Abstract

Information on the influence of tillage on nitrous oxide (N 2O) emissions is needed by researchers, policy makers and farmers for assessment of global ramifications of warming potential of greenhouse gas N 2O. This research evaluates the effects of continuous long-term tillage and seasonal changes in N 2O emissions in New Zealand temperate climate. The experiment was conducted in a Kairanga silty clay loam (Eutric Gleysol) where maize ( Zea mays L.) was grown continuously for either 17 (K17) or 34 (K34) years, with conventional tillage. An adjacent permanent ryegrass ( Lolium perenne L.) and clover ( Trifolium sp.) pasture (PP) was used as a control. Mean N 2O emissions under K17 and K34 and PP ranged from 0.04 to 1.35, 0.03 to 1.13, and 0.03 to 0.99 g N 2O-N/ha/h, respectively. Average annual N 2O emissions from K34 were slightly lower than those in the K17 fields although there were no differences in N 2O emissions between PP and K17. Depleted organic C, total N and microbial biomass C in K34 as compared with K17, possibly limited denitrification process and decreased N 2O emissions. Soil water content (SWC) was a key factor controlling N 2O emissions in both pasture and cropped soils. Low emissions occurred when gravimetric SWC content was less than 30%. N 2O emissions from grazed pasture were low during summer (dry) period and increased during winter (wet) season. There were no differences in N 2O between the K17 and K34 during dry season but N 2O emission rates in wet season were lower in the K34. Despite high temporal variability observed in the N 2O emissions, our estimates based on low frequency of measurements over 1 year were in general agreement with those in the literature.

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