The Nitrogen Cycle
Nitrogen makes up 78% of our atmosphere, but most living things can't use it directly! Nitrogen fixation converts atmospheric nitrogen into usable forms through several processes. Natural processes like cosmic radiation, meteorite trails, and lightning account for some fixation, but biological fixation is responsible for 90% of it.
Biological nitrogen fixation is performed by special bacteria and cyanobacteria (like Anabaena and Nostoc). These organisms use an enzyme called nitrogenase to break down N₂ gas. Some plants, like Azolla, form partnerships with these bacteria to get nitrogen directly. When organisms die, decomposers break down their proteins through ammonification, releasing ammonia.
The nitrogen cycle continues through nitrification, where bacteria convert ammonia to nitrite (Nitrosomonas bacteria) and then to nitrate (Nitrobacter bacteria). Plants easily absorb nitrates from the soil. Finally, denitrification by bacteria like Pseudomonas converts fixed nitrogen back to N₂ gas, completing the cycle.
🔍 The nitrogen cycle demonstrates an amazing partnership between different organisms: bacteria fix nitrogen, plants use it to grow, animals eat the plants, and decomposers recycle it when organisms die.