. The ionic equation for this reaction is as follows:^[10]

3 Cl₂ + 6 OH⁻ → 5 Cl⁻ + ClO−3 + 3 H₂O

The chlorine reactant is in oxidation state 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 ClO−3 ion is +5, indicating that it has been oxidized.

• Decomposition of numerous interhalogen compounds involve disproportionation. Bromine fluoride undergoes a disproportionation reaction to form bromine trifluoride and bromine in non-aqueous media:^{[11][citation needed]}

3 BrF → BrF₃ + Br₂

• The dismutation of superoxide free radical to hydrogen peroxide and oxygen, catalysed in living systems by the enzyme superoxide dismutase:

2 O−2 + 2 H⁺ → H₂O₂ + O₂

The oxidation state of oxygen is −1⁄2 in the superoxide free radical anion, −1 in hydrogen peroxide and 0 in dioxygen.

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

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

2 H₂O₂ → 2 H₂O + O₂

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

2 CO → C + CO₂

• Nitrogen has oxidation state +4 in nitrogen dioxide, but when this compound reacts with water, it forms both nitric acid and nitrous acid, where nitrogen has oxidation states +5 and +3 respectively:

2 NO₂ + H₂O → HNO₃ + HNO₂

• In hydrazoic acid and sodium azide, each of the 3 nitrogen atoms of these very energetic linear polyatomic species has an oxidation state of −1⁄3. These unstable and highly toxic compounds will disproportionate in aqueous solution to form gaseous nitrogen (N₂) and ammonium ions, or ammonia, depending on pH conditions, as it can be conveniently verified by means of the Frost diagram for nitrogen:^[12]

Under acidic conditions, hydrazoic acid disproportionates as:

3 HN₃ + H⁺ → 4 N₂ + NH+4

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

3 N−3 + 3 H₂O → 4 N₂ + NH₃ + 3 OH⁻

• Dithionite undergoes acid hydrolysis to thiosulfate and bisulfite:^[13]

2 S₂O2−4 + H₂O → S₂O2−3 + 2 HSO−3

• Dithionite also undergoes alkaline hydrolysis to sulfite and sulfide:^[13]

3 Na₂S₂O₄ + 6 NaOH → 5 Na₂SO₃ + Na₂S + 3 H₂O

• Dithionate is prepared on a larger scale by oxidizing a cooled aqueous solution of sulfur dioxide with manganese dioxide:^{[14] [citation needed]}

2 MnO₂ + 3 SO₂ → MnS₂O₆ + MnSO₄

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.^[15]

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.

In 1937, Hans Adolf Krebs, who discovered the citric acid cycle bearing his name, confirmed the anaerobic dismutation of pyruvic acid into lactic acid, acetic acid and CO₂ by certain bacteria according to the global reaction:^[16]

2 CH₃COCOOH + H₂O → CH₃CH(OH)COOH + CH₃COOH + CO₂

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 donor and acceptor of electrons in the redox reactions supplying the chemical energy in these complex biochemical systems are the same organic molecules simultaneously acting as reductant or oxidant.

Another example of biochemical dismutation reaction is the disproportionation of acetaldehyde into ethanol and acetic acid.^[17]

While in respiration electrons are transferred from substrate (electron donor) 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 oxidation state of the substrate. Most of the fermentative substrates are organic molecules. However, a rare type of fermentation may also involve the disproportionation of inorganic sulfur compounds in certain sulfate-reducing bacteria.^[18]

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

Sulfate-reducing bacteria fractionate sulfur isotopes as they take in sulfate and produce sulfide. Prior to 2010s, it was thought that sulfate reduction could fractionate sulfur isotopes up to 46 ‰^[19] 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.^[20] 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.^[9]

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 sulfur (S₈), thiosulfate (S₂O2−3) and sulfite (SO2−3).^[9]

The Claus reaction is an example of comproportionation reaction (the inverse of disproportionation) involving hydrogen sulfide (H₂S) and sulfur dioxide (SO₂) to produce elemental sulfur and water as follows:

2 H₂S + SO₂ → 3 S + 2 H₂O

The Claus reaction is one of the chemical reactions involved in the Claus process used for the desulfurization of gases in the oil refinery plants and leading to the formation of solid elemental sulfur (S₈), which is easier to store, transport, reuse when possible, and dispose of.

• Dismutase
• Oxidoreductase
• Fermentation (biochemistry)