Empirical Critical Loads of Atmospheric Nitrogen Deposition for Nutrient Enrichment and Acidification of Sensitive US Lakes
Author(s) -
Jill S. Baron,
Charles T. Driscoll,
John L. Stoddard,
Eric E. Richer
Publication year - 2011
Publication title -
bioscience
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.761
H-Index - 209
eISSN - 1525-3244
pISSN - 0006-3568
DOI - 10.1525/bio.2011.61.8.6
Subject(s) - nutrient , environmental science , deposition (geology) , snowmelt , watershed , nitrogen , vegetation (pathology) , hydrology (agriculture) , soil acidification , environmental chemistry , ecology , soil water , chemistry , surface runoff , soil ph , sediment , biology , geology , soil science , medicine , paleontology , geotechnical engineering , organic chemistry , pathology , machine learning , computer science
The ecological effects of elevated atmospheric nitrogen (N) deposition on high-elevation lakes of the western and northeastern United States include nutrient enrichment and acidification. The nutrient enrichment critical load for western lakes ranged from 1.0 to 3.0 kilograms (kg) of N per hectare (ha) per year, reflecting the nearly nonexistent watershed vegetation in complex, snowmelt-dominated terrain. The nutrient enrichment critical load for northeastern lakes ranged from 3.5 to 6.0 kg N per ha per year. The N acidification critical loads associated with episodic N pulses in waters with low values of acid neutralizing capacity were 4.0 kg N per ha per year (western) and 8.0 kg N per ha per year (northeastern). The empirical critical loads for N-caused acidification were difficult to determine because of a lack of observations in the West, and high sulfur deposition in the East. For both nutrient enrichment and acidification, the N critical load was a function of how atmospheric N deposition was determined.
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