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Arvin R. Mosier

Researcher at University of Melbourne

Publications -  202
Citations -  26030

Arvin R. Mosier is an academic researcher from University of Melbourne. The author has contributed to research in topics: Soil water & Denitrification. The author has an hindex of 86, co-authored 200 publications receiving 24540 citations. Previous affiliations of Arvin R. Mosier include United States Department of Agriculture & Colorado State University.

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Global estimates of potential mitigation of greenhouse gas emissions by agriculture

TL;DR: In this paper, the potential reduction of radiative forcing by the agricultural sector ranges from 115-33 Gt C equivalents per year of the total potential reduction, approximately 32% could result from reduction in CO2 emissions, 42% of carbon offsets by biofuel production on 15% of existing croplands, 16% from reduced CH4 emissions and 10% from reducing emissions of N2O Agriculture.
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CO2, CH4 and N2O flux through a Wyoming snowpack and implications for global budgets

TL;DR: In this article, the authors present evidence that the soils under alpine and sub-alpine snowpacks emit CO2 and N2O and take up atmospheric CH4 throughout the snow-covered period.
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Generalized model for NOx and N2O emissions from soils

TL;DR: In this paper, the authors describe a submodel to simulate NOx and N2O emissions from soils and present comparisons of simulated NOx fluxes from the DAYCENT ecosystem model with observations from different soils.
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Ammonia volatilization from synthetic fertilizers and its mitigation strategies: A global synthesis

TL;DR: In this paper, a meta-analysis of 824 observations on impacts on NH3 volatilization of ⿿4R Nutrient Stewardship (right source, rate, place and time), farming practices (irrigation, residue retention, amendments), and enhanced efficiency fertilizers (fertilizers with urease inhibitors, nitrification inhibitors or controlled release coatings) was conducted.
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Crop Residue Type and Placement Effects on Denitrification and Mineralization

TL;DR: In this article, residue type, placement, and degree of incorporation, and soil water regimes largely control availability and loss of soil N and were evaluated in the laboratory and showed significant denitrification was greatest during the first 8-10 d, as was CO evolution.