i 6 Marks

Explain carbon emission and absorption in nature.

Answer: Carbon Emission and Absorption in Nature

The Carbon Cycle is the continuous movement of carbon atoms between the atmosphere, oceans, land, and living organisms. In nature, carbon is constantly being released (emission) and taken up (absorption) through various biological, chemical, and physical processes, maintaining a dynamic equilibrium that has been disrupted by human activities.

1. Natural Carbon Emission Sources

A. Biological Processes:

B. Geological/Physical Processes:

Photosynthesis: 6CO2 + 6H2O + Light → C6H12O6 + 6O2

Respiration: C6H12O6 + 6O2 → 6CO2 + 6H2O + Energy

2. Natural Carbon Absorption (Sinks)

A. Terrestrial Sinks:

Sink Mechanism Carbon Stored
Photosynthesis Plants convert CO2 to glucose using sunlight ~120 Gt C/year absorbed
Forests Trees store carbon in wood, leaves, roots ~450 Gt C in biomass
Soil Organic matter, humus, peat accumulation ~1,500 Gt C (top 1m)
Grasslands Root systems store carbon underground 30% of terrestrial carbon

B. Oceanic Sinks:

Ocean's Role: Oceans absorb approximately 25% of human CO2 emissions annually (~10 Gt CO2), making them the largest active carbon sink. However, this causes ocean acidification (pH drop from 8.2 to 8.1 since industrialization).

3. Carbon Reservoirs

Reservoir Carbon Content (Gt C) Exchange Rate
Atmosphere ~870 Fast (days to years)
Oceans ~38,000 Medium (decades to centuries)
Terrestrial Biosphere ~2,000 Fast (seasonal to decades)
Soil ~1,500 Slow (decades to centuries)
Fossil Fuels ~4,000 Very slow (millions of years)

4. Natural Carbon Balance

Before industrialization, natural emissions and absorptions were roughly balanced:

5. Human Disruption of Balance

Key Statistic: Human activities add ~40 Gt CO2/year to the natural carbon cycle. Natural sinks absorb only ~50% (~20 Gt), leaving the rest to accumulate in the atmosphere.

Conclusion

In nature, carbon continuously cycles between atmosphere, land, and oceans through processes like photosynthesis, respiration, decomposition, and ocean exchange. For millennia, natural emissions and absorptions remained balanced, maintaining stable atmospheric CO2 levels. However, human activities - primarily fossil fuel combustion and deforestation - have disrupted this balance by adding approximately 40 Gt CO2 annually to the cycle. Since natural sinks can only absorb about half of these emissions, excess carbon accumulates in the atmosphere, driving climate change. Protecting and enhancing natural carbon sinks (forests, oceans, soils) is essential for climate mitigation alongside emission reductions.

Sources: Module 1 Notes | Global Carbon Project | IPCC AR6 | NASA Carbon Cycle