Biogeochemical cycle:
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- Any of the natural pathways by which essential elements of living matter are circulated can be called the biogeochemical cycle.
- The term biogeochemical is a contraction that refers to the consideration of the biological, geological, and chemical aspects of each cycle.
- Elements within biogeochemical cycles flow in various forms from the nonliving (abiotic) components of the biosphere to the living (biotic) components and back.
- Each biogeochemical cycle can be considered as having a reservoir pool, a larger (slow-moving, usually abiotic portion), and an exchange (cycling) pool (a smaller but more active portion) concerned with the rapid exchange between the biotic and abiotic aspects of an ecosystem.
- Energy and nutrient circulation are the major functions of the ecosystem. Energy is lost as heat whereas nutrients are recycled indefinitely.
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Types of biogeochemical cycling:
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A nutrient cycle is gaseous or sedimentary based on the nature of the reservoir.
Gaseous cycle:
- The main reservoir of nutrients is the atmosphere and the hydrosphere.
- Gaseous cycles tend to move more rapidly to adjust more readily to changes in the biosphere because of the large atmospheric reservoir.
- Extraordinary disturbances (such as global warming) and more-frequent local disturbances(such as wildfires and storm-driven events) can, however, seriously affect the capacity for self-adjustment.
- Examples: water cycle, oxygen cycle, carbon cycle, nitrogen cycle, etc.
- They are usually perfect- nutrients are replaced as fast as they are utilized.
Sedimentary cycle:
- The main reservoir is the soil and the sedimentary and other rocks of the earth’s crust.
- Sedimentary cycles vary from one element to another, but each cycle consists fundamentally of a solution(or water-related) phase and a rock (or sediment) phase.
- Examples: phosphorus cycle, sulfur cycle, calcium cycle, magnesium cycle, etc.
- These are imperfect as some nutrients lost get locked into sediments and are unavailable for immediate cycling.
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