Metallurgy and steel
Iron is used in iron and steel processing, either as an alloying element, a refining aid or part of the ore-to-metal chemistry.
Iron is element 26 (Fe), located in period 4, group 8 and the d block. At room temperature its reference phase is solid. Its electron configuration is [Ar] 3d6 4s2.
The d subshell participates in the chemistry of iron. Transition metals can use electrons of similar energies in bonding, which is why variable oxidation states, coordination compounds and catalytic behaviour are common across the d block.
Its electron configuration, [Ar] 3d6 4s2, should be read together with the oxidation state of the compound: removing electrons changes which d orbitals are occupied and can alter colour, magnetism, bonding and reactivity.
For iron, important chemical forms include metals and alloys, oxides, halides and coordination compounds. Variable oxidation states are common because s and d electrons have similar energies, and ligands around the metal ion can strongly alter colour, magnetism and reactivity.
The reference phase at room temperature is solid. The listed density is 7.874 g/cm³. The melting point is 1 811 K (1 538 °C). The boiling point is 3 134 K (2 861 °C). Pressure, purity and crystal structure can shift measured physical properties.
In practice, iron is encountered in metallurgy and steel, construction and biology.
Iron is used in iron and steel processing, either as an alloying element, a refining aid or part of the ore-to-metal chemistry.
Iron is used in structural materials, coatings, cement chemistry or alloys chosen for mechanical durability.
Iron ions or compounds participate in biological structures, enzymes, signalling or metabolism.
Iron is in period 4 and group 8. In the neighbourhood shown here, it lies between manganese and cobalt in the same period; ruthenium is directly below it in the same group. These positions make it possible to compare atomic size, ionisation energy and bonding behaviour with nearby elements.
Values describe the element or neutral atom where applicable. Physical data can depend on allotrope, pressure and measurement conditions.
Use of iron is recorded from about 5000 BC. This predates modern chemistry, so early use, chemical identification and the later atomic-number definition are separate stages.
The standard atomic weight is 55.845(2). This value refers to the isotopic composition of natural terrestrial material, not to the mass of one specific atom.
Iron has at least one stable isotope. Different isotopes have the same number of protons and therefore the same element identity, but different neutron numbers and atomic masses.
The hazards associated with iron depend on chemical form, dose and route of exposure. Pure iron, its ions and its compounds can have very different biological and environmental effects, so safety data should be checked for the actual substance being handled.