摘要
大气中的O_3主要是O_2吸收阳光中的紫外辐射生成的;即使没有人为的臭氧消耗性物质。O_3也在不断分解和消耗、O_3的生成和消耗若能保持平衡.则臭氧层保持稳定。否则臭氧层将变稀薄:分析了极地冬半年大气受紫外辐射微弱。O_3的生成量剧减.但O_3的分解和消耗却在继续.结果出现臭氧层薄弱区;认为北极必然与南极一样在冬半年有臭氧层薄弱区。
Most of ozone in the atmosphere is made from molecular oxygen by the shining of ultraviolet ray from sunlight. Ozone in the atmosphere is also continue resolved and depleted in some chemical reactions. even if there is no man-made ozone deplete materials. If the reactions of ozone synthesis and resolution are in balance. the ozonosphere is stable; analyses that ultraviolet ray is very weak in the half year of winter at the Poles, area, so the synthesize amount of ozone is abated. but the depletion of ozone goes continue. the result is that the ozonospere becomes meagre; Just like in the South Pole. in the North Pole there should be ozonosphere thiner area in the half year of winter.
出处
《国土与自然资源研究》
2000年第2期49-51,共3页
Territory & Natural Resources Study
关键词
臭氧层薄弱区
板地
紫外线辐射
大气污染
the Poles area
ultraviolet ray
the half year of winter
ozonosphere thiner area