Testing a Conceptual Model of Soil Emissions of Nitrous and Nitric Oxides

By Eric Davidson, M. Keller, H. Erickson, Louis Verchot, E. Veldkamp. 2000

930 citations recorded by the source corpus.

Subfields: Agronomy and Crop Science, Plant Science, Soil Science

View Paper: https://www.semanticscholar.org/paper/34bddaa1358102f4e713e2bda9d4afea1c361a12

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Agronomy and Crop Science

1. Lydia P. Olander

In Plant Science

1. S. Medinets
2. K. Butterbach‐Bahl
3. R. B. Jackson
4. Gregory P. Asner
5. Roberta E. Martin
6. H. Rennenberg
7. Lydia P. Olander
8. J. Canadell

In Soil Science

1. R. B. Jackson
2. H. Rennenberg
3. D. Cusack
4. Lydia P. Olander
5. Noah Fierer
6. Rob Knight
7. C. Lauber

Citations in the corpus

• GRAZING SYSTEMS, ECOSYSTEM RESPONSES, AND GLOBAL CHANGE (2004, background): “(129) found for a variety of tropical sites in Costa Rica, Puerto Rico, and Brazil that old tropical pastures produce consistently lower NO fluxes than old-growth tropical forests.”
• The Nitrogen Cascade (2003, background): “Effluxes of NO and N2O also may increase because of nitrification or denitrification processes (Davidson et al. 2000), which may become significant if soils are imperfectly or variably drained soils.”
• Emissions of CO2, CH4 and N2O from Southern European peatlands (2010, background): “…be substantial (up to 80% of total N2O emissions) (Webster and Hopkins, 1996; Pihlatie et al., 2004), and another product of nitrification is nitrate, which is the rate controlling factor for anaerobic N2O production via denitrification (Conrad, 1996; Davidson et al., 2000; Öquist et al., 2007).”
• A review of soil NO transformation: associated processes and possible physiological significance on organisms (2015, background): “414 Optimum conditions for nitrification are normally met at a water filled 415 pore space (WFPS) of 30-60% (Firestone and Davidson, 1989; Bouwman., 416 1998; Davidson et al., 2000).”
• Global change effects on humid tropical forests: Evidence for biogeochemical and biodiversity shifts at an ecosystem scale (2016, background): “In particular, the high levels of soil moisture, soil N availability, soil microbial activity, and fluctuating soil redox common inmany tropical forests make them dominant contributors to N2O fluxes on a global scale [Breuer et al., 2000; Crill et al., 2000; Davidson et al., 2000].”
• The Global N2O Model Intercomparison Project (2018, background): “In general, N2O emissions from soil are regulated at two levels, which are the rates of nitrification and denitrification in the soil and soil physical factors regulating the ratio of N2O to other nitrous gases (Davidson et al. 2000).”