1.6 The Phosphorus Cycle

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Phosphorus Sources
- Weathering of rocks that contain P
- Mining P for synthetic fertilizers, detergents, and cleaners
- Weathering of rocks that contain P
- Mining P for synthetic fertilizers, detergents, and cleaners
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Assimilation
- P is absorbed by plant roots and assimilates into tissues; animals assimilate P by eating plants or other animals
- P is absorbed by plant roots and assimilates into tissues; animals assimilate P by eating plants or other animals
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Decomposition
- Animal waste, plant matter, and other biomass is broken down by bacteria/soil decomposers that return phosphate to the soil
- Animal waste, plant matter, and other biomass is broken down by bacteria/soil decomposers that return phosphate to the soil
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Sedimentation
- P does not dissolve well in water
- Falls to the bottom of the ocean as sediment
- Sediment compressed by water pressure
- P does not dissolve well in water
- Falls to the bottom of the ocean as sediment
- Sediment compressed by water pressure
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Geological Uplift
- Tectonic plates collide, forcing up rock layers that form mountains
- P cycle restarts
- Tectonic plates collide, forcing up rock layers that form mountains
- P cycle restarts
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Eutrophication
- Caused by excess P or N
- Major algae bloom -> kills plants below surface -> algae die and bacteria use up O2 to break it down -> low O2 levels kill aquatic animals -> bacteria uses even more O2 to decomp. dead animals
- Caused by excess P or N
- Major algae bloom -> kills plants below surface -> algae die and bacteria use up O2 to break it down -> low O2 levels kill aquatic animals -> bacteria uses even more O2 to decomp. dead animals
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Major reservoirs of P
- Rocks & Sediments
- Rocks & Sediments