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Updated: Jun 6, 2026

Measuring Phosphorus Release in Laboratory Microcosms for Water Quality Assessment
Published on: July 22, 2019
Phosphorus transformations during decomposition of wetland macrophytes.
Alexander W Cheesman1, Benjamin L Turner, Patrick W Inglett
1Wetland Biogeochemistry Laboratory, Soil and Water Science Department, University of Florida, Gainesville, Florida, United States. CheesmanA@si.edu
Wetland leaf litter decomposition sequesters phosphorus (P) in nutrient-rich soils by forming microbial P compounds. In contrast, P sequestration is limited in nutrient-poor soils, indicating P pools are independent of litter decomposition.
Area of Science:
- Environmental Science
- Soil Science
- Microbiology
Background:
- Detrital phosphorus (P) transformation in wetlands is crucial for P cycling and soil sequestration.
- Understanding P dynamics in macrophyte leaf litter is key to predicting wetland ecosystem responses to nutrient changes.
Purpose of the Study:
- To investigate changes in phosphorus (P) forms during sawgrass and cattail leaf litter decomposition.
- To compare P sequestration in subtropical wetland soils with differing nutrient statuses.
Main Methods:
- Analysis of phosphorus forms in leaf litter of sawgrass (Cladium jamaicense) and cattail (Typha domingensis).
- 15-month decomposition study at two sites with contrasting nutrient levels in a Florida subtropical wetland.
- Comparison of P sequestration rates and P forms between nutrient-enriched and unenriched sites.
Main Results:
- Nutrient-enriched sites showed net P sequestration, with P accumulating in microbial cell-like forms (phosphodiesters, pyrophosphate).
- Unenriched sites exhibited minimal P sequestration, with P form changes limited to the loss of initial leaf litter compounds.
- P pools in nutrient-poor wetland soils were largely unaffected by heterotrophic decomposition of macrophyte litter.
Conclusions:
- Nutrient-rich conditions promote P sequestration via microbial P accumulation and potential concentration of macrophyte P.
- In nutrient-poor wetlands, soil P pools appear decoupled from macrophyte leaf litter decomposition.
- Findings impact predictions of P sequestration stability and rates in wetlands under varying nutrient loads.
Related Concept Videos
The Phosphorus Cycle
Microbial Wastewater Treatment
Freshwater Microbial Ecology
Metabolism of Chemolithotrophs
What are Biogeochemical Cycles?
Microbial Bioremediation of Uranium

