70-8 Reducing Nitrous Oxide Emissions from US Row Crop Agriculture through N Fertilizer Management

See more from this Division: Joint Sessions
See more from this Session: U.S. Agriculture’s Role in Soil Carbon Sequestration and Greenhouse Gas Mitigation (GRACEnet)

Tuesday, 7 October 2008: 3:15 PM
George R. Brown Convention Center, General Assembly Theater Hall C

Neville Millar1, G. Philip Robertson1, Peter Grace2, Ronald Gehl3, K. Kahmark4, S. Bohm4 and John Patrick Hoben5, (1)Kellogg Biological Station, Michigan State University, Hickory Corners, MI
(2)Institute for Sustainable Resources, Queensland University of Technology, Brisbane, Australia
(3)Horticultural Crops Research and Extension Center, North Carolina State University, Fletcher, NC
(4)Kellogg Biological Station, Michigan State Univ., Hickory Corners, MI
(5)Department of Crop and Soil Sciences, Michigan State Univ., East Lansing, MI
Abstract:
Nitrous oxide (N2O) is a potent greenhouse gas (GHG) produced in soils primarily through the microbial processes of nitrification and denitrification. It is the predominant GHG emitted by US agricultural activities, with annual emissions from cropland greater than 1 Tg. Soil management activities such as nitrogen (N) fertilizer application are the largest contributor (78 %) to US N2O emissions.

Due to the high global warming potential of N2O, every ton of avoided N2O emissions is equivalent to approximately 300 tons of sequestered CO2. Increasing crop N-use efficiency by altering N management practices is likely the most promising strategy for mitigating agricultural N2O emissions across a range of cropland systems.

Annual inventories of N2O emissions from agricultural soil are typically calculated by assuming a constant linear relationship between total N inputs and subsequent N2O emissions. However, our previous research found evidence of a non-linear relationship, with N2O emissions sharply increasing above the N fertilizer rate at which crop yields were optimized. This implies that a substantial decrease in N2O flux from cropland could be achieved with moderate reductions in fertilizer N input and little yield impact.

To better refine this relationship we established automated flux chambers at the Kellogg Biological Station (KBS) in southwest Michigan to monitor near-continuous N2O emissions from a field scale, rain-fed N fertility gradient planted to corn. Fluxes of N2O were measured from 8 fertilizer-N rate applications (0, 34, 67, 101, 134, 168, 202 and 246 kg N ha-1) every 4 hours and related to soil N, moisture, temperature and crop yield.

Results from the 2008 field season will be presented, along with progress on, and the challenges associated with, implementing potential fertilizer N reduction strategies including the introduction of an agricultural N2O reduction protocol within a cap and trade system.

See more from this Division: Joint Sessions
See more from this Session: U.S. Agriculture’s Role in Soil Carbon Sequestration and Greenhouse Gas Mitigation (GRACEnet)