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(2005) Eutrophication of ecosystems: bistability and soil phosphorus.

Authors
Carpenter S.
Source
Proceedings of the National Academy of Sciences of the United States of America (PNAS) (128)
Type
P - Paper (2851)
Peer Review
1 - High (2301)
Audience
S - Specialist (3514)
Pages
10002-10005
Journal Number
102
Notes

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.

World_link Resources online

Folder Categories
Marine and Freshwater Dynamics pH: Acidification Productivity Lakes
 
Tag_blue Keywords
lake alternate states recycling regime shift
 
 
 

Entered by: Sonia Khela, 4/2010

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