33 As Arsenic 74.922
Metalloid p-block Period 4 Group 15

Arsenic

As · Element 33 · Metalloid

The classic poison of history — tasteless, undetectable for centuries, and still a groundwater crisis for millions.

State at 20°C Solid
Atomic mass 74.922 u
Electron configuration[Ar] 3d¹⁰ 4s² 4p³

Structure

The arsenic atom

Not a diagram of dots on rings — a Monte-Carlo sample of the actual probability density |ψ|² for each occupied subshell. Drag to rotate. Blue and violet mark opposite signs of the wavefunction, which is what makes bonding possible.

Orbital cloud

Measured values

Property sheet

Every bar shows where arsenic sits among all 118 elements for that property.

Physical

Density 5.727 g/cm³ 32%
Sublimation point 887 K at 1 atm
Melting point 1090 K at 3.63 MPa
Specific heat 0.329 J/g·K
Thermal conductivity 50 W/m·K 65%

Atomic

Atomic radius 119 pm 13%
Covalent radius 119 pm
Van der Waals radius 185 pm

Electronic

Electronegativity 2.18 76%
Ionisation energy 944.6 kJ/mol 84%
Electron affinity 78.2 kJ/mol 63%

Occurrence

Abundance in crust 1.8 mg/kg 56%

Identity

SymbolAs
Atomic number33
Atomic mass74.9216 u
CategoryMetalloid
Blockp
Crystal structurerhombohedral
Oxidation states-3, +2, +3, +5
DiscoveredAncient
Discovered byAlbertus Magnus

Sources: IUPAC 2021 standard atomic weights · CRC Handbook of Chemistry and Physics · NIST. Values marked ~ are predicted rather than measured.

Same element, different neutrons

Isotopes of arsenic

All arsenic atoms have the same number of protons, 33, and differ only in their number of neutrons: those variants are its isotopes. The most common, As-75, has 42 neutrons and makes up 100% of natural arsenic.

Isotopes of arsenic found in nature, with their share of the natural element
ISOTOPE Neutrons Natural Abundance Half-life Decay Mode
As-75 most common 42 100% Stable —

Here the classroom shortcut, rounded atomic mass (74.922) minus atomic number, gives the same answer: 42.

Data: IAEA Nuclear Data Section, LiveChart of Nuclides, ground-state evaluations, retrieved October 10, 2026. Abundance is the share of atoms in the natural element; a dash means the isotope has no standard natural abundance.

Size, to scale

How big is an arsenic atom?

Radius 119 pm — that is 0.119 nm, so about 4.2 million of them side by side would span a millimetre.

Thermal range

Solid, gas — and when

At ordinary pressure arsenic has no liquid phase at all. It sublimes at 887 K, passing straight from solid to vapour. The 1090 K melting point is real, but only above about 3.63 MPa.

Where it sits

Position in the table

Arsenic sits in period 4, group 15. Everything in group 15 shares the same outer-electron count, which is why they behave so similarly.

Other metalloids

All metalloids

The story

What arsenic is, and how we found it

Arsenic (As) is element 33, a metalloid in group 15, below phosphorus. Its most stable form, gray arsenic, is a brittle, metallic-looking solid with a density of 5.727 g/cm³. At normal pressure it does not melt but turns directly into vapor (sublimes) at 614 °C (887 K); it melts at about 817 °C (1,090 K) only under a pressure of about 36 atmospheres.

Arsenic is best known as a poison. Inorganic arsenic compounds are toxic and cause cancer, and arsenic that dissolves naturally into groundwater affects the drinking water of millions of people.

Atomic structure and isotopes

Arsenic has 33 electrons in four shells, arranged 2, 8, 18, 5, with the configuration [Ar] 3d¹⁰ 4s² 4p³. It forms compounds in the −3, +3 and +5 oxidation states, such as arsine (AsH₃), arsenic trioxide and the arsenates.

Natural arsenic is a single stable isotope, arsenic-75.

The discovery of arsenic

Known since antiquity

The arsenic sulfides orpiment and realgar were used as pigments and medicines in ancient Egypt, Greece, China and India. The name comes from the Greek arsenikon, the word for yellow orpiment, which probably derives from a Persian word for gold-colored.

Albertus Magnus (around 1250)

The German scholar Albertus Magnus is credited with first isolating the element, around 1250, by heating orpiment with soap. In 1649 Johann Schröder published two methods for preparing it.

The poisoner's poison

Arsenic trioxide is tasteless and looks like sugar or flour, which made it a notorious poison from the Middle Ages to the 19th century. In 1836 the British chemist James Marsh developed a sensitive test for arsenic in body tissues, and reliable detection helped end its use for murder.

Recognized as an element

Antoine Lavoisier included arsenic in his 1789 list of chemical elements.

Applications

What arsenic is used for

Semiconductors

Very pure arsenic is combined with gallium to make gallium arsenide (GaAs), a semiconductor used in LEDs, laser diodes, radio-frequency chips in mobile phones and high-efficiency solar cells on satellites. Arsenic is also used in small amounts as a dopant in silicon chips.

Wood preservation and alloys

  • Wood preservative: chromated copper arsenate (CCA) protected outdoor timber against rot and insects. Since 2004 it has no longer been used for residential timber in the United States and Canada, but it is still used for utility poles and some industrial wood.
  • Lead alloys: small additions of arsenic harden lead for battery grids and ammunition.

Medicine

Arsenic trioxide is a standard treatment for acute promyelocytic leukemia, approved in the United States in 2000. Earlier, Salvarsan, an arsenic compound introduced by Paul Ehrlich in 1910, was the first effective treatment for syphilis.

Former uses

Arsenic was once widely used in pesticides and herbicides, in pigments such as Scheele's green and Paris green, and in glassmaking. Most of these uses have ended because of its toxicity.

In everyday life

  • Electronics: phones, Wi-Fi equipment and LEDs contain gallium arsenide chips.
  • Outdoor wood: older decks, fences and playground structures may be made of CCA-treated timber.
  • Food and water: rice, seafood and some groundwater contain arsenic. Most of the arsenic in fish and shellfish is in organic forms, such as arsenobetaine, that are of low toxicity, while rice can contain the more harmful inorganic forms.

Where it comes from

Natural occurrence

1.8 mg/kg of Earth's crust · more abundant than 56% of elements

Abundance

Arsenic makes up about 1.8 parts per million of Earth's crust. It is found in hundreds of minerals and occasionally as the native element.

Minerals

  • Arsenopyrite (FeAsS), the most common arsenic mineral.
  • Realgar (red arsenic sulfide) and orpiment (yellow arsenic sulfide), used as pigments since antiquity.

Production and groundwater

Commercial arsenic trioxide is recovered from the dust and residues of copper, gold and lead smelting; Peru, China and Morocco, in that order, are the largest producers (USGS). Arsenic also dissolves naturally from rocks into groundwater. According to the WHO, an estimated 140 million people in at least 70 countries have been drinking water with arsenic above the WHO provisional guideline of 10 micrograms per liter, including large populations in Bangladesh and India.

Handling

Safety

Health hazards

Inorganic arsenic compounds are highly toxic. A large single dose causes vomiting, abdominal pain and diarrhea and can be fatal. Long-term exposure, mainly through drinking water, causes skin lesions and cancers of the skin, lungs and bladder, and is linked to heart disease and diabetes. The International Agency for Research on Cancer classifies arsenic as carcinogenic to humans.

Arsine and workplace exposure

Arsine (AsH₃), a gas used in the semiconductor industry, is one of the most toxic arsenic compounds: it destroys red blood cells. In the United States the OSHA limit for inorganic arsenic in workplace air is 10 micrograms per cubic meter.

Reducing exposure

  • Test private wells for arsenic, and use treated water if levels exceed 10 micrograms per liter.
  • Do not burn CCA-treated wood, and wash your hands after handling it.
  • Handle arsenic compounds only with ventilation, gloves and protection against dust, and keep them away from acids and reducing agents that can release arsine.

Quick answers

Arsenic: common questions

What is arsenic?

Arsenic (symbol As) is element 33 on the periodic table, a metalloid in period 4, group 15. The classic poison of history — tasteless, undetectable for centuries, and still a groundwater crisis for millions. At room temperature it is a solid.

What is the electron configuration of arsenic?

Arsenic's ground-state electron configuration is [Ar] 3d¹⁰ 4s² 4p³, giving 4 occupied shells with the distribution 2, 8, 18, 5. Its outer shell holds 5 electrons, which is what sets its bonding behaviour.

Does arsenic melt, or does it sublime?

At ordinary pressure arsenic does not melt at all — it sublimes, passing straight from solid to vapour at about 887 K (613.9 °C). A liquid phase only exists above roughly 3.63 MPa, where it melts near 1090 K. That is why a single "melting point" for arsenic is misleading without a stated pressure.

What is the atomic mass of arsenic?

The standard atomic weight of arsenic is 74.922 u. That is a weighted average across its naturally occurring isotopes, which is why it is rarely a whole number.

How many neutrons does arsenic have?

The most common arsenic atom, As-75, has 42 neutrons: its mass number, 75, minus its atomic number, 33. It makes up 100% of natural arsenic. The classroom shortcut, rounded atomic mass (74.922) minus atomic number, gives the same 42.

How dense is arsenic?

Arsenic has a density of 5.727 g/cm³. Water is 1.0 g/cm³, so a block of arsenic is about 5.7× heavier.

What is the electronegativity of arsenic?

Arsenic has a Pauling electronegativity of 2.18. The scale runs from 0.70 (francium, the least greedy for electrons) to 3.98 (fluorine, the most). Values in this middle band tend to form covalent rather than strongly ionic bonds.

Who discovered arsenic, and when?

Arsenic has been known since antiquity, long before anyone recorded its discovery, so no single person can be credited with it. Origin of the name: Greek arsenikon, yellow orpiment.

How common is arsenic on Earth?

Arsenic makes up about 1.8 mg/kg of the Earth's crust — uncommon, but not rare.