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The global nitrogen cycle: changes and consequences

Citation

James N Galloway, The global nitrogen cycle: changes and consequences: .

Summary

In the absence of human activities, biological N fixation is the primary source of reactive N, providing about 90–130 Tg N year−1 (Tg = 1012 g) on the continents. Human activities have resulted in the fixation of an additional 150 Tg N year−1 by energy production, fertilizer production, and cultivation of crops (e.g., legumes, rice). Some sinks of anthropogenic N have been estimated (e.g., N2O accumulation in the atmosphere; loss to coastal oceans), however due to the uncertainty around the magnitude of other sinks (e.g., retention in groundwater, soils, or vegetation or denitrification to N2) a possibly large portion of the N fixed by humans is missing. While we know that N is accumulating in the environment, we do not know [...]

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James N Galloway

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  • Upper Colorado River Basin

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From Source - Mendeley RIS export <br> On - Mon Feb 14 17:30:54 CST 2011

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Title Citation The global nitrogen cycle: changes and consequences

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