What it is: The continuous movement of nitrogen atoms between the Earth's atmosphere, soil, and living organisms.
Importance: Nitrogen is an essential component of proteins, nucleic acids (DNA and RNA), and other vital organic molecules necessary for life.
Atmosphere: The largest reservoir of nitrogen, present as nitrogen gas (N₂), which is unusable by most organisms in this form. (Fun fact: the atmosphere is made up of approximately 78% Nitrogen gas.)
Nitrogen Fixation: The conversion of atmospheric nitrogen (N₂) into usable forms of nitrogen compounds (like ammonia, NH₃, or ammonium ions, NH₄⁺). This can occur through:
Nitrification: The conversion of ammonia (NH₃ or NH₄⁺) into nitrites (NO₂⁻) and then into nitrates (NO₃⁻) by specific types of soil bacteria (nitrifying bacteria). Nitrates are the primary form of nitrogen absorbed by plants.
Assimilation: Plants absorb nitrates (NO₃⁻) from the soil through their roots and use them to synthesize proteins and nucleic acids. Animals obtain nitrogen by eating plants or other animals.
Ammonification (Mineralization): When plants and animals die, or when animals excrete waste products, the organic nitrogen compounds are broken down by decomposers (bacteria and fungi) into ammonia (NH₃) or ammonium ions (NH₄⁺), returning nitrogen to the soil.
Denitrification: The conversion of nitrates (NO₃⁻) back into nitrogen gas (N₂) by denitrifying bacteria, which occurs under anaerobic (oxygen-deficient) conditions, often in waterlogged soils. This process returns nitrogen to the atmosphere.
Written by Kasiban Parthipan