Iron (Fe)
Stable isotopes of iron available from ISOFLEX
Isotope | Z(p) | N(n) | Atomic Mass | Natural Abundance | Enrichment Level | Chemical Form |
Fe-54 | 26 | 28 | 53.939613 | 5.85% | 94.30-99.90% | Metal |
Fe-54 | 26 | 28 | 53.939613 | 5.85% | >99.80% | Oxide |
Fe-56 | 26 | 30 | 55.934941 | 91.75% | ≥99.90% | Metal |
Fe-56 | 26 | 30 | 55.934941 | 91.75% | ≥99.70% | Oxide |
Fe-57 | 26 | 31 | 56.935398 | 2.12% | >95.00% | Metal |
Fe-57 | 26 | 31 | 56.935398 | 2.12% | >95.00% | Oxide |
Fe-58 | 26 | 32 | 57.933280 | 0.28% | 92.80-99.80% | Metal |
Fe-58 | 26 | 32 | 57.933280 | 0.28% | 92.80-99.80% | Oxide |
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Iron has been known since prehistoric times. Genesis says that Tubal-Cain, seven generations from Adam, was “an instructor of every artificer in brass and iron.” Smelted iron artifacts have been identified from as early as 3000 BC. The name “iron” derives from the Anglo-Saxon word iron or iren, and the symbol Fe comes from the Latin word ferrum, meaning “iron.”
Iron is a soft, white, ductile metal, and the fourth most abundant element in earth’s crust. It is the only metal that can be tempered. Its body-centered cubic form is stable to 910 ºC; from 910 ºC to 1390 ºC it has a face-centered cubic form; and above 1390 ºC it returns to the body-centered form. Its mechanical properties are altered by impurities, especially carbon. Iron is highly reactive chemically, it is a strong reducing agent, and it oxidizes readily in moist air and reacts with steam when hot to yield hydrogen and iron oxides. It is attracted by magnets and rapidly loses its magnetism. It is ferromagnetic at ordinary temperatures but becomes paramagnetic when heated to its Curie point of 768 ºC.
Iron exhibits single-replacement reactions, precipitating less electropositive metals out of their salt solutions. Thus, solid iron can reduce many metals, such as copper, silver, gold, mercury, tin and nickel. Solid iron undergoes rusting by reacting with oxygen in the presence of water; in moist air, it rapidly converts to rust.
Iron occurs in every mammalian cell and is vital for life processes. It is bound to various proteins and is found in blood tissues. Industrial uses of iron as carbon steels are numerous, surpassing the uses of any other alloys (carbon steels are alloys of iron containing carbon in varying proportions). Non-steel iron alloys such as cast iron, wrought iron, nickel iron and silicon iron have many important applications as well. Another important application of iron is as an industrial catalyst: it is used in catalyst compositions in the Haber process for synthesis of ammonia, and in the Fischer-Tropsch process for producing synthetic gasoline.
Properties of Iron
Name | Iron |
Symbol | Fe |
Atomic number | 26 |
Atomic weight | 55.847 |
Standard state | Solid at 298 °K |
CAS Registry ID | 7439-89-6 |
Group in periodic table | 8 |
Group name | None |
Period in periodic table | 4 |
Block in periodic table | d-block |
Color | Lustrous, metallic, grayish tinge |
Classification | Metallic |
Melting point | 1535 °C |
Boiling point | 2750 °C |
Thermal conductivity | 79.5 W/(m·K) |
Electrical resistivity | 4.71 µΩ·cm at 0 °C |
Electronegativity | 1.83 |
Heat of vaporization | 347 kJ·mol-1 at 2750 °C |
Heat of fusion | 13.8 kJ·mol-1 |
Density of liquid | 7.00 g/cm3 at 1564 ºF |
Density of solid | 7.873 g/cm3 |
Electron configuration | [Ar]3d64s2 |
Atomic radius | 1.24 Å |
Most common oxidation states | +2, +3 |
Other oxidation states | -1, 0, +1, +4, +6 |
Research
- Pressure-dependent isotopic composition of iron alloys
- Characterization of hydrothermal sources of iron in the oceans - Constraints from iron stable isotopes
- Iron isotopes as a potential tool for ancient iron metals tracing
- Iron isotopic fractionation between silicate mantle and metallic core at high pressure
- Triggered Star Formation Inside the Shell of a Wolf-Rayet Bubble as the origin of the Solar System
- Photobiological Effects at Earth’s Surface Following a 50 pc Supernova
- Triggering Collapse of the Presolar Dense Cloud Core and Injecting Short-lived Radioisotopes with a Shock Wave. V. Nonisothermal Collapse Regime
- Potential use of Fe isotopes for ancient non-ferrous metals tracing through the example of a lead-silver production site (Imiter mine, Anti-Atlas, Morocco)
- The importance of lawniron ores for the reconstruction of origin using iron isotopes
- From Cosmic Explosions to Terrestrial Fires?
- Interstellar 60Fe in Antarctica