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Tetrachloroethylene

Chemical compound

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Through Hydrocarbon, Michael Faraday and Chemist

Tetrachloroethylene is produced industrially by the chlorination or oxychlorination of hydrocarbons. Approximately a million tons of tetrachloroethylene are produced every year and the production amount is increasing every year, especially to be used in the production of HCFC and HFC refrigerants. It was first obtained from the thermal decomposition of hexachloroethane in 1820 by the English chemist-physicist Michael Faraday.

Tetrachloroethylene is more stable compared to other chlorinated solvents and similar compounds as it does not react easily, does not tend to polymerize and has lower toxicity. Inhalation of vapours may affect the central nervous system, causing drowsiness, numbness, hallucinations and loss of consciousness. Exposure to high concentrations may irritate the skin and respiratory tract. It has been suspected of causing cancer in humans, but the evidence is limited. It was classified as "group 2A - probably carcinogenic" by the International Agency for Research on Cancer in 1995 due to sufficient evidence in some experimental animals and limited evidence for humans. The majority of studies investigating people exposed to tetrachloroethylene in the workplace and the environment have not found relation between tetrachloroethylene and human cancers. It is considered an industrial organic pollutant and has caused groundwater pollution in the past due to improper disposal. Its use has been restricted in some regions due to its environmental impacts and possible effects on human health, and alternatives are being explored in sectors such as dry cleaning.

History and production

The English chemist Michael Faraday first synthesized tetrachloroethylene in 1820 by thermal decomposition of hexachloroethane:

Cl3C−CCl3 → Cl2C=CCl2 + Cl2

Tetrachloroethylene can be made by passing chloroform vapour through a red-hot tube, the side products include hexachlorobenzene and hexachloroethane, as reported in 1886.

Most tetrachloroethylene is produced by high-temperature chlorinolysis of light hydrocarbons. The method is related to Faraday's method since hexachloroethane is generated and thermally decomposes. Side products include carbon tetrachloride, hydrogen chloride, and hexachlorobutadiene.

Several other methods have been developed. When 1,2-dichloroethane is heated to 400 °C (752 °F; 673 K) with chlorine, tetrachloroethylene is produced:

ClCH2−CH2Cl + 3 Cl2 → Cl2C=CCl2 + 4 HCl

This reaction can be catalyzed by a mixture of potassium chloride and aluminium chloride or by activated carbon. Trichloroethylene is a major byproduct, which is separated by distillation.

Worldwide production was about 1 million metric tons (980,000 long tons; 1,100,000 short tons) in 1985. In the USA, annual production was 700 million pounds (310,000 long tons) by 1978.

Although in very small amounts, tetrachloroethylene occurs naturally in volcanoes along with trichloroethylene.

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