Lussich Facundo, Dhaliwal Jashanjeet Kaur, Faiia Anthony M, Jagadamma Sindhu, Schaeffer Sean M, Saha Debasish
Department of Biosystems Engineering and Soil Science, University of Tennessee, Knoxville, TN, 37996, USA.
Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN, 37996, USA.
Sci Rep. 2024 Apr 10;14(1):8437. doi: 10.1038/s41598-024-58942-7.
Cover cropping is a promising strategy to improve soil health, but it may also trigger greenhouse gas emissions, especially nitrous oxide (NO). Beyond nitrogen (N) availability, cover crop residue decomposition may accelerate heterotrophic respiration to limit soil O availability, hence promote NO emissions from denitrification under sub-optimal water-filled pore space (WFPS) conditions that are typically not conducive to large NO production. We conducted a 21-day incubation experiment to examine the effects of contrasting cover crop residue (grass vs legume) decomposition on soil O and biogeochemical changes to influence NO and CO emissions from N labeled fertilized soils under 50% and 80% WFPS levels. Irrespective of cover crop type, mixing cover crop residue with N fertilizer resulted in high cumulative NO emissions under both WFPS conditions. In the absence of cover crop residues, the N fertilizer effect of NO was only realized under 80% WFPS, whereas it was comparable to the control under 50% WFPS. The NO peaks under 50% WFPS coincided with soil O depletion and concomitant high CO emissions when cover crop residues were mixed with N fertilizer. While N fertilizer largely contributed to the total NO emissions from the cover crop treatments, soil organic matter and/or cover crop residue derived NO had a greater contribution under 50% than 80% WFPS. Our results underscore the importance of NO emissions from cover crop-based fertilized systems under relatively lower WFPS via a mechanism of respiration-induced anoxia and highlight potential risks of underestimating NO emissions under sole reliance on WFPS.
覆盖作物种植是改善土壤健康的一种有前景的策略,但它也可能引发温室气体排放,尤其是一氧化二氮(N₂O)。除了氮(N)的有效性外,覆盖作物残茬分解可能会加速异养呼吸,从而限制土壤中的氧气(O₂)供应,进而在通常不利于大量产生N₂O的次优充水孔隙空间(WFPS)条件下促进反硝化作用产生N₂O排放。我们进行了一项为期21天的培养实验,以研究不同的覆盖作物残茬(草类与豆类)分解对土壤O₂以及生物地球化学变化的影响,从而影响在50%和80% WFPS水平下施有N标记肥料的土壤中N₂O和CO₂的排放。无论覆盖作物类型如何,在两种WFPS条件下,将覆盖作物残茬与氮肥混合都会导致较高的累积N₂O排放。在没有覆盖作物残茬的情况下,氮肥对N₂O的影响仅在80% WFPS下才会显现,而在50% WFPS下与对照相当。当覆盖作物残茬与氮肥混合时,50% WFPS下的N₂O排放峰值与土壤O₂耗尽以及随之而来的高CO₂排放同时出现。虽然氮肥在覆盖作物处理产生的总N₂O排放中占很大比例,但在50% WFPS下,土壤有机质和/或覆盖作物残茬产生的N₂O贡献比在80% WFPS下更大。我们的研究结果强调了在相对较低的WFPS条件下,基于覆盖作物的施肥系统通过呼吸诱导缺氧机制排放N₂O的重要性,并突出了仅依赖WFPS时低估N₂O排放的潜在风险。