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New Directions: How dangerous is ozone?

机译:新方向:臭氧有多危险?

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Approximately one hundred years after the discovery of ozone, it was found that many human activities (e.g. combustion which leads to the formation of nitrogen oxides and volatile organic compounds) increase the concentration of ozone at the surface of our earth. Several groups have considered the high mortality rates of the 2003 heat wave in the UK and the Netherlands and have linked it to the concentrations of particulate matter and ozone that prevailed at that time (Fischer et al., 2004, Atmospheric Environment 38, 1083; Sted-man, 2004, Atmospheric Environment 38, 1087). This causes some concern because ozone at the surface of the earth can damage and destroy both plants and animals. As a result, the high ozone concentrations and their long persistence times have now become a new and frightening aspect of life on our planet. At genesis, some 4000 million years ago, all life was anaerobic. The gradual accumulation of atmospheric oxygen introduced both opportunity and risk; some anaerobes began to "breathe" it and to create a completely new route for the production of energy through respiration: hence, the ascent of aerobes some 2000 million years ago.
机译:发现臭氧大约一百年后,人们发现许多人类活动(例如燃烧导致形成氮氧化物和挥发性有机化合物)增加了地球表面臭氧的浓度。有几个小组考虑了英国和荷兰2003年热浪的高死亡率,并将其与当时盛行的颗粒物和臭氧的浓度联系起来(Fischer等人,2004年,《大气环境》 38期,第1083页;斯特德曼,2004年,《大气环境》 38,1087)。这引起了一些关注,因为地球表面的臭氧会破坏和破坏动植物。结果,高浓度的臭氧及其长的持续时间现在已成为地球上生命的一个新的令人恐惧的方面。在大约40亿年前的创世纪,所有生命都是厌氧的。大气中氧气的逐渐积累既带来了机遇,也带来了风险。一些厌氧菌开始“呼吸”,并为通过呼吸产生能量的生产开辟了一条全新的途径:因此,大约20亿年前,有氧菌的崛起。

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