79-6 Does Increasing Soil Carbon Increase Soil Nitrous Oxide Emissions from a Cropping Soil in a Semiarid Region?.

See more from this Division: ASA Section: Environmental Quality
See more from this Session: Management Practices and Land-Use Impact on Global Warming Potential and Greenhouse Gas Intensity

Monday, November 16, 2015: 2:15 PM
Minneapolis Convention Center, 102 E

Louise Barton, School of Earth and Environment (M087), University of Western Australia, Crawley, WA, AUSTRALIA, Frances Hoyle, Department of Agriculture and Food Western Australia, Bentley, Australia and Daniel Murphy, School of Earth and Environment (M087), The University of Western Australia, Crawley, Australia
Abstract:
Increasing soil organic carbon (SOC) is promoted as a strategy for sequestering carbon dioxide (CO2) and mitigating anthropogenic greenhouse gas (GHG) emissions. Although increasing SOC can benefit crop productivity, it has enhanced nitrous oxide (N2O) emissions in temperate environments. Our field-based study investigated the extent to which increasing SOC altered N2O and methane (CH4) emissions from a rainfed, cropped soil in a semiarid region. The experimental design included two organic matter (OM) additions (no OM, plus OM) by two N fertiliser rates (0, 100 kg ha-1 yr-1) by three replicate plots. Organic matter (chaff) had been applied to a free-draining sandy soil every three years (80 t ha-1 applied to date) since 2003, and tillage had occurred annually. Soil organic carbon (0–100 mm) averaged 1.20 % in the plus OM treatment versus 0.64% in the no OM treatment during the present study. Nitrous oxide and CH4 fluxes were measured for two years on a sub-daily basis using soil chambers connected to a fully automated system that analysed trace gases by gas chromatography. Increasing SOC increased soil N2O emissions (and inhibited CH4 uptake), but also improved grain yield and quality. Nitrous oxide emissions were low by international standards and represented up to 0.1% of the N fertiliser applied. Total N2O emissions after two years were ranked: plus OM, plus N (409 g N2O-N ha-1) > plus OM, no N (202 g N2O-N ha-1) > no OM, plus N (41 g N2O-N ha-1) = no OM, no N (14 g N2O-N ha-1). Increasing SOC has also decreased CH4 uptake by 30%. Land management practises that increase SOC in sandy-textured rainfed, cropping soils in semiarid regions should be encouraged as it can improve grain yield without substantial increases in soil N2O emissions.

See more from this Division: ASA Section: Environmental Quality
See more from this Session: Management Practices and Land-Use Impact on Global Warming Potential and Greenhouse Gas Intensity