The effects of clipping frequency and nitrogen fertilisation on greenhouse gas emissions and net ecosystem exchange in an Australian temperate grassland
Field | Value | Language |
dc.contributor.author | Padashbarmchi, Zahra | |
dc.contributor.author | Minasny, Budiman | |
dc.contributor.author | Shirvan, Milad Bagheri | |
dc.contributor.author | González, Luciano A. | |
dc.contributor.author | Dijkstra, Feike A. | |
dc.date.accessioned | 2025-01-31T03:04:44Z | |
dc.date.available | 2025-01-31T03:04:44Z | |
dc.date.issued | 2025 | en_AU |
dc.identifier.uri | https://hdl.handle.net/2123/33576 | |
dc.description.abstract | Grassland ecosystems store significant amounts of organic carbon (C) and have the potential to function as a source or sink of greenhouse gases (GHGs) under different environmental conditions and management practices. However, the effects of management (clipping frequency and N fertilisation) on the GHGs remain uncertain. In this study, a field-based experiment with automated-lid gas exchange chambers was conducted to simultaneously measure different GHG fluxes (CO 2 , N 2 O, CH 4 ), their overall global warming potential (GWP-100) impact, and net ecosystem exchange (NEE) from a grassland. The experiment had two clipping frequencies (simulating moderate and high grazing intensity) and two nitrogen (N) fertiliser treatments (0 and 40 kg N ha −1 year −1 ). The measurements were conducted during two periods (each approximately 2 weeks long) of varied temperature and moisture in early autumn. High clipping frequency caused higher daily NEE emissions, higher GWP-100 impact and lower photosynthesis; however, it did not significantly affect these parameters. Nitrogen fertilisation effects were lower than the clipping frequency treatment, but the impact on N on the time of N application. Methane (CH 4 ) 2 O fluxes was likely to be dependent was predominantly controlled by soil moisture, whereas nitrous oxide (N 2 O) was more strongly affected by temperature. N O emissions increased significantly after the break-point temperature of 20°C. Our results have highlighted the sensitivity of CH 4 2 uptake and N 2 2 O emissions to environmental conditions, particularly their increase under warmer temperatures. The main contributor of GWP-100 impact in this study was CO emissions and uptake. For the observation period, the grassland was a small C sink. For a comprehensive understanding, longer-term studies spanning over several years are needed to accurately assess the impact of different management practices on GHG emissions. | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | CSIRO Publishing | en_AU |
dc.relation.ispartof | The Rangeland Journal | en_AU |
dc.rights | Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 | en_AU |
dc.subject | global warming potential (GWP-100) | en_AU |
dc.subject | grassland ecosystem | en_AU |
dc.subject | greenhouse gases (GHGs) | en_AU |
dc.subject | soil moisture | en_AU |
dc.subject | soil temperature | en_AU |
dc.subject | clipping frequency | en_AU |
dc.subject | nitrogen fertilisation | en_AU |
dc.subject | net ecosystem exchange (NEE) | en_AU |
dc.title | The effects of clipping frequency and nitrogen fertilisation on greenhouse gas emissions and net ecosystem exchange in an Australian temperate grassland | en_AU |
dc.type | Article | en_AU |
dc.identifier.doi | 10.1071/RJ23026 | |
dc.type.pubtype | Publisher's version | en_AU |
usyd.faculty | SeS faculties schools::Faculty of Science::School of Life and Environmental Sciences | en_AU |
usyd.faculty | SeS faculties schools::Faculty of Science::Sydney Institute of Agriculture (SIA) | en_AU |
usyd.citation.volume | 47 | en_AU |
workflow.metadata.only | No | en_AU |
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