Abstract
Cover crop management during the fallow season may play a relevant role in improving crop productivity and soil quality, by increasing nitrogen (N) and soil organic carbon (SOC) accumulation, but has the possibility of increasing greenhouse gas (GHG) emissions from the soil. A year-long consistency experiment was conducted to examine the effects of various winter covering crops on annual nitrous oxide (N2O) together with methane (CH4) emissions in the mono-rice planting system, including direct emissions in the cover crop period and the effects of incorporating these crops on gaseous emissions during the forthcoming rice (Oryza Sativa L.) growing period, to improve the development of winter fallow paddy field with covering crops and to assess rice cultivation patterns. The experiment included three treatments: Chinese milk vetch-rice (Astragalus sinicus L.) with cover crop residue returned (T1), ryegrass (Lolium multiflorum L.)-rice with cover crop residue returned (T2), and rice with winter fallow (CK). Compared with CK, the two winter cover crop treatments significantly increased rice yield, soil organic carbon (SOC) and total nitrogen (TN) by 6.9–14.5%, 0.8–2.1% and 3.4–5.4%, respectively. In all cases, the fluxes of CH4 and N2O could increase with the incorporation of N fertilizer application and cover crop residues. Short-term peaks of these two gas fluxes were monitored after all crop residues were incorporated in the soil preparation period, the early vegetative growth period and the midseason drainage period. The winter cover crop residue application greatly enhanced CH4 and N2O cumulative emissions compared with CK (by 193.6–226.5% and 37.5–43.7%, respectively) during rice growing season and intercropping period. Meanwhile, the mean values of global warming potentials (GWPs) from paddy fields with different cropping crops were T2 > T1 > CK. Considering the advantages of crop productivity together with environmental safety and soil quality, Chinese milk vetch-rice with cover crop residue returned would be the most practicable and sustainable cultivation pattern for the mono-rice cropping systems.
Highlights
Introduction published maps and institutional affilIt is assumed that agricultural soils are a major source of greenhouse gas (GHG)leading to Earth’s climate change, nitrous oxide (N2 O) and methane (CH4 )—the most important long-lived GHGs [1]
Our results indicated that the paddy soil with cover crop residues was the main source of atmospheric CH4
Compared with CK, the CH4 emissions of T1 and T2 increased in the rice growing period and cover crop period
Summary
Introduction published maps and institutional affilIt is assumed that agricultural soils are a major source of greenhouse gas (GHG)leading to Earth’s climate change, nitrous oxide (N2 O) and methane (CH4 )—the most important long-lived GHGs [1]. The global warming potentials (GWPs) of N2 O and CH4 are 298 and 25 times higher than that of carbon dioxide (CO2 ). Both gases are reactive chemicals, CH4 influences the atmospheric chemistry and oxidation capacity, and the increased N2 O in the atmosphere affects ozone depletion in the stratosphere [2]. CH4 and N2 O emissions mostly rely on crop/soil management practices, such as fertilization, irrigation, soil cultivation and organic farming. These changes in agricultural practices would provide mitigation options [5]. CH4 is produced by the decomposition of organic materials in iations
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