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Suyun dunya yuzeyi ile atmosfer arasinda kati sivi ve gaz hallerini birbirinden digerine donuserek yer degistirmesine su dongusu denir Su dongusunde buharlasma yogusma terleme bosaltim fotesentez solunum gibi olaylar etkiler su dongusu sayedinde dunya bulunan su surekli yer degistirir fakat hic kaybolmaz yani suan ictiginiz su milyonlarca yil once dinozorlarin ictigi su ile su olabilir Karbon karbondioksit protein yag DNA gibi bir cok molekulun yapisinda bulunur Karbon temel kaynagi atmosverdeki karbondioksit gazdir. fotosentez sirasinda karbondioksit yolu ile bitkiler tarafindan kullanilan karbon besinler yapisinda ve besinler yoluyla da diger canlilarin yapsina katilir solunum sirasinda bu besinlerde bulunan karbon karbondioksit gazi olarak tekrar atmosfere verilir fosil yakitlarin (komur petrol dogal gaz )yapisinda karbonda yanma sonucunda aciga cikarak havaya karisir . ayrica ayristiricilar da havadaki karbondioksit miktarini artirir . Atmosferde gazlarin %21ini oksijen gazi olusturur .
Canlilar solunum sonuunda havadaki oksijen alip karbondioksit verirler fotosentez yapan canlilar atmosferde karbondioksit gazina kulanilir atmosver geri oksijen gazi verirler Dogadaki oksijen gazinin bu cevremizde oksijen dongusu denir Atmosferdeki gazlarin %78ini azot gazi olusturur Proteinler yapisinda azot bulunur bazi mikrooganizma haric canlilar azot gazina dogrudan dogruya kulanilalidir Havadaki azot simsek veya yildirim olaylari sonucunda azotlu bilesikler donuserek toprega gecer
Topraktaki azotlu bilesikler once bitkilerin yapisina sonra da besin zinciri yolu ile hayvanlarin yapisina gecer Ayrica bakterilerin koklerinde azot baglayici bakteriler havadaki serbest azot tutarak bakterilerin yapisina aktarmasina saglar . Canlilar aktarilan veya olmeleri sonucu ayristiricilar bu azotu ayristirici tekrar atmosfere aktarmalarina

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