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James N. Galloway

Researcher at University of Virginia

Publications -  311
Citations -  57524

James N. Galloway is an academic researcher from University of Virginia. The author has contributed to research in topics: Reactive nitrogen & Deposition (aerosol physics). The author has an hindex of 92, co-authored 293 publications receiving 50832 citations. Previous affiliations of James N. Galloway include Cornell University & Marine Biological Laboratory.

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The Western Atlantic Ocean Experiment

TL;DR: The WATOX program as mentioned in this paper uses diverses methodes d'echantillonnage, de tracage par aerosols and de precipitation for determiner les cycles atmospheriques chimiques of l'Ouest de l'Ocean Atlantique.
Book ChapterDOI

The Intercontinental Transport of Sulfur and Nitrogen

TL;DR: In this paper, the impact of anthropogenic activities on the atmosphere is evident on several spatial scales and it is realized that the contributing materials are not entirely deposited in the region in which they are emitted, thus, hemispheric and global scales of atmospheric contamination are now realities.

Nitrogen efficiency in agriculture in Europe and India.

TL;DR: Notably, the balance sheets for crop production and the agricultural sector as a whole showed a surplus of about 60 kg of nitrogen per hectare of agricultural land, while the EU15 and India were chosen for this study on nitrogen efficiency using balance sheets.

Assessments of impacts of nitrogen deposition on beech forests: results from the Pan-European Intensive Monitoring Programme.

TL;DR: In this article, the effects of nitrogen deposition on beech forest ecosystems in Europe were reviewed on the basis of beech plots of the Pan-European Monitoring Programme of ICP Forests and the EU, the deposition of N compounds as well as input-output budgets are listed and compared with studies in North America.
Book ChapterDOI

The Deposition of Sulfur and Nitrogen from the Remote Atmosphere Working-Group Report

TL;DR: In this paper, the authors classified the materials present in the atmosphere can be deposited by a wide range of physical mechanisms including sedimentation, impaction, interception, and diffusion of particles and the diffusion of gases.