what is nitogen cycle
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Nitrogen Cycle:
- Nitrogen is the most abundant element in the atmosphere.
- Nitrogen Cycle is the circulation of nitrogen in various forms through nature.
- It is a biogeochemical process.
- Nitrogen is transformed from its inert atmospheric molecular form to a usable form for plants and other organisms.
- There are mainly five stages in nitrogen cycle. They are discussed below:
1. Nitrogen Fixation:
- Conversion of nitrogen into an organic form is called nitrogen Fixation.
- This process is carried out by microorganisms like Rhizobium.
- Rhizonium is a nitrogen fixing bacteria. It is found in the root nodules of leguminous plants.
2. Nitrification:
- Conversion of nitrite into nitrate is called nitrification.
- Ammonia can be used by some of the plants.
- Nitrogen is converted from bacteria from Ammonia.
3. Assimilation:
- Nitrogen compounds exist in various forms, such as nitrate, nitrite, ammonia, and ammonium etc.
- These are taken up from soil by plants.
- These are then used in the formation of plant and animal proteins.
4. Ammonification:
- When plants or animals die, they emit waste.
- The nitrogen present in this organic matter renters the soil, where it is broken down by decomposers.
- This produces ammonia which is then available for other biological processes.
5. Denitrification:
- Conversion of nitrate back into nitrogen is called denitrification.
- This process is carried out by denitrifying bacteria.
- It occurs primarily in wet soils.
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- Nitrogen is the most abundant element in the atmosphere.
- Circulation of nitrogen in various forms through nature is called nitrogen cycle.
- Nitrogen, a component of proteins and nucleic acids, is essential to life on Earth.
- Although 78 percent by volume of the atmosphere is nitrogen gas, this abundant reservoir exists in a form unusable by most organisms
- Through a series of microbial transformations, however, nitrogen is made available to plants, which in turn ultimately sustain all animal life
- The steps, which are not altogether sequential, fall into the following classifications: nitrogen fixation, nitrogen assimilation, ammonification, nitrification, and denitrification.
- Nitrogen fixation, in which nitrogen gas is converted into inorganic nitrogen compounds, is mostly (90 percent) accomplished by certain bacteria and blue-green algae.
- A much smaller amount of free nitrogen is fixed by abiotic means (e.g., lightning, ultraviolet radiation, electrical equipment) and by conversion to ammonia through the Haber-Bosch process.
- Nitrates and ammonia resulting from nitrogen fixation are assimilated into the specific tissue compounds of algae and higher plants.
- Animals then ingest these algae and plants, converting them into their own body compounds.
- The remains of all living things—and their waste products—are decomposed by microorganisms in the process of ammonification, which yields ammonia (NH₃) and ammonium (NH⁴⁺) (Under anaerobic, or oxygen-free, conditions, foul-smelling putrefactive products may appear, but they too are converted to ammonia in time.)
- Ammonia can leave the soil or be converted into other nitrogen compounds, depending in part on soil conditions.
- Nitrification, a process carried out by nitrifying bacteria, transforms soil ammonia into nitrates (NO₃⁻), which plants can incorporate into their own tissues.
- Nitrates also are metabolized by denitrifying bacteria, which are especially active in water-logged anaerobic soils. The action of these bacteria tends to deplete soil nitrates, forming free atmospheric nitrogen.
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