Nitrous oxide emissions in soils cropped with maize under long-term tillage and under permanent pasture in New Zealand

Citation
Ma. Choudhary et al., Nitrous oxide emissions in soils cropped with maize under long-term tillage and under permanent pasture in New Zealand, SOIL TILL R, 62(1-2), 2001, pp. 61-71
Citations number
24
Categorie Soggetti
Agriculture/Agronomy
Journal title
SOIL & TILLAGE RESEARCH
ISSN journal
01671987 → ACNP
Volume
62
Issue
1-2
Year of publication
2001
Pages
61 - 71
Database
ISI
SICI code
0167-1987(200110)62:1-2<61:NOEISC>2.0.ZU;2-0
Abstract
Information on the influence of tillage on nitrous oxide (N2O) emissions is needed by researchers, policy makers and farmers for assessment of global ramifications of warming potential of greenhouse gas NO. This research eval uates 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 conventi onal tillage. An adjacent permanent ryegrass (Lolium perenne L.) and clover (Trifolium sp.) pasture (PP) was used as a control. Mean N2O emissions und er K17 and K34 and PP ranged from 0.04 to 1.35, 0.03 to 1.13, and 0.03 to 0 .99 g N2O-N/ha/h, respectively. Average annual N2O emissions from K34 were slightly lower than those in the K17 fields although there were no differen ces in N2O emissions between PP and K17. Depleted organic C, total N and mi crobial biomass C in K34 as compared with K17, possibly limited denitrifica tion process and decreased N2O emissions. Soil water content (SWC) was a ke y factor controlling N2O emissions in both pasture and cropped soils. Low e missions occurred when gravimetric SWC content was less than 30%. N2O emiss ions from grazed pasture were low during summer (dry) period and increased during winter (wet) season. There were no differences in N2O between the K1 7 and K34 during dry season but N2O emission rates in wet season were lower in the K34. Despite high temporal variability observed in the N2O emission s, our estimates based on low frequency of measurements over I year were in general agreement with those in the literature. (C) 2001 Elsevier Science B.V. All rights reserved.