Differences in the carbon, hydrogen, oxygen, nitrogen, phospheres and sulfur cycles
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Biogeochemical cycles describe the passage and interactions of chemical elements, not all elements are essential in appreciable quantities for life, the most essential for life are carbon, oxygen, nitrogen, calcium, phosphorus, potassium, chlorine, some others are needed but in small amounts such as copper, cobalt and zinc.
The cycles complement each other and allow life in nature, so they represent a cycle of constant transformation that allows you to recycle the materials you use for your benefit. They differ because each one of them fulfills a particular process, in which they give way to a new element.
Among the main characteristics of the cycles are:
Sulfur cycle: sulfur has been absorbed by plants through the roots, sulfur is found in nature in the form of sulfate SO₄. Once it is found in the plants, it is distributed in the organism of the animals that consume the plants. Once carnivorous and herbivorous organisms die and their bodies are broken down by spoilage organisms, these remains return to the soil as nutrients. Once in the soil, it becomes hydrogen sulfide, which, when oxidized, turns the sulfur back into sulfate.
Oxygen Cycle: It is a multicyclonic process since the elements that compose it comply with a specific cycle to be carried out. The oxygen cycle includes the cycles of water, carbon, and oxygen.
Nitrogen Cycle, transforms organic matter into nutrients that are used by plants and in turn by living beings for their food.
Carbon Cycle, carbon is essential for the formation of organic matter and therefore for living beings. Part of the carbon is used by living beings for their metabolism.
Phosphorus cycle, consists of the taking of phosphorus in the form of phosphates from the decomposition of rocks and that are dragged to the ground in their decomposition process.
crown please...