The phosphorus cycle differs from the biogeochemical cycles in that:


A. It does not have an atmospheric reservoir.

B. It does not have an oceanic reservoir.

C. There is no assimilation of phosphorus.

D. There is no decomposition of phosphorus



B. It does not have an oceanic reservoir.


The absence of an air tank distinguishes the phosphorus cycle from the other biogeochemical cycles. Although phosphorus does not exist in the atmosphere, it can be found in soil and the ocean. Phosphorous moves through the environment, hydrosphere, and geosphere in a variety of ways. In contrast to other biogeochemical cycles, like as carbon or nitrogen, this typically does not socialize through the atmosphere.


Phosphorus flows through the cycle via rocks, water, soil, residues, and organisms. Rain and enduring cause rocks to release phosphate ions and other reserves over time. This mineral phosphate is subsequently spread throughout the soil and water. Mineral phosphate is taken up by plants from the soil.


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