Iron
Iron is a chemical element in the periodic table that has the symbol Fe (L.: Ferrum) and atomic number 26. Iron is a group 8 and period 4 metal. Iron is notable for being the final element produced by stellar nucleosynthesis, and thus the heaviest element which does not require a supernova or similarly cataclysmic event for its formation. It is therefore the most abundant heavy metal in the universe.
Compounds
Common oxidation states of iron include:
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- the Iron(II) state, Fe2+, previously ferrous is very common.
- the Iron(III) state, Fe3+, previously ferric, is also very common, for example in rust.
- the Iron(IV) state, Fe4+, previously ferryl, stabilized in some enzymes (e.g. peroxidases).
- the Iron(VI) state, Fe6+ is also known, if rare, in potassium ferrate.
Iron carbide Fe3C is known as cementite.
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~ Table of Content ~
| ► | Introduction |
| ► | Notable characteristics |
| ► | Applications |
| ► | History |
| ► | Occurrence |
| ► | Extraction from ore |
| ► | Compounds |
| ► | Biological role |
| ► | Isotopes |
| ► | Precautions |
| ► | References |
| ► | External links |
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