Abstract

Eutrophication (the overenrichment of aquatic ecosystems with nutrients leading to algal blooms and anoxic events) is a persistent condition of surface waters and a widespread environmental problem. Some lakes have recovered after sources of nutrients were reduced. In others, recycling of phosphorus from sediments enriched by years of high nutrient inputs causes lakes to remain eutrophic even after external inputs of phosphorus are decreased. Slow flux of phosphorus from overfertilized soils may be even more important for maintaining eutrophication of lakes in agricultural regions. This type of eutrophication is not reversible unless there are substantial changes in soil management. Technologies for rapidly reducing phosphorus content of overenriched soils, or reducing erosion rates, are needed to improve water quality.

Keywords

EutrophicationEnvironmental sciencePhosphorusNutrientAquatic ecosystemEcosystemAnoxic watersSoil waterWater qualityEcologySoil scienceBiologyChemistry

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Publication Info

Year
2005
Type
article
Volume
102
Issue
29
Pages
10002-10005
Citations
822
Access
Closed

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Stephen R. Carpenter (2005). Eutrophication of aquatic ecosystems: Bistability and soil phosphorus. Proceedings of the National Academy of Sciences , 102 (29) , 10002-10005. https://doi.org/10.1073/pnas.0503959102

Identifiers

DOI
10.1073/pnas.0503959102