Understanding the Nitrogen Cycle
The nitrogen cycle is a crucial ecological process that involves the transformation of nitrogen in various forms. Key stages include:
- Nitrogen Fixation: Atmospheric nitrogen (N₂) is converted into ammonia (NH₃) by nitrogen-fixing bacteria like Rhizobium, found in root nodules of legumes.
- Nitrification: Ammonia is oxidized to nitrites (NO₂⁻) and then to nitrates (NO₃⁻) by nitrifying bacteria such as Nitrosomonas and Nitrobacter.
- Assimilation: Plants absorb nitrates from the soil and use them to synthesize proteins and nucleic acids. Herbivores then consume these plants, incorporating nitrogen into their bodies.
- Ammonification: Decomposers, including bacteria and fungi, break down organic matter, releasing ammonia back into the soil.
- Denitrification: Denitrifying bacteria, such as Pseudomonas, convert nitrates back into nitrogen gas (N₂), returning it to the atmosphere.
This cycle is vital for maintaining ecosystem health and fertility.
Key points to remember
- Nitrogen fixation converts atmospheric nitrogen into ammonia.
- Nitrification involves bacteria converting ammonia to nitrates.
- Plants assimilate nitrates to build proteins.
- Decomposers release ammonia during ammonification.
- Denitrification returns nitrogen to the atmosphere.
Worked example
Describe the nitrogen cycle, mentioning key organisms involved.
- Nitrogen fixation occurs via Rhizobium in legumes.
- Nitrification is carried out by Nitrosomonas and Nitrobacter.
- Plants assimilate nitrates, and Pseudomonas facilitates denitrification.