Respiration
Oxygen chemistry supports aerobic respiration by accepting electrons in cellular metabolism.
Oxygen is element 8 (O), located in period 2, group 16 and the p block. At room temperature its reference phase is gas. Its electron configuration is [He] 2s2 2p4.
Group 16 atoms have six valence electrons. Bonding often involves gaining or sharing two electrons, while the heavier members can access a wider range of oxidation states.
For oxygen, this outer-shell structure helps explain the importance of oxides, sulfides, oxoanions and covalent compounds across the chalcogen family.
Elemental oxygen is mainly O₂, with ozone O₃ as another molecular form. In compounds, oxygen forms oxides, hydroxides, oxoanions and covalent bonds throughout mineral and biological chemistry. The −2 oxidation state is especially common, with important exceptions such as peroxides.
The reference phase at room temperature is gas. The listed density is 1.429 g/L. The melting point is 54.37 K (-218.8 °C). The boiling point is 90.19 K (-183 °C). Pressure, purity and crystal structure can shift measured physical properties.
In practice, oxygen is encountered in respiration, metallurgy, steel and water treatment.
Oxygen chemistry supports aerobic respiration by accepting electrons in cellular metabolism.
Oxygen is used in extraction, refining, alloying or heat-treatment processes that control the properties of metals.
Oxygen changes the properties of steels or appears in steelmaking chemistry and alloy design.
Oxygen is used in disinfection, purification, oxidation or treatment chemistry.
Oxygen is in period 2 and group 16. In the neighbourhood shown here, it lies between nitrogen and fluorine in the same period; sulfur 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.
The discovery of oxygen is associated with Carl Wilhelm Scheele. Recognition of the element, isolation of a pure sample and assignment of its modern atomic number did not necessarily occur at the same time.
The standard atomic weight is given as the interval [15.99903, 15.99977]. Natural samples can differ slightly in isotope proportions, so a single universal decimal value would hide real variation between materials.
Oxygen 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 oxygen depend on chemical form, dose and route of exposure. Pure oxygen, 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.