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Ozone ( / ˈoʊzoʊn /) (or trioxygen) is an inorganic molecule with the chemical formula O. 3. It is a pale blue gas with a distinctively pungent smell. It is an allotrope of oxygen that is much less stable than the diatomic allotrope O. 2, breaking down in the lower atmosphere to O.
- Ozone Layer
Ozone layer. The ozone layer visible from space at Earht's...
- Ozone (Disambiguation)
Fictional characters. Ozone (G.I. Joe), a fictional...
- Dioxygen
Triatomic oxygen (ozone, O 3) is a very reactive allotrope...
- Christian Friedrich Schönbein
Christian Friedrich Schönbein HFRSE (18 October 1799 – 29...
- Allotrope
Diamond and graphite are two allotropes of carbon: pure...
- Ground-level ozone
Ground-level ozone ( O3 ), also known as surface-level ozone...
- Ozone depletion
Ozone depletion consists of two related events observed...
- Ozone Layer
Ozone layer, region of the upper atmosphere, between roughly 15 and 35 km (9 and 22 miles) above Earth’s surface, containing relatively high concentrations of ozone molecules. Approximately 90 percent of the atmosphere’s ozone occurs from 10–18 km (6–11 miles) to about 50 km (about 30 miles) above Earth’s surface.
- Donald Wuebbles
Ozone, or trioxygen, is a chemical with the symbol O3. This means one molecule of ozone is made of three oxygen atoms. Ozone is rarely called trioxygen, even though this is its IUPAC systematic name. [3] Ozone is formed from oxygen gas (O 2) by the action of ultraviolet light and also atmospheric electrical discharges.
- Spacefill model of ozone
- 1101
- 233–069–2
- RS8225000
Ozone is an inorganic molecule with the chemical formula O3. It is a pale blue gas with a distinctively pungent smell. It is an allotrope of oxygen that is much less stable than the diatomic allotrope O2, breaking down in the lower atmosphere to O2 (dioxygen). Ozone is formed from dioxygen by the action of ultraviolet (UV) light and electrical discharges within the Earth's atmosphere. It is ...
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