J
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 biogeochemical cycling of formic and acetic acids through the troposphere: an overview of current understanding
TL;DR: In this article, a general picture of the biogeochemical cycling of HCOOH and CH 3 COOH is beginning to emerge, and the similarity of concentrations in remote and impacted regions indicates that anthropogenic emissions of carboxylic acids or precursors are probably not important sources over broad geographic areas.
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An atmospheric sulfur budget for eastern North America
TL;DR: In this paper, atmospheric sulfur budgets for the eastern United States, eastern Canada and eastern North America are formulated, based on the fluxes: natural and man-made emissions, wet and dry deposition and atmospheric inflows and outflows.
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Modeling soil organic carbon change in croplands of china
Changsheng Li,Yahui Zhuang,Steve Frolking,James N. Galloway,Robert C. Harriss,Berrien Moore,David S. Schimel,David S. Schimel,Xiaoke Wang +8 more
TL;DR: In this paper, the authors modeled carbon and nitrogen biogeochemical cycles in croplands of China (and, for comparison, the United States) to estimate the annual soil organic carbon (SOC) balance for all cropland.
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Time scales of catchment acidification. A quantitative model for estimating freshwater acidification
TL;DR: This paper discussed the quantitative model used to estimate patterns and absolute time scales of surface water acidification, called MAGIC (model of acidification of groundwater in catchments), based on mathematical representations of those processes thought the preliminary catchment controls on acidification.
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Effects of global change during the 21st century on the nitrogen cycle
David Fowler,Claudia Steadman,David Stevenson,Mhairi Coyle,Robert M. Rees,Ute Skiba,Mark A. Sutton,John N. Cape,Anthony J. Dore,Massimo Vieno,David Simpson,David Simpson,Sönke Zaehle,Benjamin D. Stocker,Matteo Rinaldi,Maria Cristina Facchini,Christophe Flechard,Eiko Nemitz,Marsailidh Twigg,J.W. Erisman,Klaus Butterbach-Bahl,James N. Galloway +21 more
TL;DR: The global nitrogen cycle at the beginning of the 21st century has been shown to be strongly influenced by the inputs of reactive nitrogen (Nr) from human activities, including combustion-related NOx, industrial and agricultural N fixation, estimated to be 220 Tg N yr−1 in 2010, which is approximately equal to the sum of biological N fixation in unmanaged terrestrial and marine ecosystems.