まとめ
フレオン,またはクロロフルオロ炭素 (CFC) は,平流層のオゾン層を枯渇させる可能性があります. 継続的な使用は,CFCが段階的に廃止されても,何世紀にもわたって重要なオゾン減少を引き起こす可能性があります.
科学分野:
- 大気化学 大気化学
- オゾン層の研究について
背景:
- クロロフルオロ炭素 (フレオン) は,重層塩素の重要な源として特定されています.
- フレオンからの塩素は,間接的にオゾン層の破壊につながる可能性があります.
研究 の 目的:
- ストラトスフィアのオゾン濃度に対するフリーオン消費の潜在的な影響を評価する.
- フレオンの使用率に基づいて将来のオゾン減少シナリオを予測する.
主な方法:
- モデリング フレオン消費の増加.
- 塩素がオゾン層に及ぼす影響をシミュレートする.
主要な成果:
- オゾン層の減少は1980年までに3%に達し,2000年までに16%に達し,フレオンの年間10%の増加となる.
- 1990年のフリーオンの段階的淘汰でさえ,長期にわたるオゾン層の効果をもたらすだろう.
結論:
- フレオンの排出は,平流層のオゾン層に重大な脅威をもたらす.
- フレオンの環境への影響は,停止後も何百年も続く.
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