Phosphorus Cycle Basics
Phosphorus Sources and Weathering
Human Impacts
Phosphorus Assimilation and Decomposition
Phosphorus and the Geological Cycle
100

This cycle describes the movement of phosphorus atoms and molecules between reservoirs.

Phosphorus cycle

100

This natural process slowly breaks down rocks to release phosphate into soil and water.

Weathering

100

This activity speeds up rock weathering and phosphorus release by breaking rocks into smaller pieces.

Mining

100

Plants absorb phosphorus primarily through these structures.

Roots

100

This process involves small particles of rock settling and accumulating to form soil or sediment.

Sedimentation

200

Phosphorus is mainly stored in this type of Earth material.

rocks and sediments

200

Phosphate is carried from rocks to soil and water by these natural forces.

Wind and rain

200

These agricultural products contain phosphate and can lead to runoff pollution.

Synthetic fertilizers
200

Animals obtain phosphorus by consuming these.

Plants and/or other animals

200

Over long periods, sedimented phosphorus can become this type of rock.

Sedimentary rocks

300

Unlike nitrogen or carbon, phosphorus does not have this phase in its cycle.

gaseous phase

300

Because phosphorus is released slowly, it often limits this biological process in ecosystems.

Plant growth

300

This household product can contribute phosphorus to waterways if not fully removed during treatment.

Detergents/Cleaners

300

The breakdown of dead organisms and waste to release phosphorus back into the environment is done by these organisms.

Decomposers

300

This geological event can expose sedimentary phosphorus rocks, restarting the cycle.

Geological uplift

400

The phosphorus cycle is much slower than these two other biogeochemical cycles.

carbon and nitrogen cycles

400

This term describes nutrients like phosphorus that limit ecosystem productivity due to their scarcity.

Limiting nutrient

400

Wastewater treatment plants often do not completely remove this nutrient before releasing water into rivers.

Phosphate

400

Decomposers release nutrients from dead matter through this process.

Decomposition

400

Phosphorus buried in sedimentary rock remains unavailable for this reason.

locked away until it weathers

500

This molecule represents the form phosphorus takes in rocks and is important biologically.

Phosphate

500

The phosphate released from weathered rocks is sometimes dissolved in this.

Water
500

Excess phosphorus runoff into water bodies often contributes to this environmental problem.

Eutrophication

500

This type of nutrient cycling includes the absorption and buildup of phosphorus by organisms.

Assimilation

500

Sedimentation in aquatic environments contributes phosphorus to these long-term storage reservoirs.

sedimentary rocks

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