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phosphorus cycle
movement of P atoms & molecules between sources & sinks/reservoirs
natural source
weathering of rocks that contain P minerals
synthetic source
synthetic fertilizers that support roles in plant growth
assimilation
the absorption of phosphorus into plant roots and conversion into tissue, or the consumption of plants or animals by other animals
excretion
animal waste, plant matter & other biomass is broken down by bacteria/soil decomposers that return phosphate to soil
decomposition
animal waste, plant matter & other biomass is broken down by bacteria/soil decomposers that return phosphate to soil
sedimentation
phosphate doesn’t dissolve very well into water, much of it forms solid bits of phosphate that fall to the bottom as sediment
geological uplift
tectonic plate collision forcing up rock layers that form mountains; P cycle can start over again with weathering & release of phosphate from rock
eutrophication
excessive richness of nutrients in a lake or other body of water, frequently due to runoff from the land, which causes a dense growth of plant life and death of animal life from lack of oxygen