GSA Annual Meeting in Denver, Colorado, USA - 2016

Paper No. 321-13
Presentation Time: 9:00 AM-6:30 PM


MEHR, Nicole K.1, ADAIR, Carol2, BARBIERI, Lindsay2 and GOESCHEL, Tyler2, (1)Rubenstein School of Environment and Natural Resources, University of Vermont, 81 Carrigan Drive, Burlington, VT 05405; Department of Geology and Environmental Sciences, Hartwick College, 1 Hartwick Drive, Oneonta, NY 13820, (2)Rubenstein School of Environment and Natural Resources, University of Vermont, 81 Carrigan Drive, Burlington, VT 05405,

Agricultural practices directly augment the emissions of greenhouse gases (GHGs) to our atmosphere and alter nutrient cycling in fields. Fertilizers (manure) applied to agricultural fields can increase GHG flux rates and the amount of nitrogen (N) and phosphorus (P) in soils. Fertilization can lead to leaching, volatilization, denitrification and water runoff of nutrients. Excess N and P can cause eutrophication in water bodies, which is a major issue in the Lake Champlain watershed in Vermont. While P has been widely studied throughout the Lake Champlain Basin, less is known about N. Yet, understanding N cycling is important for controlling and managing eutrophication. Best Management practices (BMPs), such as the incorporation of manure via aeration tillage, have been adopted in an attempt to minimize nutrient runoff, but little is known about the effects of such BMPs on GHG emissions. This study focused on comparing soil NO3- and NH4+concentrations, and GHG fluxes of carbon dioxide (CO2) and nitrous oxide (N2O). While CO2 emissions are the result of plant and microbial respiration, N2O emissions result primarily from dentrification, a process that relies on low oxygen soils and high nitrate availability. Two pasture fields, adjacent to Lake Champlain, were selected for this four-year study in Shelburne, Vermont. Field 2 is a conventional field where manure is spread directly across the field (broadcast). Field 1 is a BMP where soil is aerated before manure is spread. After the second year of sampling, these practices yielded a difference in NO3- and NH4+ concentrations and GHG emissions. Using static flux chambers and an Infrared Photoacoustic Spectroscopy gas analyzer, CO2 and N2O fluxes were measured on site. Soil temperature, air temperature, and soil moisture were recorded and soil cores were taken at times of gas sampling and analyzed in the lab for NO3- and NH4+. The BMP decreased N2O fluxes (P < 0.1) but had no impact on CO2 fluxes relative to broadcast manure application alone. However, the broadcast field had 2x the amount of NH4+ after manure was spread, compared to the BMP field. Differences in NO3- followed a similar trend. Our results suggest that aeration tillage may be used as a management technique to reduce post-manure N2O fluxes, likely by increasing oxygen availability and reducing rates of N2O production.