Carbon Dioxide and Methane — Sources and Properties
CO₂ and CH₄ are the major greenhouse gases — their rising atmospheric concentrations are driving global warming.
Carbon dioxide (CO₂):
- Sources: Combustion of fossil fuels (coal, oil, gas); respiration; volcanic eruptions; decomposition; deforestation (reduces absorption)
- Properties: Colourless, odourless gas; denser than air; does not support combustion (unlike O₂); acidic (dissolves to form carbonic acid, H₂CO₃)
- Tests: Turns limewater milky (Ca(OH)₂ + CO₂ → CaCO₃ + H₂O); turns hydrogen carbonate indicator yellow
- Uses: Carbonated drinks (dissolved under pressure); fire extinguishers; greenhouse horticulture; dry ice (solid CO₂ for refrigeration)
Methane (CH₄):
- Sources: Decomposition of organic matter in waterlogged conditions (bogs, rice paddies, landfill); cattle digestion (enteric fermentation); natural gas extraction leaks
- Properties: Colourless, odourless, highly flammable gas; burns → CO₂ + H₂O
- Greenhouse potency: ~25× more potent than CO₂ over 100 years (stronger absorption of infrared)
The greenhouse effect:
- Sun's energy (shortwave radiation) passes through atmosphere → heats Earth's surface
- Earth radiates heat as infrared (longwave) radiation upward
- Greenhouse gases (CO₂, CH₄, H₂O, N₂O) absorb some of this infrared
- They re-radiate it in all directions → some returns to Earth surface → warms atmosphere
- Enhanced greenhouse effect: higher CO₂ and CH₄ → more heat retained → global temperature rise
Consequences: Sea level rise (ice melt + thermal expansion), extreme weather (floods, droughts), habitat loss, ocean acidification, agricultural disruption.
- CO₂ sources: combustion, respiration, decomposition. Test: limewater milky.
- CH₄ sources: cattle, landfill, paddy fields, natural gas. 25× more potent than CO₂.
- Greenhouse gases absorb infrared → re-radiate → warms Earth (enhanced if concentration rises).