|Preferred IUPAC name
|3D model (Jmol)||Interactive image|
|Molar mass||62.13 g·mol−1|
|Density||0.846 g cm−3|
|Melting point||−98 °C; −145 °F; 175 K|
|Boiling point||35 to 41 °C; 95 to 106 °F; 308 to 314 K|
|Vapor pressure||53.7 kPa (at 20 °C)|
Refractive index (nD)
Std enthalpy of
|-66.9--63.9 kJ mol−1|
Std enthalpy of
|-2.1818--2.1812 MJ mol−1|
|Safety data sheet||osha.gov|
|GHS signal word||DANGER|
|H225, H315, H318, H335|
|P210, P261, P280, P305+351+338|
EU classification (DSD)
|R-phrases||R11, R22, R37/38, R41|
|S-phrases||S7, S9, S16, S26, S29, S33, S36/39|
|Flash point||−36 °C (−33 °F; 237 K)|
|206 °C (403 °F; 479 K)|
|Dimethyl ether (dimethyl oxide)
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
|what is ?)(|
Dimethyl sulfide (DMS) or methylthiomethane is an organosulfur compound with the formula (CH3)2S. Dimethyl sulfide is a water-insoluble flammable liquid that boils at 37 °C (99 °F) and has a characteristic disagreeable odor. It is a component of the smell produced from cooking of certain vegetables, notably maize, cabbage, beetroot and seafoods. It is also an indication of bacterial contamination in malt production and brewing. It is a breakdown product of dimethylsulfoniopropionate (DMSP), and is also produced by the bacterial metabolism of methanethiol.
DMS originates primarily from DMSP, a major secondary metabolite in some marine algae. DMS is the most abundant biological sulfur compound emitted to the atmosphere. Emission occurs over the oceans by phytoplankton. DMS is also produced naturally by bacterial transformation of dimethyl sulfoxide (DMSO) waste that is disposed of into sewers, where it can cause environmental odor problems.
DMS is oxidized in the marine atmosphere to various sulfur-containing compounds, such as sulfur dioxide, dimethyl sulfoxide (DMSO), dimethyl sulfone, methanesulfonic acid and sulfuric acid. Among these compounds, sulfuric acid has the potential to create new aerosols which act as cloud condensation nuclei. Through this interaction with cloud formation, the massive production of atmospheric DMS over the oceans may have a significant impact on the Earth's climate. The CLAW hypothesis suggests that in this manner DMS may play a role in planetary homeostasis.
Marine phytoplankton also produce dimethyl sulfide, and DMS is also produced by bacterial cleavage of extracellular DMSP. DMS has been characterized as the "smell of the sea", though it would be more accurate to say that DMS is a component of the smell of the sea, others being chemical derivatives of DMS, such as oxides, and yet others being algal pheromones such as dictyopterenes.
Dimethyl sulfide, dimethyl disulfide, and dimethyl trisulfide have been found among the volatiles given off by the fly-attracting plant known as dead-horse arum (Helicodiceros muscivorus). Those compounds are components of an odor like rotting meat, which attracts various pollinators that feed on carrion, such as many species of flies.
Physiology of dimethyl sulfide
Dimethyl sulfide has a characteristic smell commonly described as cabbage-like. It becomes highly disagreeable at even quite low concentrations. Some reports claim that DMS has a low olfactory threshold that varies from 0.02 to 0.1 ppm between different persons, but it has been suggested that the odor attributed to dimethyl sulfide may in fact be due to di- and polysulfides and thiol impurities, since the odor of dimethyl sulfide is much less disagreeable after it is freshly washed with saturated aqueous mercuric chloride. Dimethyl sulfide is also available as a food additive to impart a savory flavor; in such use, its concentration is low. Beetroot, asparagus, cabbage, corn and seafoods produce dimethyl sulfide when cooked.
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Dimethyl sulfide has been used in petroleum refining to pre-sulfide hydrodesulfurization catalysts, although other disulfides or polysulfides are preferred and easier to handle. It is used as a presulfiding agent to control the formation of coke and carbon monoxide in ethylene production. DMS is also used in a range of organic syntheses, including as a reducing agent in ozonolysis reactions. It also has a use as a food flavoring component. It can also be oxidized to dimethyl sulfoxide, (DMSO), which is an important industrial solvent.
The largest single commercial producer of DMS in the world is Gaylord Chemical Corporation, which until mid-2010 was a significant economic component of the paper industry of Bogalusa, Louisiana. The Bogalusa DMS plant operated continuously until this date, since its startup in 1961 by the now defunct Crown Zellerbach Corporation. The process technology practiced at the Bogalusa plant (alkylation of sulfur using Kraft lignin) is no longer in operation anywhere in the world. All DMS manufacturers currently use hydrocarbon-based feedstocks. Gaylord has no production of any kind at the old Louisiana site after opening its expanded DMS / Dimethyl sulfoxide operation in Tuscaloosa, Alabama in 2010.
ChevronPhillips Chemical Company is another major manufacturer of DMS. CP Chem produces this material at their facilities in Borger, Texas, USA and Tessenderlo, Belgium.
Dimethyl sulfide finds a niche use as a displaceable ligand in chloro(dimethyl sulfide)gold(I) and other coordination compounds. Dimethyl sulfide is also used in the ozonolysis of alkenes, reducing the intermediate trioxolane and oxidizing to DMSO.
- Coccolithophore, a marine unicellular planktonic photosynthetic algae, producer of DMS
- Dimethylsulfoniopropionate, a parent molecule of DMS and methanethiol in the oceans
- Dimethyl selenide, a selenium analogue of DMS produced by bacteria and phytoplankton
- Dimethyl telluride, a tellurium analogue of DMS
- Emiliania huxleyi, a coccolithophorid producing DMS
- Swern oxidation
- Gaia hypothesis
- Stefels, J.; Steinke, M.; Turner, S.; Malin, S.; Belviso, A. (2007). "Environmental constraints on the production and removal of the climatically active gas dimethylsulphide (DMS) and implications for ecosystem modelling". Biogeochemistry. 83 (1–3): 245–275. doi:10.1007/s10533-007-9091-5.
- Kappler, Ulrike; Schäfer, Hendrik (2014). "Chapter 11. Transformations of Dimethylsulfide". In Peter M.H. Kroneck and Martha E. Sosa Torres. The Metal-Driven Biogeochemistry of Gaseous Compounds in the Environment. Metal Ions in Life Sciences. 14. Springer. pp. 279–313. doi:10.1007/978-94-017-9269-1_11.
- Simpson, D.; Winiwarter, W.; Börjesson, G.; Cinderby, S.; Ferreiro, A.; Guenther, A.; Hewitt, C. N.; Janson, R.; Khalil, M. A. K.; Owen, S.; Pierce, T. E.; Puxbaum, H.; Shearer, M.; Skiba, U.; Steinbrecher, R.; Tarrasón, L.; Öquist, M. G. (1999). "Inventorying emissions from nature in Europe". Journal of Geophysical Research. 104 (D7): 8113–8152. Bibcode:1999JGR...104.8113S. doi:10.1029/98JD02747.
- Glindemann, D.; Novak, J.; Witherspoon, J. (2006). "Dimethyl Sulfoxide (DMSO) Waste Residues and Municipal Waste Water Odor by Dimethyl Sulfide (DMS): the North-East WPCP Plant of Philadelphia". Environmental Science and Technology. 40 (1): 202–207. Bibcode:2006EnST...40..202G. doi:10.1021/es051312a. PMID 16433352.
- Lucas, D. D.; Prinn, R. G. (2005). "Parametric sensitivity and uncertainty analysis of dimethylsulfide oxidation in the clear-sky remote marine boundary layer". Atmospheric Chemistry and Physics. 5 (6): 1505–1525. doi:10.5194/acp-5-1505-2005.
- Malin, G.; Turner, S. M.; Liss, P. S. (1992). "Sulfur: The plankton/climate connection". Journal of Phycology. 28 (5): 590–597. doi:10.1111/j.0022-3646.1992.00590.x.
- Gunson, J.R.; Spall, S.A.; Anderson, T.R.; Jones, A.; Totterdell, I.J.; Woodage, M.J. (1 April 2006). "Climate sensitivity to ocean dimethylsulphide emissions". Geophys. Res. Lett. 33, L07701. doi:10.1029/2005GL024982.
- Charlson, R. J.; Lovelock, J. E.; Andreae, M. O.; Warren, S. G. (1987). "Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate". Nature. 326 (6114): 655–661. Bibcode:1987Natur.326..655C. doi:10.1038/326655a0.
- "The Climate Gas You've Never Heard Of". Oceanus Magazine.
- "Dimethylsulfide production from dimethylsulfoniopropionate by a marine bacterium". Marine Ecology Progress Series. 110:95-103. 1994.
- "Cloning the smell of the seaside". University of East Anglia. 2007-02-02.
- Itoh, T.; Inoue, H.; Emoto, S. (2000). "Synthesis of Dictyopterene A: Optically Active Tributylstannylcyclopropane as a Chiral Synthon". Bulletin of the Chemical Society of Japan. 73 (2): 409–416. doi:10.1246/bcsj.73.409. ISSN 1348-0634.
- Stensmyr, M. C.; Urru, I.; Collu, I.; Celander, M.; Hansson, B. S.; Angioy, A.-M. (2002). "Rotting Smell of Dead-Horse Arum Florets". Nature. 420 (6916): 625–626. Bibcode:2002Natur.420..625S. doi:10.1038/420625a. PMID 12478279.
- Gahl, WA; Bernardini, I; Finkelstein, JD; Tangerman, A; Martin, JJ; Blom, HJ; Mullen, KD; Mudd, SH (February 1988). "Transsulfuration in an adult with hepatic methionine adenosyltransferase deficiency.". The Journal of Clinical Investigation. 81 (2): 390–7. doi:10.1172/JCI113331. PMC . PMID 3339126.
- Tangerman, A (Oct 15, 2009). "Measurement and biological significance of the volatile sulfur compounds hydrogen sulfide, methanethiol and dimethyl sulfide in various biological matrices.". Journal of Chromatography B. 877 (28): 3366–77. doi:10.1016/j.jchromb.2009.05.026. PMID 19505855.
- Tangerman, A; Winkel, E. G. (September 2007). "Intra- and extra-oral halitosis: finding of a new form of extra-oral blood-borne halitosis caused by dimethyl sulphide". J. Clin. Periodontol. 34 (9): 748–55. doi:10.1111/j.1600-051X.2007.01116.x. PMID 17716310.
- Tangerman, A; Winkel, EG (March 2008). "The portable gas chromatograph OralChroma™: a method of choice to detect oral and extra-oral halitosis.". Journal of breath research. 2 (1): 017010. doi:10.1088/1752-7155/2/1/017010. PMID 21386154.
- Tangerman, A; Winkel, EG (Mar 2, 2010). "Extra-oral halitosis: an overview.". Journal of breath research. 4 (1): 017003. Bibcode:2010JBR.....4a7003T. doi:10.1088/1752-7155/4/1/017003. PMID 21386205.
- Morton, T. H. (2000). "Archiving Odors". In Bhushan, N.; Rosenfeld, S. Of Molecules and Mind. Oxford: Oxford University Press. pp. 205–216.
- Parliment, T. H.; Kolor, M. G.; Maing, I. Y. (1977). "Identification of the Major Volatile Components of Cooked Beets". Journal of Food Science. 42 (6): 1592–1593. doi:10.1111/j.1365-2621.1977.tb08434.x.
- Ulrich, Detlef; Hoberg, Edelgard; Bittner, Thomas; Engewald, Werner; Meilchen, Kathrin (2001). "Contribution of volatile compounds to the flavor of cooked asparagus". Eur Food Res Technol. 213 (3): 200–204=. doi:10.1007/s002170100349.
- Roy, Kathrin-Maria (15 June 2000). "Thiols and Organic Sulfides". Ullmann's Encyclopedia of Industrial Chemistry: 8. doi:10.1002/14356007.a26_767. ISBN 3-527-30673-0. Retrieved 2003. Check date values in:
- "Locations". Gaylord Chemicals.
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