State the different types of bio-geo-gaseous cycles and explain thebimportance of those cycles.
Answers
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To maintain the concentrations of different naturally occurring substances in the environment, there are mechanisms that constantly recycle these substances. These recycling mechanisms are called biogeochemical cycles. So, biogeochemical cycles are the cyclic flow of nutrients between non-living environment and living organisms.
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Types of Biogeochemical Cycles
There are two major types of biogeochemical cycles
1. Gaseous cycle: These are the biogeochemical cycles in which the reservoir pool is the atmosphere or hydrosphere. For example, carbon cycle, nitrogen cycle etc.
2. Sedimentary cycles: These are the biogeochemical cycles in which the reservoir pool is generally lithosphere. For example, Phosphorous cycle, Sulphur cycle etc.
3.Nitrogen Cycle
The concentration of nitrogen in the atmosphere is about 78%. Nitrogen is essential for all life forms. It is a structural component of many important bio-molecules such as DNA, RNA and vitamins.
The nitrogen cycle involves conversion of nitrogen from its elemental form in the atmosphere into simpler molecules in the soil and water. These further get converted into more complex molecules in living beings. Finally, the complex molecules are reduced and released back into the atmosphere as simple nitrogen molecules.
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Fixing of atmospheric nitrogen involve the following steps:
1. Nitrogen fixation: It is the process wherein atmospheric nitrogen is converted into water-soluble nitrates. This step is performed by organisms like Rhizobium, Azotobacter and blue-green algae.
N2 → NO3− or NH4
2. Nitrification: It is the process in which ammonia is first converted into nitrites and then into nitrates. This step is performed by nitrifying bacteria like Nitrosomonas and Nitrobacter.
NH3 → NO2− → NO3−
3. Assimilation: In this step, NH3 and NO3 are incorporated into the biological tissues.
4. Ammonification: It is the process in which complex, dead organic matter is decomposed into ammonia. This step is performed by organisms like decay bacteria and fungi.
Organic nitrogen compounds → NH4+
5. Denitrification: It is the process wherein the nitrates present in the soil are reduced to release nitrogen back into the atmosphere.
NO3− → N2
Oxygen cycle
Oxygen is an important component of life. We cannot survive without oxygen. It comprises about 21% of atmospheric air. It is also present in dissolved form in water bodies and helps in the survival of aquatic life. In combined form, it is found both in Earth’s crust and in the air. In the air, it occurs as carbon dioxide. In the crust, it is present as oxides of most metals and silicon and also as carbonate, sulphate, nitrate and other minerals.
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Explanation:
Types of Biogeochemical Cycles.
Types of Biogeochemical Cycles.Gaseous cycle: These are the biogeochemical cycles in which the reservoir pool is the atmosphere or hydrosphere. ...
Types of Biogeochemical Cycles.Gaseous cycle: These are the biogeochemical cycles in which the reservoir pool is the atmosphere or hydrosphere. ...Sedimentary cycles: These are the biogeochemical cycles in which the reservoir pool is generally lithosphere. ...
Types of Biogeochemical Cycles.Gaseous cycle: These are the biogeochemical cycles in which the reservoir pool is the atmosphere or hydrosphere. ...Sedimentary cycles: These are the biogeochemical cycles in which the reservoir pool is generally lithosphere. ...Nitrogen Cycle.