Ozone Formation by UV Light
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3O2 → 2O3
概要
Ultraviolet radiation (wavelength < 240 nm) splits O₂ molecules in the stratosphere. The resulting oxygen atoms combine with intact O₂ to form ozone (O₃). This Chapman cycle creates the ozone layer at 15–35 km altitude, which absorbs 97–99% of UV-B and UV-C radiation that would otherwise damage DNA.
参加者
| 役割 | 物質 | 係数 | 状態 |
|---|---|---|---|
| 生成物 | Ozone O₃ | 2 | (g) |
日常の例
The ozone layer protects life on Earth from harmful UV radiation. Without it, rates of skin cancer and cataracts would skyrocket.
産業上の重要性
モントリオール議定書(1987年)はオゾンを破壊するフロンを禁止した。オゾン発生装置は水質浄化や空気処理に使用される。
特性
- タイプ
- Photochemical
- 可逆的
- はい
- エネルギー
- 吸熱性
- ΔH
- 285.4 kJ/mol