The nitrogen cycle depicts the flow of nitrogen through the natural world. Nitrogen is a vital element for life; it is present in amino acids, proteins, and DNA.

Additionally, nitrogen is the most prevalent element in the atmosphere (78%). However, nitrogen must be "fixed" into another form before living organisms may utilise it.

Fixation by lightning: The energy of lightning causes the combination of nitrogen (N2) and water (H2O) to generate ammonia (NH3) and nitrates (NO3). Precipitation transports ammonia and nitrates to the soil, where plants can absorb them.

Nitrogen Fixation

Biological fixation: Approximately 90 percent of nitrogen fixation is performed by bacteria. Nitrogen is converted by cyanobacteria into ammonia and ammonium: N2 + 3 H2 2 NH3. Then, plants can utilise ammonia directly. Ammonia and ammonium may undergo further reactions throughout the nitrification procedure.

Nitrogen Fixation

Nitrification occurs by the following reactions: 2 NH3 + 3 O2 → 2 NO2 + 2 H+ + 2 H2O 2 NO2- + O2 → 2 NO3-

Nitrification

Aerobic bacteria convert ammonia and ammonium using oxygen. Nitrosomonas bacteria transform nitrogen into nitrite (NO2-), and subsequently Nitrobacter transforms nitrite into nitrate (NO3-). Some bacteria have a symbiotic connection with plants (legumes and certain root-nodule species), and plants use nitrate as a nutrition. Meanwhile, mammals receive nitrogen through consuming plants or animals that consume plants.

Nitrification

Bacteria turn nitrogen nutrients back into ammonium ions and ammonia when plants and animals die. This transformation is known as ammonification. Through the process of denitrification, anaerobic bacteria can convert ammonia into nitrogen gas. NO3- + CH2O + H+ → ½ N2O + CO2 + 1½ H2O Denitrification returns nitrogen to the atmosphere, completing the cycle.

Ammonification