๐ In-Depth Theory
Current Composition of the Atmosphere
The Earth's atmosphere has been approximately STABLE for the last 200 million years.
APPROXIMATE COMPOSITION BY VOLUME:
NITROGEN (Nโ): ~78%
OXYGEN (Oโ): ~21%
ARGON (Ar): ~0.9%
CARBON DIOXIDE (COโ): ~0.04% (rising due to human activity)
Other gases: water vapour (variable), neon, helium, methane etc. โ tiny amounts.
Simplified: approximately 4/5 nitrogen and 1/5 oxygen.
The proportions of gases are maintained by:
PHOTOSYNTHESIS โ plants absorb COโ and release Oโ.
RESPIRATION โ all living organisms absorb Oโ and release COโ.
COMBUSTION โ burning fuels consumes Oโ and produces COโ.
NITROGEN CYCLE โ bacteria fix and release Nโ from/to the atmosphere.
Maintaining the Balance
The current balance is maintained by natural CYCLES:
CARBON CYCLE:
COโ absorbed: photosynthesis (plants), dissolving in oceans.
COโ released: respiration, combustion, decomposition, volcanic activity.
OXYGEN BALANCE:
Oโ produced: photosynthesis.
Oโ consumed: respiration, combustion, oxidation of metals.
NITROGEN:
Nโ is extremely unreactive โ doesn't participate in most reactions.
Fixed by nitrogen-fixing bacteria in soil (convert Nโ to nitrates for plants).
Released back by denitrifying bacteria.
Human activities are disrupting these balances:
Burning fossil fuels โ increases COโ.
Deforestation โ reduces COโ absorption and Oโ production.
Industrial processes โ release various gases.
Noble Gases and Water Vapour
ARGON (Ar) โ 0.9%:
A noble gas โ extremely unreactive, single atoms (monatomic).
Present in the atmosphere since the Earth formed โ doesn't participate in any reactions.
Uses: filling light bulbs, welding (inert atmosphere prevents oxidation).
WATER VAPOUR:
Variable amount โ ranges from near 0% in deserts to ~4% in humid tropical air.
Evaporates from oceans, lakes, rivers.
Condenses to form clouds and rain.
Plays a crucial role in weather and climate.
CARBON DIOXIDE โ ~0.04%:
Small but critically important:
ESSENTIAL for photosynthesis โ all plant life depends on it.
GREENHOUSE GAS โ absorbs infrared radiation and warms the Earth.
DISSERVES IN OCEANS โ oceans are a major carbon sink.
RISING due to fossil fuel combustion.
โ ๏ธ Common Mistake
The atmosphere is approximately 78% NITROGEN and 21% OXYGEN โ not the other way round. Many students think oxygen is the main component because we need it to breathe โ but nitrogen is far more abundant. COโ is only about 0.04% โ tiny but critically important for the greenhouse effect and photosynthesis.