Impacts of low-disturbance dairy manure incorporation on ammonia and greenhouse gas fluxes in a corn silage-winter rye cover crop system.

Abstract

Manure and fertilizer applications contribute to greenhouse gas (GHG) and ammonia (NH3 ) emissions. Losses of NH3 and nitrous oxide (N2 O) are an economic loss of nitrogen (N) to farms, and methane (CH4 ), N2 O, and carbon dioxide (CO2 ) are important GHGs. Few studies have examined the effects of low-disturbance manure incorporation (LDMI) on both NH3 and GHG fluxes. Here, NH3 , N2 O, CH4 , and CO2 fluxes in corn (Zea mays L.)-winter rye (Secale cereale L.) field plots were measured under fall LDMI (aerator/band, coulter injection, strip-till, sweep inject, surface/broadcast application, broadcast-disk) and spring-applied urea (134kg N ha-1 ) treatments from 2013 to 2015 in central Wisconsin. Whereas broadcast lost 35.5% of applied ammonium-N (NH4 -N) as NH3 -N, strip-till inject and coulter inject lost 0.11 and 4.5% of applied NH4 -N as NH3 , respectively. Mean N2 O loss ranged from 2.7 to 3.6% of applied total N for LDMI, compared with 4.2% for urea and 2.6% for broadcast. Overall, greater CO2 fluxes for manure treatments contributed to larger cumulative GHG fluxes compared with fertilizer N. There were few significant treatment effects for CH4 (P>.10); however, fluxes were significantly correlated with changes in soil moisture and temperature. Results indicate that LDMI treatments significantly decreased NH3 loss but led to modest increases in N2 O and CO2 fluxes compared with broadcast and broadcast-disk manure incorporation. Tradeoffs between N conservation versus increased GHG fluxes for LDMI and other methods should be incorporated into nutrient management tools as part of assessing agri-environmental farm impacts.