| Hydrogen sulfide |
|---|
 Hydrogen sulfide's geometry  Hydrogen sulfide |
| General | |
|---|---|
| Systematic name | Hydrogen sulfide, sulfane |
| Other names | Sulfuretted hydrogen sulfane sulfur hydride sour gas sulfurated hydrogen hydrosulfuric acid sewer gas stink damp |
| Molecular formula | H2S |
| Molar mass | 34.082 g/mol |
| Appearance | Colorless gas. |
| CAS number | |
| Properties |
|---|
| Density and phase | 1.363 g/L, gas. |
| Solubility in water | 0.25 g/100 mL (40°C) |
| Melting point | -82.30°C (190.85 K) |
| Boiling point | -60.28°C (212.87 K) |
| Acidity (p''K''a) | 6.89 19±2 (''See Text'') |
| Structure |
|---|
| Molecular shape | Bent. |
| Dipole moment | 0.97 D |
| Hazards |
|---|
| MSDS | External MSDS |
| Main hazards | Toxic, flammable. |
| NFPA 704 | |
| Flash point | -82.4 °C |
| R/S statement | R: , , S: , , , , , |
| RTECS number | MX1225000 |
| Supplementary data page |
|---|
Structure and properties | ''n'', É√r, etc. |
Thermodynamic data | Phase behaviour Solid, liquid, gas |
| Spectral data | UV, IR, NMR, MS |
| Related compounds |
|---|
| Inorganic derivatives | sodium sulfide sodium hydrosulfide |
| Organic derivatives | dimethyl sulfide |
| Related hydrogen compounds | water hydrogen selenide hydrogen telluride |
Except where noted otherwise, data are given for materials in their standard state (at 25°C, 100 kPa)
|
'Hydrogen sulfide' (hydrogen sulphide in
British English) is the
chemical compound with the
formula H
2S. This colorless,
toxic and flammable
gas is responsible for the foul odor of
rotten eggs and
flatulence. It often results from the
bacterial break down of organic matter in the absence of
oxygen, such as in
swamps and sewers (
anaerobic digestion). It also occurs in
volcanic gases,
natural gas and some well waters. The odor of H
2S is commonly misattributed to elemental
sulfur, which is in fact odorless. Hydrogen sulfide has numerous names, some of which are archaic (see Table).
Basic properties
Hydrogen sulfide is a
covalent hydride structurally related to
water (H
2O) since
oxygen and
sulfur occur in the same
periodic table group.
Hydrogen sulfide is weakly
acidic, dissociating in aqueous solution into hydrogen
cations H
+ and the
hydrosulfide anion HS
−:
::H
2S → HS
− + H
+
:::
''K''a = 1.3×10
−7 mol/L; p''K''
a = 6.89.
The
sulfide ion, S
2−, is known in the solid state but not in aqueous solution (''c.f.''
oxide). The second
dissociation constant of hydrogen sulfide is often stated to be around 10
−13, but it is now clear that this is an error caused by
oxidation of the sulfur in alkaline solution. The current best estimate for p''K''
a2 is 19±2.
[1]
Hydrogen sulfide reacts with many
metals cations to produce the corresponding metal
sulfides. Well-known examples are
silver sulfide (Ag
2S), the
tarnish that forms on
silver when exposed to the hydrogen sulfide of the atmosphere, and
cadmium sulfide (CdS), a
pigment also known as cadmium yellow.
Transition metal sulfides are characteristically insoluble, thus H
2S is commonly used to separate metal ions from aqueous solutions. (
Sulfides should not be confused with
sulfites or
sulfates, which contain the sulfite ion SO
32− and the sulfate ion SO
42−, respectively.)
Hydrogen sulfide is
corrosive and renders some
steels brittle, leading to
sulphide stress cracking — a concern especially for handling "
sour gas" and
sour crude oil in the
oil industry. Hydrogen sulfide burns to give the gas
sulfur dioxide, which is more familiar as the odor of a burnt match.
Occurrence

Deposit of sulphur on a rock, caused by volcanic gases
Small amounts of hydrogen sulfide occur in
crude petroleum but
natural gas can contain up to 28%.
Volcanoes and
hot springs emit some H
2S, where it probably arises via the
hydrolysis of sulfide minerals, i.e. MS + H
2O to give MO + H
2S. Normal concentration in clean air is about 0.0001-0.0002
ppm.
Sulfate-reducing bacteria obtain energy by
oxidizing organic matter or hydrogen with
sulfates, producing H
2S. These microorganisms are prevalent in low-oxygen environments, such as in swamps and standing waters.
Sulfur-reducing bacteria (such as
Salmonella) and some
archaea obtain their energy by oxidizing organic matter or hydrogen with elemental
sulfur, also producing H
2S. Other
anaerobic bacteria liberate hydrogen sulfide when they digest sulfur-containing
amino acids, for instance during the decay of organic matter. H
2S-producing bacteria also operate in the human
colon, and the odor of
flatulence is largely due to trace amounts of the gas. Such bacterial action in the mouth may contribute to
bad breath. Evidence exists that hydrogen sulfide produced by sulfate-reducing bacteria in the colon may cause or contribute to
ulcerative colitis.
About 10% of total global emissions of H
2S are due to human activity. By far the largest industrial route to H
2S occurs in
petroleum refineries: the
hydrodesulfurization process liberates sulfur from
petroleum by the action of hydrogen. The resulting H
2S is converted to elemental sulfur by partial combustion via the
Claus process, which is a major source of elemental sulfur. Other anthropogenic sources of hydrogen sulfide include
coke ovens,
paper mills (using the sulphate method), and
tanneries. H
2S arises from virtually anywhere where elemental sulfur comes into contact with organic material, especially at high temperatures.
Hydrogen sulfide can be present naturally in well water. In such cases,
ozone is often used for its removal. An alternative method uses a filter with
manganese dioxide. Both methods oxidize sulfides to less toxic
sulfates.
A buildup of hydrogen sulfide in the atmosphere could have caused the
Permian-Triassic extinction event 252 million years ago.
[2]
Manufacture and use
Hydrogen sulfide used to have importance in
analytical chemistry for well over a century, in the
qualitative inorganic analysis of metal ions. For such small-scale laboratory use, H
2S was made as needed in a
Kipp generator by reaction of
sulfuric acid (H
2SO
4) with
ferrous sulfide FeS. Kipp generators were superseded by the use of
thioacetamide, an organic solid that converts in water to H
2S. In these analyses, heavy metal (and
nonmetal) ions (e.g. Pb(II), Cu(II), Hg(II), As(III)) are precipitated from solution upon exposure to H
2S. The components of the resulting precipitate redissolve with some selectivity.
Industrial production focuses on separation of hydrogen sulfide from
sour gas — natural gas with high content of H
2S.
It is used for the preparation of metallic sulfides, which find use as phosphors and
oil additives, in separation of metals, removal of metallic impurities, and in organic chemical synthesis. Hydrogen sulfide is also used in the separation of deuterium oxide, i.e.
heavy water, from normal water via the
Girdler Sulfide process.
Safety
Hydrogen sulfide is a highly
toxic and flammable gas. Being heavier than air, it tends to accumulate at the bottom of poorly ventilated spaces. Although very pungent at first, it quickly deadens the sense of smell, so potential victims may be unaware of its presence until it is too late. For more information see an
MSDS.
Toxicity
Hydrogen sulfide is considered a broad-spectrum poison, meaning that it can poison several different systems in the body, although the
nervous system is most affected. The toxicity of H
2S is comparable with that of
hydrogen cyanide. It forms a complex bond with
iron in the
mitochondrial
cytochrome enzymes, thereby blocking oxygen from binding and stopping
cellular respiration. Since hydrogen sulfide occurs naturally in the environment and the gut, enzymes exist in the body capable of detoxifying it by oxidation to (harmless) sulfate. Hence low levels of sulfide may be tolerated indefinitely. However, at some threshold level, the oxidative enzymes will be overwhelmed. This threshold level is believed to average around 300-350 ppm. Many personal safety gas detectors are set to alarm at 10 PPM and to go into high alarm at 15 PPM (Utility, sewage & petrochemical workers).
An interesting diagnostic clue of extreme poisoning by H
2S is the discoloration of
copper coins in the pockets of the victim. Treatment involves immediate inhalation of
amyl nitrite, injections of
sodium nitrite, inhalation of pure oxygen, administration of
bronchodilators to overcome eventual
bronchospasm, and in some cases hyperbaric oxygen therapy.
Exposure to lower concentrations can result in
eye irritation, a sore throat and
cough, shortness of breath, and fluid in the
lungs. These symptoms usually go away in a few weeks. Long-term, low-level exposure may result in
fatigue, loss of appetite,
headaches, irritability, poor memory, and
dizziness. Chronic exposures to low level H2S (around 2
ppm) has been implicated in increased miscarriage and reproductive health issues amongst Russian and Finnish wood pulp workers, but the reports hadn't (as of circa 1995) been replicated. Higher concentrations of 700-800
ppm tend to be fatal.
★ 0.0047 ppm is the recognition threshold, the concentration at which 50% of humans can detect the characteristic odor of hydrogen sulfide
[1], normally described as resembling "a rotten egg".
★ 10-20 ppm is the borderline concentration for eye irritation.
★ 50-100 ppm leads to eye damage.
★ At 150-250 ppm the olfactory nerve is paralyzed after a few inhalations, and the sense of smell disappears, often together with awareness of danger,
★ 320-530 ppm leads to
pulmonary edema with the possibility of death.
★ 530-1000 ppm causes strong stimulation of the
central nervous system and rapid breathing, leading to loss of breathing;
★
★ 800 ppm is the lethal concentration for 50% of humans for 5 minutes exposure(
LC50).
★ Concentrations over 1000 ppm cause immediate collapse with loss of breathing, even after inhalation of a single breath.
A practical test used in the oilfield industry to determine whether someone requires overnight observation for
pulmonary edema is the knee test: if a worker that gets "gassed" loses his balance and at least one knee touches the ground, the dose was high enough to cause pulmonary edema.
Function in the body
Hydrogen sulfide is produced in small amounts by some cells of the
mammalian body and has a number of biological functions. (
nitric oxide (NO) and
carbon monoxide (CO) are also implicated as gaseous signalling agents.) It is produced from
cysteine by various
enzymes. It acts as a
vasodilator and is also active in the
brain, where it increases the response of the
NMDA receptor and facilitates
long term potentiation, which is involved in the formation of memory. Eventually the gas is converted to
sulfites and further oxidized to
thiosulfate and
sulfate.{{fact}
In
trisomy 21 (the most common form of Down syndrome) the body produces an excess of hydrogen sulfide.
Induced hibernation
In 2005 it was shown that
mice can be put into a state of
suspended animation by applying a low dosage of hydrogen sulfide (80
ppm H
2S) in the air. The breathing rate of the animals sank from 120 to 10 breaths per minute and their temperature fell from 37 °C to 2 °C above ambient temperature (in effect, they had become
cold-blooded). The mice survived this procedure for 6 hours and afterwards showed no negative health consequences.
[3]
Such a
hibernation occurs naturally in many
mammals and also in
toads, but not in mice. (Mice can fall into a state called
clinical torpor when food shortage occurs). If the H
2S-induced hibernation can be made to work in humans, it could be useful in the emergency management of severely injured patients, and in the conservation of donated organs.
As mentioned above, hydrogen sulfide binds to
cytochrome oxidase and thereby prevents oxygen from binding, which leads to the dramatic slowdown of
metabolism. Animals and humans naturally produce some hydrogen sulfide in their body; researchers have proposed that the gas is used to regulate metabolic activity and body temperature, which would explain the above findings.
[4]
In 2006 it was shown that the
blood pressure of mice treated in this fashion with hydrogen sulfide did not significantly decrease.
[5]
Participant in the sulfur cycle
Hydrogen sulfide is a central participant in the
sulfur cycle, the
biogeochemical cycle of
sulfur on Earth. As mentioned above, sulfur-reducing and sulfate-reducing bacteria derive energy from
oxidizing hydrogen or organic molecules in the absence of oxygen by reducing sulfur or sulfate to hydrogen sulfide. Other bacteria liberate hydrogen sulfide from sulfur-containing
amino acids. Several groups of bacteria can use hydrogen sulfide as fuel,
oxidizing it to elemental sulfur or to sulfate by using dissolved oxygen, metal oxides (e.g. Fe oxyhyroxides and Mn oxides) or nitrate as oxidant
[6]. The
purple sulfur bacteria and the
green sulfur bacteria use hydrogen sulfide as electron donor in
photosynthesis, thereby producing elemental sulfur. (In fact, this mode of photosynthesis is older than the mode of
cyanobacteria,
algae and
plants which uses water as electron donor and liberates oxygen.)
H2S implicated in mass extinctions
Hydrogen sulfide has been implicated in some of the five mass extinctions that have occurred in the Earth's past. Although asteroid impacts have been implicated in some extinctions, the
Permian mass extinction (sometimes known as the "Great Dying") may have been caused by hydrogen sulfide. Organic residues from these extinction boundaries indicate that the oceans were anoxic (oxygen depleted) and had species of shallow plankton that metabolized H
2S. The formation of H
2S may have been initated by massive volcanic eruptions, which emitted CO
2 and methane into the atmosphere which warmed the oceans, lowering their capacity to absorb oxygen which would otherwise oxidize H
2S. The increased levels of hydrogen sulfide could have killed oxygen-generating plants as well as depleted the ozone layer causing further stress. Small H
2S blooms have been detected in modern times in the Dead sea and in the Atlantic ocean off the coast of Namibia.
See also
★
Amine gas treating
★
Claus process
References
1. Giggenbach, W. (1971). ''Inorg. Chem.'' 10:1333. Meyer, B.; Ward, K.; Koshlap, K.; & Peter, L. (1983). ''Inorganic Chemistry'' 22:2345. Myers, R. J. (1986). ''Journal of Chemical Education'' 63:687.
2. "Impact From the Deep" in the October 2006 issue of Scientific American.
3. Mice put in 'suspended animation', BBC News, 21 April 2005
4. Mark B. Roth and Todd Nystul. Buying Time in Suspended Animation. ''Scientific American, 1 June 2005
5. Gas induces 'suspended animation', BBC News, 9 October 2006
6. Jørgensen, B. B. & D. C. Nelson (2004) Sulfide oxidation in marine sediments: Geochemistry meets microbiology, pp. 36-81. In J. P. Amend, K. J. Edwards, and T. W. Lyons (eds.) Sulfur Biogeochemistry - Past and Present. Geological Society of America.
★ "Hydrogen Sulfide", Committee on Medical and Biological Effects of Environmental Pollutants, University Park Press, 1979, Baltimore. ISBN 0-8391-0127-9
External links
★
International Chemical Safety Card 0165
★
Concise International Chemical Assessment Document 53
★
National Pollutant Inventory - Hydrogen sulfide fact sheet
★
NIOSH Pocket Guide to Chemical Hazards
★
MSDS safety data sheet
★
Abstract of survey article on H2S as used by the body, by P. Kamoun
★
Computational Chemistry Wiki
★ NACE (National Association of Corrosion Epal) http://www.nace.org/