Arsenic | |||||||||||||||||||||||||||||
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Pronunciation |
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Allotropes | grey (most common), yellow, black | ||||||||||||||||||||||||||||
Appearance | metallic grey | ||||||||||||||||||||||||||||
Standard atomic weight Ar, std(As) | 74.921595(6) | ||||||||||||||||||||||||||||
Arsenic in the periodic table | |||||||||||||||||||||||||||||
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Atomic number (Z) | 33 | ||||||||||||||||||||||||||||
Group | group 15 (pnictogens) | ||||||||||||||||||||||||||||
Period | period 4 | ||||||||||||||||||||||||||||
Block | p-block | ||||||||||||||||||||||||||||
Element category | metalloid | ||||||||||||||||||||||||||||
Electron configuration | [Ar] 3d10 4s2 4p3 | ||||||||||||||||||||||||||||
Electrons per shell
| 2, 8, 18, 5 | ||||||||||||||||||||||||||||
Physical properties | |||||||||||||||||||||||||||||
Phase at STP | solid | ||||||||||||||||||||||||||||
Sublimation point | 887 K (615 °C, 1137 °F) | ||||||||||||||||||||||||||||
Density (near r.t.) | 5.727 g/cm3 | ||||||||||||||||||||||||||||
when liquid (at m.p.) | 5.22 g/cm3 | ||||||||||||||||||||||||||||
Triple point | 1090 K, 3628 kPa | ||||||||||||||||||||||||||||
Critical point | 1673 K, ? MPa | ||||||||||||||||||||||||||||
Heat of fusion | grey: 24.44 kJ/mol | ||||||||||||||||||||||||||||
Heat of vaporization | 34.76 kJ/mol (?) | ||||||||||||||||||||||||||||
Molar heat capacity | 24.64 J/(mol·K) | ||||||||||||||||||||||||||||
Vapor pressure
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Atomic properties | |||||||||||||||||||||||||||||
Oxidation states | −3, −2, −1, +1, +2, +3, +4, +5 (a mildly acidic oxide) | ||||||||||||||||||||||||||||
Electronegativity | Pauling scale: 2.18 | ||||||||||||||||||||||||||||
Ionization energies |
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Atomic radius | empirical: 119 pm | ||||||||||||||||||||||||||||
Covalent radius | 119±4 pm | ||||||||||||||||||||||||||||
Van der Waals radius | 185 pm | ||||||||||||||||||||||||||||
Spectral lines of arsenic | |||||||||||||||||||||||||||||
Other properties | |||||||||||||||||||||||||||||
Natural occurrence | primordial | ||||||||||||||||||||||||||||
Crystal structure | rhombohedral | ||||||||||||||||||||||||||||
Thermal expansion | 5.6 µm/(m·K) (at r.t.) | ||||||||||||||||||||||||||||
Thermal conductivity | 50.2 W/(m·K) | ||||||||||||||||||||||||||||
Electrical resistivity | 333 nΩ·m (at 20 °C) | ||||||||||||||||||||||||||||
Magnetic ordering | diamagnetic | ||||||||||||||||||||||||||||
Magnetic susceptibility | −5.5·10−6 cm3/mol | ||||||||||||||||||||||||||||
Young's modulus | 8 GPa | ||||||||||||||||||||||||||||
Bulk modulus | 22 GPa | ||||||||||||||||||||||||||||
Mohs hardness | 3.5 | ||||||||||||||||||||||||||||
Brinell hardness | 1440 MPa | ||||||||||||||||||||||||||||
CAS Number | 7440-38-2 | ||||||||||||||||||||||||||||
History | |||||||||||||||||||||||||||||
Discovery | before 300 CE | ||||||||||||||||||||||||||||
Main isotopes of arsenic | |||||||||||||||||||||||||||||
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Arsenic is a chemical element with symbol As and atomic number 33. Arsenic occurs in many minerals, usually in combination with sulfur and metals, but also as a pure elemental crystal. Arsenic is a metalloid. It has various allotropes, but only the gray form, which has a metallic appearance, is important to industry.
The primary use of arsenic is in alloys of lead (for example, in car batteries and ammunition). Arsenic is a common n-type dopant in semiconductor electronic devices, and the optoelectronic compound gallium arsenide is the second most commonly used semiconductor after doped silicon. Arsenic and its compounds, especially the trioxide, are used in the production of pesticides, treated wood products, herbicides, and insecticides. These applications are declining due to the toxicity of arsenic and its compounds.
A few species of bacteria are able to use arsenic compounds as respiratory metabolites. Trace quantities of arsenic are an essential dietary element in rats, hamsters, goats, chickens, and presumably other species. A role in human metabolism is not known. However, arsenic poisoning occurs in multicellular life if quantities are larger than needed. Arsenic contamination of groundwater is a problem that affects millions of people across the world.
The United States' Environmental Protection Agency states that all forms of arsenic are a serious risk to human health. The United States' Agency for Toxic Substances and Disease Registry ranked arsenic as number 1 in its 2001 Priority List of Hazardous Substances at Superfund sites. Arsenic is classified as a Group-A carcinogen.
Characteristics
Physical characteristics
The three most common arsenic allotropes are gray, yellow, and black arsenic, with gray being the most common. Gray arsenic (α-As, space group R3m
No. 166) adopts a double-layered structure consisting of many
interlocked, ruffled, six-membered rings. Because of weak bonding
between the layers, gray arsenic is brittle and has a relatively low Mohs hardness
of 3.5. Nearest and next-nearest neighbors form a distorted octahedral
complex, with the three atoms in the same double-layer being slightly
closer than the three atoms in the next. This relatively close packing leads to a high density of 5.73 g/cm3. Gray arsenic is a semimetal, but becomes a semiconductor with a bandgap of 1.2–1.4 eV if amorphized. Gray arsenic is also the most stable form. Yellow arsenic is soft and waxy, and somewhat similar to tetraphosphorus (P
4). Both have four atoms arranged in a tetrahedral structure in which each atom is bound to each of the other three atoms by a single bond. This unstable allotrope, being molecular, is the most volatile, least dense, and most toxic. Solid yellow arsenic is produced by rapid cooling of arsenic vapor, As
4. It is rapidly transformed into gray arsenic by light. The yellow form has a density of 1.97 g/cm3. Black arsenic is similar in structure to black phosphorus. Black arsenic can also be formed by cooling vapor at around 100–220 °C. It is glassy and brittle. It is also a poor electrical conductor.
4). Both have four atoms arranged in a tetrahedral structure in which each atom is bound to each of the other three atoms by a single bond. This unstable allotrope, being molecular, is the most volatile, least dense, and most toxic. Solid yellow arsenic is produced by rapid cooling of arsenic vapor, As
4. It is rapidly transformed into gray arsenic by light. The yellow form has a density of 1.97 g/cm3. Black arsenic is similar in structure to black phosphorus. Black arsenic can also be formed by cooling vapor at around 100–220 °C. It is glassy and brittle. It is also a poor electrical conductor.
Isotopes
Arsenic occurs in nature as a monoisotopic element, composed of one stable isotope, 75As. As of 2003, at least 33 radioisotopes have also been synthesized, ranging in atomic mass from 60 to 92. The most stable of these is 73As with a half-life of 80.30 days. All other isotopes have half-lives of under one day, with the exception of 71As (t1/2=65.30 hours), 72As (t1/2=26.0 hours), 74As (t1/2=17.77 days), 76As (t1/2=1.0942 days), and 77As (t1/2=38.83 hours). Isotopes that are lighter than the stable 75As tend to decay by β+ decay, and those that are heavier tend to decay by β− decay, with some exceptions.
At least 10 nuclear isomers have been described, ranging in atomic mass from 66 to 84. The most stable of arsenic's isomers is 68mAs with a half-life of 111 seconds.
Chemistry
Arsenic
has a similar electronegativity and ionization energies to its lighter
congener phosphorus and as such readily forms covalent molecules with
most of the nonmetals. Though stable in dry air, arsenic forms a
golden-bronze tarnish upon exposure to humidity which eventually becomes
a black surface layer. When heated in air, arsenic oxidizes to arsenic trioxide; the fumes from this reaction have an odor resembling garlic. This odor can be detected on striking arsenide minerals such as arsenopyrite with a hammer. It burns in oxygen to form arsenic trioxide and arsenic pentoxide, which have the same structure as the more well-known phosphorus compounds, and in fluorine to give arsenic pentafluoride. Arsenic (and some arsenic compounds) sublimes
upon heating at atmospheric pressure, converting directly to a gaseous
form without an intervening liquid state at 887 K (614 °C). The triple point is 3.63 MPa and 1,090 K (820 °C). Arsenic makes arsenic acid with concentrated nitric acid, arsenous acid with dilute nitric acid, and arsenic trioxide with concentrated sulfuric acid; however, it does not react with water, alkalis, or non-oxidising acids. Arsenic reacts with metals to form arsenides, though these are not ionic compounds containing the As3− ion as the formation of such an anion would be highly endothermic and even the group 1 arsenides have properties of intermetallic compounds. Like germanium, selenium, and bromine, which like arsenic succeed the 3d transition series,
arsenic is much less stable in the group oxidation state of +5 than its
vertical neighbors phosphorus and antimony, and hence arsenic pentoxide
and arsenic acid are potent oxidizers.
Compounds
Compounds of arsenic resemble in some respects those of phosphorus which occupies the same group (column) of the periodic table. The most common oxidation states for arsenic are: −3 in the arsenides, which are alloy-like intermetallic compounds, +3 in the arsenites, and +5 in the arsenates and most organoarsenic compounds. Arsenic also bonds readily to itself as seen in the square As3−
4 ions in the mineral skutterudite. In the +3 oxidation state, arsenic is typically pyramidal owing to the influence of the lone pair of electrons.
4 ions in the mineral skutterudite. In the +3 oxidation state, arsenic is typically pyramidal owing to the influence of the lone pair of electrons.
Inorganic compounds
One of the simplest arsenic compound is the trihydride, the highly toxic, flammable, pyrophoric arsine (AsH3).
This compound is generally regarded as stable, since at room
temperature it decomposes only slowly. At temperatures of 250–300 °C
decomposition to arsenic and hydrogen is rapid. Several factors, such as humidity, presence of light and certain catalysts (namely aluminium) facilitate the rate of decomposition. It oxidises readily in air to form arsenic trioxide and water, and analogous reactions take place with sulfur and selenium instead of oxygen.
Arsenic forms colorless, odorless, crystalline oxides As2O3 ("white arsenic") and As2O5 which are hygroscopic and readily soluble in water to form acidic solutions. Arsenic(V) acid is a weak acid and the salts are called arsenates, the most common arsenic contamination of groundwater, and a problem that affects many people. Synthetic arsenates include Scheele's Green (cupric hydrogen arsenate, acidic copper arsenate), calcium arsenate, and lead hydrogen arsenate. These three have been used as agricultural insecticides and poisons.
The protonation steps between the arsenate and arsenic acid are similar to those between phosphate and phosphoric acid. Unlike phosphorous acid, arsenous acid is genuinely tribasic, with the formula As(OH)3.
A broad variety of sulfur compounds of arsenic are known. Orpiment (As2S3) and realgar (As4S4) are somewhat abundant and were formerly used as painting pigments. In As4S10, arsenic has a formal oxidation state of +2 in As4S4 which features As-As bonds so that the total covalency of As is still 3. Both orpiment and realgar, as well as As4S3, have selenium analogs; the analogous As2Te3 is known as the mineral kalgoorlieite, and the anion As2Te− is known as a ligand in cobalt complexes.
All trihalides of arsenic(III) are well known except the astatide, which is unknown. Arsenic pentafluoride (AsF5)
is the only important pentahalide, reflecting the lower stability of
the +5 oxidation state; even so, it is a very strong fluorinating and
oxidizing agent. (The pentachloride is stable only below −50 °C, at which temperature it decomposes to the trichloride, releasing chlorine gas.)
Alloys
Arsenic is used as the group 5 element in the III-V semiconductors gallium arsenide, indium arsenide, and aluminium arsenide. The valence electron count of GaAs is the same as a pair of Si atoms, but the band structure is completely different which results in distinct bulk properties. Other arsenic alloys include the II-V semiconductor cadmium arsenide.
Organoarsenic compounds
A large variety of organoarsenic compounds are known. Several were developed as chemical warfare agents during World War I, including vesicants such as lewisite and vomiting agents such as adamsite. Cacodylic acid, which is of historic and practical interest, arises from the methylation of arsenic trioxide, a reaction that has no analogy in phosphorus chemistry. Indeed, cacodyl was the first organometallic compound known (even though arsenic is not a true metal) and was named from the Greek κακωδἰα "stink" for its offensive odor; it is very poisonous.
Occurrence and production
Arsenic comprises about 1.5 ppm (0.00015%) of the Earth's crust, and is the 53rd most abundant element. Typical background concentrations of arsenic do not exceed 3 ng/m3 in the atmosphere; 100 mg/kg in soil; and 10 μg/L in freshwater.
Minerals with the formula MAsS and MAs2 (M = Fe, Ni, Co) are the dominant commercial sources of arsenic, together with realgar (an arsenic sulfide mineral) and native (elemental) arsenic. An illustrative mineral is arsenopyrite (FeAsS), which is structurally related to iron pyrite. Many minor As-containing minerals are known. Arsenic also occurs in various organic forms in the environment.
In 2014, China was the top producer of white arsenic with almost 70% world share, followed by Morocco, Russia, and Belgium, according to the British Geological Survey and the United States Geological Survey.
Most arsenic refinement operations in the US and Europe have closed
over environmental concerns. Arsenic is found in the smelter dust from copper, gold, and lead smelters, and is recovered primarily from copper refinement dust.
On roasting arsenopyrite in air, arsenic sublimes as arsenic(III) oxide leaving iron oxides,
while roasting without air results in the production of gray arsenic.
Further purification from sulfur and other chalcogens is achieved by sublimation in vacuum, in a hydrogen atmosphere, or by distillation from molten lead-arsenic mixture.
Rank | Country | 2014 As2O3 Production |
---|---|---|
1 | China | 25,000 T |
2 | Morocco | 8,800 T |
3 | Russia | 1,500 T |
4 | Belgium | 1,000 T |
5 | Bolivia | 52 T |
6 | Japan | 45 T |
— | World Total (rounded) | 36,400 T |
History
The word arsenic has its origin in the Syriac word ܠܐ ܙܐܦܢܝܐ (al) zarniqa, from the Persian word زرنيخ zarnikh, meaning "yellow" (literally "gold-colored") and hence "(yellow) orpiment". It was adopted into Greek as arsenikon (ἀρσενικόν), a form that is folk etymology, being the neuter form of the Greek word arsenikos (ἀρσενικός), meaning "male", "virile". The Greek word was adopted in Latin as arsenicum, which in French became arsenic, from which the English word arsenic is taken. Arsenic sulfides (orpiment, realgar) and oxides have been known and used since ancient times. Zosimos (circa 300 AD) describes roasting sandarach (realgar) to obtain cloud of arsenic (arsenic trioxide), which he then reduces to gray arsenic. As the symptoms of arsenic poisoning are not very specific, it was frequently used for murder until the advent of the Marsh test, a sensitive chemical test for its presence. (Another less sensitive but more general test is the Reinsch test.)
Owing to its use by the ruling class to murder one another and its
potency and discreetness, arsenic has been called the "poison of kings"
and the "king of poisons".
During the Bronze Age, arsenic was often included in bronze, which made the alloy harder (so-called "arsenical bronze").
Albertus Magnus
(Albert the Great, 1193–1280) is believed to have been the first to
isolate the element from a compound in 1250, by heating soap together
with arsenic trisulfide. In 1649, Johann Schröder published two ways of preparing arsenic. Crystals of elemental (native) arsenic are found in nature, although rare.
Cadet's fuming liquid (impure cacodyl), often claimed as the first synthetic organometallic compound, was synthesized in 1760 by Louis Claude Cadet de Gassicourt by the reaction of potassium acetate with arsenic trioxide.
In the Victorian era, "arsenic" ("white arsenic" or arsenic trioxide) was mixed with vinegar and chalk and eaten by women to improve the complexion of their faces, making their skin paler to show they did not work in the fields.
Arsenic was also rubbed into the faces and arms of women to "improve
their complexion". The accidental use of arsenic in the adulteration of
foodstuffs led to the Bradford sweet poisoning in 1858, which resulted in around 20 deaths. Wallpaper production also began to use dyes made from arsenic, which was thought to increase the pigment’s brightness.
Two arsenic pigments have been widely used since their discovery – Paris Green and Scheele's Green.
After the toxicity of arsenic became widely known, these chemicals were
used less often as pigments and more often as insecticides. In the
1860s, an arsenic byproduct of dye production, London Purple was widely
used. This was a solid mixture of arsenic trioxide, aniline, lime, and
ferrous oxide, insoluble in water and very toxic by inhalation or
ingestion But it was later replaced with Paris Green, another arsenic-based dye. With better understanding of the toxicology mechanism, two other compounds were used starting in the 1890s. Arsenite of lime and arsenate of lead were used widely as insecticides until the discovery of DDT in 1942.
Applications
Agricultural
The toxicity of arsenic to insects, bacteria, and fungi led to its use as a wood preservative. In the 1930s, a process of treating wood with chromated copper arsenate (also known as CCA or Tanalith)
was invented, and for decades, this treatment was the most extensive
industrial use of arsenic. An increased appreciation of the toxicity of
arsenic led to a ban of CCA in consumer products in 2004, initiated by
the European Union and United States. However, CCA remains in heavy use in other countries (such as on Malaysian rubber plantations).
Arsenic was also used in various agricultural insecticides and poisons. For example, lead hydrogen arsenate was a common insecticide on fruit trees, but contact with the compound sometimes resulted in brain damage among those working the sprayers. In the second half of the 20th century, monosodium methyl arsenate (MSMA) and disodium methyl arsenate
(DSMA) – less toxic organic forms of arsenic – replaced lead arsenate
in agriculture. These organic arsenicals were in turn phased out by 2013
in all agricultural activities except cotton farming.
The biogeochemistry of arsenic is complex and includes various
adsorption and desorption processes. The toxicity of arsenic is
connected to its solubility and is affected by pH. Arsenite (AsO3−
3) is more soluble than arsenate (AsO3−
4) and is more toxic; however, at a lower pH, arsenate becomes more mobile and toxic. It was found that addition of sulfur, phosphorus, and iron oxides to high-arsenite soils greatly reduces arsenic phytotoxicity.
3) is more soluble than arsenate (AsO3−
4) and is more toxic; however, at a lower pH, arsenate becomes more mobile and toxic. It was found that addition of sulfur, phosphorus, and iron oxides to high-arsenite soils greatly reduces arsenic phytotoxicity.
Arsenic is used as a feed additive in poultry and swine production, in particular in the U.S. to increase weight gain, improve feed efficiency, and to prevent disease. An example is roxarsone, which had been used as a broiler starter by about 70% of U.S. broiler growers. The Poison-Free Poultry Act of 2009 proposed to ban the use of roxarsone in industrial swine and poultry production.
Alpharma, a subsidiary of Pfizer Inc., which produces roxarsone,
voluntarily suspended sales of the drug in response to studies showing
elevated levels of inorganic arsenic, a carcinogen, in treated chickens. A successor to Alpharma, Zoetis, continues to sell nitarsone, primarily for use in turkeys.
Arsenic is intentionally added to the feed of chickens
raised for human consumption. Organic arsenic compounds are less toxic
than pure arsenic, and promote the growth of chickens. Under some
conditions, the arsenic in chicken feed is converted to the toxic inorganic form.
A 2006 study of the remains of the Australian racehorse, Phar Lap,
determined that the 1932 death of the famous champion was caused by a
massive overdose of arsenic. Sydney veterinarian Percy Sykes stated,
"In those days, arsenic was quite a common tonic, usually given in the
form of a solution (Fowler's Solution) ... It was so common that I'd
reckon 90 per cent of the horses had arsenic in their system."
Medical use
During the 18th, 19th, and 20th centuries, a number of arsenic compounds were used as medicines, including arsphenamine (by Paul Ehrlich) and arsenic trioxide (by Thomas Fowler). Arsphenamine, as well as neosalvarsan, was indicated for syphilis and trypanosomiasis, but has been superseded by modern antibiotics.
Arsenic trioxide has been used in a variety of ways over the past 500 years, most commonly in the treatment of cancer, but in medications as diverse as Fowler's solution in psoriasis. The US Food and Drug Administration in the year 2000 approved this compound for the treatment of patients with acute promyelocytic leukemia that is resistant to all-trans retinoic acid.
Recently, researchers have been locating tumors using arsenic-74 (a positron emitter). This isotope produces clearer PET scan images than the previous radioactive agent, iodine-124, because the body tends to transport iodine to the thyroid gland producing signal noise.
In subtoxic doses, soluble arsenic compounds act as stimulants, and were once popular in small doses as medicine by people in the mid-18th to 19th centuries.
Alloys
The main use of arsenic is in alloying with lead. Lead components in car batteries are strengthened by the presence of a very small percentage of arsenic. Dezincification of brass (a copper-zinc alloy) is greatly reduced by the addition of arsenic.
"Phosphorus Deoxidized Arsenical Copper" with an arsenic content of
0.3% has an increased corrosion stability in certain environments. Gallium arsenide is an important semiconductor material, used in integrated circuits. Circuits made from GaAs are much faster (but also much more expensive) than those made from silicon. Unlike silicon, GaAs has a direct bandgap, and can be used in laser diodes and LEDs to convert electrical energy directly into light.
Military
After World War I, the United States built a stockpile of 20,000 tons of weaponized lewisite (ClCH=CHAsCl2), an organoarsenic vesicant (blister agent) and lung irritant. The stockpile was neutralized with bleach and dumped into the Gulf of Mexico in the 1950s. During the Vietnam War, the United States used Agent Blue, a mixture of sodium cacodylate and its acid form, as one of the rainbow herbicides to deprive North Vietnamese soldiers of foliage cover and rice.
Other uses
- Copper acetoarsenite was used as a green pigment known under many names, including Paris Green and Emerald Green. It caused numerous arsenic poisonings. Scheele's Green, a copper arsenate, was used in the 19th century as a coloring agent in sweets.
- Arsenic is used in bronzing and pyrotechnics.
- As much as 2% of produced arsenic is used in lead alloys for lead shot and bullets.
- Arsenic is added in small quantities to alpha-brass to make it dezincification-resistant. This grade of brass is used in plumbing fittings and other wet environments.
- Arsenic is also used for taxonomic sample preservation.
- Until recently, arsenic was used in optical glass. Modern glass manufacturers, under pressure from environmentalists, have ceased using both arsenic and lead.
Biological role
Bacteria
Some species of bacteria obtain their energy by oxidizing various fuels while reducing
arsenate to arsenite. Under oxidative environmental conditions some
bacteria oxidize arsenite to arsenate as fuel for their metabolism. The enzymes involved are known as arsenate reductases (Arr).
In 2000, bacteria were discovered that employ a version of photosynthesis in the absence of oxygen with arsenites as electron donors,
producing arsenates (just as ordinary photosynthesis uses water as
electron donor, producing molecular oxygen). This may be classified as
chemolithoautotrophic arsenite oxidation, for which oxygen is used as
the terminal electron acceptor, arsenite is the electron donor, and
carbon dioxide is the carbon source.
Researchers conjecture that, over the course of history, these
photosynthesizing organisms produced the arsenates that allowed the
arsenate-reducing bacteria to thrive. One strain PHS-1 has been isolated and is related to the gammaproteobacterium Ectothiorhodospira shaposhnikovii. The mechanism is unknown, but an encoded Arr enzyme may function in reverse to its known homologues.
Although the arsenate and phosphate anions are similar structurally, no evidence exists for the replacement of phosphate in ATP or nucleic acids by arsenic.
Essential trace element in higher animals
Some
evidence indicates that arsenic is an essential trace mineral in birds
(chickens), and in mammals (rats, hamsters, and goats). However, the biological function is not known.
Heredity
Arsenic has been linked to epigenetic changes, heritable changes in gene expression that occur without changes in DNA sequence. These include DNA methylation, histone modification, and RNA interference. Toxic levels of arsenic cause significant DNA hypermethylation of tumor suppressor genes p16 and p53, thus increasing risk of carcinogenesis. These epigenetic events have been studied in vitro using human kidney cells and in vivo using rat liver cells and peripheral blood leukocytes in humans. Inductively coupled plasma mass spectrometry
(ICP-MS) is used to detect precise levels of intracellular arsenic and
other arsenic bases involved in epigenetic modification of DNA. Studies investigating arsenic as an epigenetic factor can be used to develop precise biomarkers of exposure and susceptibility.
The Chinese brake fern (Pteris vittata) hyperaccumulates arsenic from the soil into its leaves and has a proposed use in phytoremediation.
Biomethylation
Inorganic arsenic and its compounds, upon entering the food chain, are progressively metabolized through a process of methylation. For example, the mold Scopulariopsis brevicaulis produces significant amounts of trimethylarsine if inorganic arsenic is present. The organic compound arsenobetaine
is found in some marine foods such as fish and algae, and also in
mushrooms in larger concentrations. The average person's intake is about
10–50 µg/day. Values about 1000 µg are not unusual following
consumption of fish or mushrooms, but there is little danger in eating
fish because this arsenic compound is nearly non-toxic.
Environmental issues
Exposure
Naturally
occurring sources of human exposure include volcanic ash, weathering of
minerals and ores, and mineralized groundwater. Arsenic is also found
in food, water, soil, and air. Arsenic is absorbed by all plants, but is more concentrated in leafy vegetables, rice, apple and grape juice, and seafood. An additional route of exposure is inhalation of atmospheric gases and dusts.
Occurrence in drinking water
Extensive arsenic contamination of groundwater has led to widespread arsenic poisoning in Bangladesh and neighboring countries. It is estimated that approximately 57 million people in the Bengal basin are drinking groundwater with arsenic concentrations elevated above the World Health Organization's standard of 10 parts per billion (ppb). However, a study of cancer rates in Taiwan
suggested that significant increases in cancer mortality appear only at
levels above 150 ppb. The arsenic in the groundwater is of natural
origin, and is released from the sediment into the groundwater, caused
by the anoxic conditions of the subsurface. This groundwater was used after local and western NGOs and the Bangladeshi government undertook a massive shallow tube well
drinking-water program in the late twentieth century. This program was
designed to prevent drinking of bacteria-contaminated surface waters,
but failed to test for arsenic in the groundwater. Many other countries
and districts in Southeast Asia, such as Vietnam and Cambodia, have geological environments that produce groundwater with a high arsenic content. Arsenicosis was reported in Nakhon Si Thammarat, Thailand in 1987, and the Chao Phraya River
probably contains high levels of naturally occurring dissolved arsenic
without being a public health problem because much of the public uses
bottled water. In Pakistan, more than 60 million people are exposed to arsenic polluted drinking water indicated by a recent report of Science. Podgorski’s team investigated more than 1200 samples and more than 66% samples exceeded the WHO minimum contamination level.
In the United States, arsenic is most commonly found in the ground waters of the southwest. Parts of New England, Michigan, Wisconsin, Minnesota and the Dakotas are also known to have significant concentrations of arsenic in ground water.
Increased levels of skin cancer have been associated with arsenic
exposure in Wisconsin, even at levels below the 10 part per billion
drinking water standard. According to a recent film funded by the US Superfund,
millions of private wells have unknown arsenic levels, and in some
areas of the US, more than 20% of the wells may contain levels that
exceed established limits.
Low-level exposure to arsenic at concentrations of 100 parts per
billion (i.e., above the 10 parts per billion drinking water standard)
compromises the initial immune response to H1N1 or swine flu
infection according to NIEHS-supported scientists. The study, conducted
in laboratory mice, suggests that people exposed to arsenic in their
drinking water may be at increased risk for more serious illness or
death from the virus.
Some Canadians are drinking water that contains inorganic
arsenic. Private-dug–well waters are most at risk for containing
inorganic arsenic. Preliminary well water analysis typically does not
test for arsenic. Researchers at the Geological Survey of Canada have
modeled relative variation in natural arsenic hazard potential for the
province of New Brunswick. This study has important implications for
potable water and health concerns relating to inorganic arsenic.
Epidemiological evidence from Chile
shows a dose-dependent connection between chronic arsenic exposure and
various forms of cancer, in particular when other risk factors, such as
cigarette smoking, are present. These effects have been demonstrated at
contaminations less than 50 ppb. Arsenic is itself a constituent of tobacco smoke.
Analyzing multiple epidemiological studies on inorganic arsenic
exposure suggests a small but measurable increase in risk for bladder
cancer at 10 ppb. According to Peter Ravenscroft of the Department of Geography at the University of Cambridge,
roughly 80 million people worldwide consume between 10 and 50 ppb
arsenic in their drinking water. If they all consumed exactly 10 ppb
arsenic in their drinking water, the previously cited multiple
epidemiological study analysis would predict an additional 2,000 cases
of bladder cancer alone. This represents a clear underestimate of the
overall impact, since it does not include lung or skin cancer, and
explicitly underestimates the exposure. Those exposed to levels of
arsenic above the current WHO standard should weigh the costs and
benefits of arsenic remediation.
Early (1973) evaluations of the processes for removing dissolved
arsenic from drinking water demonstrated the efficacy of
co-precipitation with either iron or aluminum oxides. In particular,
iron as a coagulant was found to remove arsenic with an efficacy
exceeding 90%. Several adsorptive media systems have been approved for use at point-of-service in a study funded by the United States Environmental Protection Agency (US EPA) and the National Science Foundation (NSF). A team of European and Indian scientists and engineers have set up six arsenic treatment plants in West Bengal
based on in-situ remediation method (SAR Technology). This technology
does not use any chemicals and arsenic is left in an insoluble form (+5
state) in the subterranean zone by recharging aerated water into the
aquifer and developing an oxidation zone that supports arsenic oxidizing
micro-organisms. This process does not produce any waste stream or
sludge and is relatively cheap.
Another effective and inexpensive method to avoid arsenic
contamination is to sink wells 500 feet or deeper to reach purer waters.
A recent 2011 study funded by the US National Institute of
Environmental Health Sciences' Superfund Research Program shows that
deep sediments can remove arsenic and take it out of circulation. In
this process, called adsorption, arsenic sticks to the surfaces of deep sediment particles and is naturally removed from the ground water.
Magnetic separations of arsenic at very low magnetic field gradients with high-surface-area and monodisperse magnetite (Fe3O4) nanocrystals have been demonstrated in point-of-use water purification. Using the high specific surface area of Fe3O4 nanocrystals, the mass of waste associated with arsenic removal from water has been dramatically reduced.
Epidemiological studies have suggested a correlation between
chronic consumption of drinking water contaminated with arsenic and the
incidence of all leading causes of mortality. The literature indicates that arsenic exposure is causative in the pathogenesis of diabetes.
Chaff-based filters have recently been shown to reduce the
arsenic content of water to 3 µg/L. This may find applications in areas
where the potable water is extracted from underground aquifers.
San Pedro de Atacama
For several centuries, the people of San Pedro de Atacama in Chile have been drinking water that is contaminated with arsenic, and some evidence suggests they have developed some immunity.
Hazard maps for contaminated groundwater
Around
one-third of the world’s population drinks water from groundwater
resources. Of this, about 10 percent, approximately 300 million people,
obtains water from groundwater resources that are contaminated with
unhealthy levels of arsenic or fluoride. These trace elements derive mainly from minerals.
Redox transformation of arsenic in natural waters
Arsenic is unique among the trace metalloids
and oxyanion-forming trace metals (e.g. As, Se, Sb, Mo, V, Cr, U, Re).
It is sensitive to mobilization at pH values typical of natural waters
(pH 6.5–8.5) under both oxidizing and reducing conditions. Arsenic can
occur in the environment in several oxidation states (−3, 0, +3 and +5),
but in natural waters it is mostly found in inorganic forms as
oxyanions of trivalent arsenite [As(III)] or pentavalent arsenate
[As(V)]. Organic forms of arsenic are produced by biological activity,
mostly in surface waters, but are rarely quantitatively important.
Organic arsenic compounds may, however, occur where waters are
significantly impacted by industrial pollution.
Arsenic may be solubilized by various processes. When pH is high,
arsenic may be released from surface binding sites that lose their
positive charge. When water level drops and sulfide
minerals are exposed to air, arsenic trapped in sulfide minerals can be
released into water. When organic carbon is present in water, bacteria
are fed by directly reducing As(V) to As(III) or by reducing the element
at the binding site, releasing inorganic arsenic.
The aquatic transformations of arsenic are affected by pH,
reduction-oxidation potential, organic matter concentration and the
concentrations and forms of other elements, especially iron and
manganese. The main factors are pH and the redox potential. Generally,
the main forms of arsenic under oxic conditions are H3AsO4, H2AsO4−, HAsO42−, and AsO43− at pH 2, 2–7, 7–11 and 11, respectively. Under reducing conditions, H3AsO4 is predominant at pH 2–9.
Oxidation and reduction affects the migration of arsenic in
subsurface environments. Arsenite is the most stable soluble form of
arsenic in reducing environments and arsenate, which is less mobile than
arsenite, is dominant in oxidizing environments at neutral pH.
Therefore, arsenic may be more mobile under reducing conditions. The
reducing environment is also rich in organic matter which may enhance
the solubility of arsenic compounds. As a result, the adsorption
of arsenic is reduced and dissolved arsenic accumulates in groundwater.
That is why the arsenic content is higher in reducing environments than
in oxidizing environments.
The presence of sulfur is another factor that affects the transformation of arsenic in natural water. Arsenic can precipitate
when metal sulfides form. In this way, arsenic is removed from the
water and its mobility decreases. When oxygen is present, bacteria
oxidize reduced sulfur to generate energy, potentially releasing bound
arsenic.
Redox reactions involving Fe also appear to be essential factors
in the fate of arsenic in aquatic systems. The reduction of iron
oxyhydroxides plays a key role in the release of arsenic to water. So
arsenic can be enriched in water with elevated Fe concentrations. Under oxidizing conditions, arsenic can be mobilized from pyrite
or iron oxides especially at elevated pH. Under reducing conditions,
arsenic can be mobilized by reductive desorption or dissolution when
associated with iron oxides. The reductive desorption occurs under two
circumstances. One is when arsenate is reduced to arsenite which adsorbs
to iron oxides less strongly. The other results from a change in the
charge on the mineral surface which leads to the desorption of bound
arsenic.
Some species of bacteria catalyze redox transformations of
arsenic. Dissimilatory arsenate-respiring prokaryotes (DARP) speed up
the reduction of As(V) to As(III). DARP use As(V) as the electron
acceptor of anaerobic respiration and obtain energy to survive. Other
organic and inorganic substances can be oxidized in this process. Chemoautotrophic arsenite oxidizers (CAO) and heterotrophic
arsenite oxidizers (HAO) convert As(III) into As(V). CAO combine the
oxidation of As(III) with the reduction of oxygen or nitrate. They use
obtained energy to fix produce organic carbon from CO2. HAO cannot obtain energy from As(III) oxidation. This process may be an arsenic detoxification mechanism for the bacteria.
Equilibrium thermodynamic calculations predict that As(V)
concentrations should be greater than As(III) concentrations in all but
strongly reducing conditions, i.e. where SO42− reduction is occurring. However, abiotic redox reactions of arsenic are slow. Oxidation of As(III) by dissolved O2 is a particularly slow reaction. For example, Johnson and Pilson (1975) gave half-lives for the oxygenation of As(III) in seawater ranging from several months to a year.
In other studies, As(V)/As(III) ratios were stable over periods of days
or weeks during water sampling when no particular care was taken to
prevent oxidation, again suggesting relatively slow oxidation rates.
Cherry found from experimental studies that the As(V)/As(III) ratios
were stable in anoxic solutions for up to 3 weeks but that gradual
changes occurred over longer timescales. Sterile water samples have been observed to be less susceptible to speciation changes than non-sterile samples.
Oremland found that the reduction of As(V) to As(III) in Mono Lake was
rapidly catalyzed by bacteria with rate constants ranging from 0.02 to
0.3 day−1.
Wood preservation in the US
As
of 2002, US-based industries consumed 19,600 metric tons of arsenic.
Ninety percent of this was used for treatment of wood with chromated copper arsenate (CCA). In 2007, 50% of the 5,280 metric tons of consumption was still used for this purpose.
In the United States, the voluntary phasing-out of arsenic in
production of consumer products and residential and general consumer
construction products began on 31 December 2003, and alternative
chemicals are now used, such as Alkaline Copper Quaternary, borates, copper azole, cyproconazole, and propiconazole.
Although discontinued, this application is also one of the most concern to the general public. The vast majority of older pressure-treated
wood was treated with CCA. CCA lumber is still in widespread use in
many countries, and was heavily used during the latter half of the 20th
century as a structural and outdoor building material.
Although the use of CCA lumber was banned in many areas after studies
showed that arsenic could leach out of the wood into the surrounding soil
(from playground equipment, for instance), a risk is also presented by
the burning of older CCA timber. The direct or indirect ingestion of
wood ash from burnt CCA lumber has caused fatalities in animals and
serious poisonings in humans; the lethal human dose is approximately
20 grams of ash.
Scrap CCA lumber from construction and demolition sites may be
inadvertently used in commercial and domestic fires. Protocols for safe
disposal of CCA lumber are not consistent throughout the world.
Widespread landfill disposal of such timber raises some concern, but other studies have shown no arsenic contamination in the groundwater.
Mapping of industrial releases in the US
One tool that maps the location (and other information) of arsenic releases in the United State is TOXMAP. TOXMAP is a Geographic Information System (GIS) from the Division of Specialized Information Services of the United States National Library of Medicine
(NLM) funded by the US Federal Government. With marked-up maps of the
United States, TOXMAP enables users to visually explore data from the United States Environmental Protection Agency's (EPA) Toxics Release Inventory and Superfund Basic Research Programs. TOXMAP's chemical and environmental health information is taken from NLM's Toxicology Data Network (TOXNET), PubMed, and from other authoritative sources.
Bioremediation
Physical, chemical, and biological methods have been used to remediate arsenic contaminated water. Bioremediation is said to be cost effective and environmentally friendly
Bioremediation of ground water contaminated with arsenic aims to
convert arsenite, the toxic form of arsenic to humans, to arsenate.
Arsenate (+5 oxidation state) is the dominant form of arsenic in surface
water, while arsenite (+3 oxidation state) is the dominant form in
hypoxic to anoxic environments. Arsenite is more soluble and mobile than
arsenate. Many species of bacteria can transform arsenite to arsenate
in anoxic conditions by using arsenite as an electron donor.
This is a useful method in ground water remediation. Another
bioremediation strategy is to use plants that accumulate arsenic in
their tissues via phytoremediation but the disposal of contaminated plant material needs to be considered.
Bioremediation requires careful evaluation and design in
accordance with existing conditions. Some sites may require the
addition of an electron acceptor while others require microbe
supplementation (bioaugmentation). Regardless of the method used, only constant monitoring can prevent future contamination.
Toxicity and precautions
Hazards | |
---|---|
GHS pictograms | |
GHS signal word | Danger |
H301, H331, H350, H410 |
Arsenic and many of its compounds are especially potent poisons.
Classification
Elemental arsenic and arsenic compounds are classified as "toxic" and "dangerous for the environment" in the European Union under directive 67/548/EEC.
The International Agency for Research on Cancer (IARC) recognizes arsenic and inorganic arsenic compounds as group 1 carcinogens, and the EU lists arsenic trioxide, arsenic pentoxide, and arsenate salts as category 1 carcinogens.
Arsenic is known to cause arsenicosis when present in drinking water, "the most common species being arsenate [HAsO2−
4; As(V)] and arsenite [H3AsO3; As(III)]".
4; As(V)] and arsenite [H3AsO3; As(III)]".
Legal limits, food, and drink
In the United States since 2006, the maximum concentration in drinking water allowed by the Environmental Protection Agency (EPA) is 10 ppb and the FDA set the same standard in 2005 for bottled water. The Department of Environmental Protection for New Jersey set a drinking water limit of 5 ppb in 2006. The IDLH (immediately dangerous to life and health) value for arsenic metal and inorganic arsenic compounds is 5 mg/m3 (5 ppb). The Occupational Safety and Health Administration has set the permissible exposure limit (PEL) to a time-weighted average (TWA) of 0.01 mg/m3 (0.01 ppb), and the National Institute for Occupational Safety and Health (NIOSH) has set the recommended exposure limit (REL) to a 15-minute constant exposure of 0.002 mg/m3 (0.002 ppb). The PEL for organic arsenic compounds is a TWA of 0.5 mg/m3. (0.5 ppb).
In 2008, based on its ongoing testing of a wide variety of American foods for toxic chemicals, the U.S. Food and Drug Administration
set the "level of concern" for inorganic arsenic in apple and pear
juices at 23 ppb, based on non-carcinogenic effects, and began blocking
importation of products in excess of this level; it also required
recalls for non-conforming domestic products. In 2011, the national Dr. Oz
television show broadcast a program highlighting tests performed by an
independent lab hired by the producers. Though the methodology was
disputed (it did not distinguish between organic and inorganic arsenic)
the tests showed levels of arsenic up to 36 ppb. In response, FDA tested the worst brand from the Dr. Oz
show and found much lower levels. Ongoing testing found 95% of the
apple juice samples were below the level of concern. Later testing by Consumer Reports showed inorganic arsenic at levels slightly above 10 ppb, and the organization urged parents to reduce consumption.
In July 2013, on consideration of consumption by children, chronic
exposure, and carcinogenic effect, the FDA established an "action level"
of 10 ppb for apple juice, the same as the drinking water standard.
Concern about arsenic in rice in Bangladesh was raised in 2002,
but at the time only Australia had a legal limit for food (one milligram
per kilogram). Concern was raised about people who were eating U.S. rice exceeding WHO standards for personal arsenic intake in 2005. In 2011, the People's Republic of China set a food standard of 150 ppb for arsenic.
In the United States in 2012, testing by separate groups of
researchers at the Children's Environmental Health and Disease
Prevention Research Center at Dartmouth College (early in the year, focusing on urinary levels in children) and Consumer Reports (in November) found levels of arsenic in rice that resulted in calls for the FDA to set limits. The FDA released some testing results in September 2012,
and as of July 2013, is still collecting data in support of a new
potential regulation. It has not recommended any changes in consumer
behavior.
Consumer Reports recommended:
- That the EPA and FDA eliminate arsenic-containing fertilizer, drugs, and pesticides in food production;
- That the FDA establish a legal limit for food;
- That industry change production practices to lower arsenic levels, especially in food for children; and
- That consumers test home water supplies, eat a varied diet, and cook rice with excess water, then draining it off (reducing inorganic arsenic by about one third along with a slight reduction in vitamin content).
- Evidence-based public health advocates also recommend that, given the lack of regulation or labeling for arsenic in the U.S., children should eat no more than 1.5 servings per week of rice and should not drink rice milk as part of their daily diet before age 5. They also offer recommendations for adults and infants on how to limit arsenic exposure from rice, drinking water, and fruit juice.
A 2014 World Health Organization advisory conference was scheduled to consider limits of 200–300 ppb for rice.
Occupational exposure limits
Country | Limit |
---|---|
Argentina | Confirmed human carcinogen |
Australia | TWA 0.05 mg/m3 - Carcinogen |
Belgium | TWA 0.1 mg/m3 - Carcinogen |
Bulgaria | Confirmed human carcinogen |
Colombia | Confirmed human carcinogen |
Denmark | TWA 0.01 mg/m3 |
Finland | Carcinogen |
Egypt | TWA 0.2 mg/m3 |
Hungary | Ceiling concentration 0.01 mg/m3 |
India | TWA 0.2 mg/m3 |
Japan | Group 1 carcinogen |
Jordan | Confirmed human carcinogen |
Mexico | TWA 0.2 mg/m3 |
New Zealand | TWA 0.05 mg/m3 - Carcinogen |
Norway | TWA 0.02 mg/m3 |
Philippines | TWA 0.5 mg/m3 |
Poland | TWA 0.01 mg/m3 |
Singapore | Confirmed human carcinogen |
South Korea | TWA 0.01 mg/m3 |
Sweden | TWA 0.01 mg/m3 |
Thailand | TWA 0.5 mg/m3 |
Turkey | TWA 0.5 mg/m3 |
United Kingdom | TWA 0.1 mg/m3 |
United States | TWA 0.01 mg/m3 |
Vietnam | Confirmed human carcinogen |
Ecotoxicity
Arsenic
is bioaccumulative in many organisms, marine species in particular, but
it does not appear to biomagnify significantly in food webs. In
polluted areas, plant growth may be affected by root uptake of arsenate,
which is a phosphate analog and therefore readily transported in plant
tissues and cells. In polluted areas, uptake of the more toxic arsenite
ion (found more particularly in reducing conditions) is likely in
poorly-drained soils.
Toxicity in animals
Compound | Animal | LD50 | Route |
---|---|---|---|
Arsenic | Rat | 763 mg/kg | oral |
Arsenic | Mouse | 145 mg/kg | oral |
Calcium arsenate | Rat | 20 mg/kg | oral |
Calcium arsenate | Mouse | 794 mg/kg | oral |
Calcium arsenate | Rabbit | 50 mg/kg | oral |
Calcium arsenate | Dog | 38 mg/kg | oral |
Lead arsenate | Rabbit | 75 mg/kg | oral |
Compound | Animal | LD50 | Route |
---|---|---|---|
Arsenic trioxide (As(III)) | Mouse | 26 mg/kg | oral |
Arsenite (As(III)) | Mouse | 8 mg/kg | im |
Arsenate (As(V)) | Mouse | 21 mg/kg | im |
MMA (As(III)) | Hamster | 2 mg/kg | ip |
MMA (As(V)) | Mouse | 916 mg/kg | oral |
DMA (As(V)) | Mouse | 648 mg/kg | oral |
im = injected intramuscularly
ip = administered intraperitoneally
|
Biological mechanism
Arsenic's toxicity comes from the affinity of arsenic(III) oxides for thiols. Thiols, in the form of cysteine residues and cofactors such as lipoic acid and coenzyme A, are situated at the active sites of many important enzymes.
Arsenic disrupts ATP production through several mechanisms. At the level of the citric acid cycle, arsenic inhibits lipoic acid, which is a cofactor for pyruvate dehydrogenase. By competing with phosphate, arsenate uncouples oxidative phosphorylation, thus inhibiting energy-linked reduction of NAD+,
mitochondrial respiration and ATP synthesis. Hydrogen peroxide
production is also increased, which, it is speculated, has potential to
form reactive oxygen species and oxidative stress. These metabolic
interferences lead to death from multi-system organ failure. The organ failure is presumed to be from necrotic cell death, not apoptosis, since energy reserves have been too depleted for apoptosis to occur.
Although arsenic causes toxicity it can also play a protective role.
Exposure risks and remediation
Occupational exposure and arsenic poisoning
may occur in persons working in industries involving the use of
inorganic arsenic and its compounds, such as wood preservation, glass
production, nonferrous metal alloys, and electronic semiconductor
manufacturing. Inorganic arsenic is also found in coke oven emissions
associated with the smelter industry.
The conversion between As(III) and As(V) is a large factor in
arsenic environmental contamination. According to Croal, Gralnick,
Malasarn and Newman, "[the] understanding [of] what stimulates As(III)
oxidation and/or limits As(V) reduction is relevant for bioremediation
of contaminated sites (Croal). The study of chemolithoautotrophic
As(III) oxidizers and the heterotrophic As(V) reducers can help the
understanding of the oxidation and/or reduction of arsenic.
Treatment
Treatment of chronic arsenic poisoning is possible. British anti-lewisite (dimercaprol)
is prescribed in doses of 5 mg/kg up to 300 mg every 4 hours for the
first day, then every 6 hours for the second day, and finally every
8 hours for 8 additional days. However the USA's Agency for Toxic Substances and Disease Registry (ATSDR) states that the long-term effects of arsenic exposure cannot be predicted.
Blood, urine, hair, and nails may be tested for arsenic; however, these
tests cannot foresee possible health outcomes from the exposure.
Long-term exposure and consequent excretion through urine has been
linked to bladder and kidney cancer in addition to cancer of the liver,
prostate, skin, lungs, and nasal cavity.