Oxygen is a colorless, odorless, reactive gas essential for most life forms. It supports combustion and forms about 21% of Earth's atmosphere. It commonly exists as a diatomic molecule (O₂).
In aerobic organisms, O2 is the terminal electron acceptor in the electron transport chain. Electrons from NADH/FADH2 reduce O2 to water, driving ATP synthesis.
\(\mathrm{C_6H_{12}O_6 + 6\,O_2 \rightarrow 6\,CO_2 + 6\,H_2O + \text{energy (ATP)}}\)
This high redox potential of O2 makes energy capture efficient.
No. Combustion is a redox reaction where a fuel is oxidized by an oxidizer (often O2). Oxygen usually acts as the oxidizer, not the fuel. However, oxygen can react with even more powerful oxidizers (e.g., fluorine), but under normal conditions we say O2 does not "burn"—it enables burning.
Most common is −2 (e.g., H2O, CO2). Special cases include:
Industrial: Fractional distillation of liquefied air after removing CO2 and H2O. Liquid O2 (b.p. ~90 K) is separated from N2 (b.p. ~77 K).
Laboratory: Decomposition of hydrogen peroxide using a catalyst (MnO2):
\(\mathrm{2\,H_2O_2(aq) \xrightarrow{MnO_2} 2\,H_2O(l) + O_2(g)}\)
O2 is a diatomic molecule essential for respiration; it is relatively stable. O3 is a triatomic allotrope (bent structure) and a much stronger oxidant. In the stratosphere, ozone absorbs harmful UV radiation; at ground level, it can be a pollutant.
\(\mathrm{O_2 + O\cdot \rightarrow O_3}\)
Photosynthetic organisms release O2 by splitting water:
\(\mathrm{6\,CO_2 + 6\,H_2O \xrightarrow{light,\;chlorophyll} C_6H_{12}O_6 + 6\,O_2}\)
Over geological time, this process oxygenated Earth’s atmosphere, enabling aerobic life.
Glowing splint test: A glowing wooden splint inserted into a sample re-lights in O2 due to enhanced combustion.
Paramagnetism: Liquid oxygen is pale blue and strongly paramagnetic; O2 is attracted into a magnetic field because it has two unpaired electrons in antibonding \(\pi^*\) orbitals.
Hydrogen burns in oxygen to form water:
\(\mathrm{2\,H_2(g) + O_2(g) \rightarrow 2\,H_2O(l)}\)
The reaction is highly exothermic (\(\Delta H^\circ < 0\)), releasing about \(\mathrm{\approx -286\,kJ\,mol^{-1}}\) per mole of water formed (value depends on phase/conditions).
As oxygen forms bonds, it typically gains electrons (is reduced), causing other species to lose electrons (be oxidized). For example, in metal oxidation:
\(\mathrm{4\,Fe + 3\,O_2 \rightarrow 2\,Fe_2O_3}\)
Oxygen’s high electronegativity and ability to stabilize the \(\mathrm{O^{2-}}\) state drive these processes.
O2 itself is not flammable, but it greatly accelerates combustion and lowers ignition temperatures of fuels. Safety tips: