What is the Biogeochemical Cycle in nature? (short definition)
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Biogeochemical Cycle Definition. A biogeochemical cycle is one of several natural cycles, in which conserved matter moves through the biotic and abiotic parts of an ecosystem. In biology, conserved matter refers to the finite amount of matter, in the form of atoms, that is present within the Earth.
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Biogeochemical cycle, any of the natural pathways by which essential elements of living matter are circulated. 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. In order for the living components of a major ecosystem (e.g., a lake or a forest) to survive, all the chemical elements that make up living cells must be recycled continuously. Each biogeochemical cycle can be considered as having a reservoir (nutrient) 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.
Biogeochemical cycles can be classed as gaseous, in which the reservoir is the air or the oceans (via evaporation), and sedimentary, in which the reservoir is Earth’s crust. Gaseous cycles include those of nitrogen, oxygen, carbon, and water; sedimentary cycles include those of iron, calcium, phosphorus, sulfur, and other more-earthbound elements.
Gaseous
cycles tend to move more rapidly than do sedimentary ones and to adjust
more readily to changes in the biosphere because of the large
atmospheric reservoir. Local accumulations of carbon dioxide (CO2), for example, are soon dissipated by winds or taken up by plants. 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.
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Elements within biogeochemical cycles flow in various forms from the nonliving (abiotic) components of the biosphere to the living (biotic) components and back. In order for the living components of a major ecosystem (e.g., a lake or a forest) to survive, all the chemical elements that make up living cells must be recycled continuously. Each biogeochemical cycle can be considered as having a reservoir (nutrient) 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.
Biogeochemical cycles can be classed as gaseous, in which the reservoir is the air or the oceans (via evaporation), and sedimentary, in which the reservoir is Earth’s crust. Gaseous cycles include those of nitrogen, oxygen, carbon, and water; sedimentary cycles include those of iron, calcium, phosphorus, sulfur, and other more-earthbound elements.
Gaseous
cycles tend to move more rapidly than do sedimentary ones and to adjust
more readily to changes in the biosphere because of the large
atmospheric reservoir. Local accumulations of carbon dioxide (CO2), for example, are soon dissipated by winds or taken up by plants. 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.
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