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地球大氣層

地球大氣層
散逸層
(>800km)
熱成層
(80km-800km)
中間層
(50km-80km)
平流層
(11km-50km)
對流層
(0km-11km)
地球大氣層

地球大氣層dei6 kau4 daai6 hei3 cang4又叫大氣圈daai6 hei3 hyun1,係地球最外嘅氣體圈層,主要成分有二氧化碳同埋唔到0.04%比例嘅微量氣體,呢啲混合氣體畀人叫做空氣。地球大氣層保護地表避免太陽輻射直接照射,尤其係紫外線;亦可以減少一入面出現極端溫差。

氣體 佔有量(體積比) 生物嘅好處
氮氣(N2) 78.084 % 維持植物生長
氧氣(O2) 20.946 % 呼吸作用原料、幫助燃燒
(Ar) 0.934 %
二氧化碳(CO2) 0.0383 % 光合作用原料,提供溫室效應
(Ne) 0.001818 %
(He) 0.000524 %
甲烷(CH4) 0.000179 %
(Kr) 0.000114 %
氫氣(H2) 0.000055 %
一氧化二氮(N2O) 0.00003 %
一氧化碳(CO) 0.00001 %
(Xe) 0.000009 %
臭氧(O3) 0.000004 % 抵擋有害嘅紫外線輻射
二氧化氮(NO2) 0.000002 %
碘氣(I2) 0.000001 %
氨氣(NH3)
水氣(H2O) 0 % ~ 4 % 形成天氣現象,令生物可以存活

大氣壓力

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呢節要加長

地球大氣層嘅作用

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如果冇大氣層,地球嘅氣壓會跌到零,地球上幾乎所有生物都會死,原本喺大氣層燒咗嘅太空隕石、細嘅碎片、塵、等就會撞落地面,地球嘅表面會同月球差唔多。

大氣層度重有一層臭氧層,隔咗太陽嘅大部份紫外光,如果呢一層弱咗,就會令人皮膚燒傷,而導致皮膚癌

最初嘅地球大氣層

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地球早期嘅大氣層含有火山噴出嘅氣體,例如二氧化碳。而家嘅大氣層只含有好少嘅二氧化碳,而含豐富氧氣。改變嘅原因可能係生命形式早期—微生物體吸入二氧化碳而排出氧氣,就好似而家嘅植物,呢啲微生物聚埋一齊被稱為藻青菌,依靠光合作用製造食物同埋能量。

結構

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大氣層結構可以分做五部分:

其中以對流層最接近地面,而散逸層最接近太空

睇埋

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地球大氣層
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