Institute of Environment Pollution Control and Treatment, College of Environment and Resource Science, Zhejiang University, Hangzhou 310029, PR China.
Institute of Environment Pollution Control and Treatment, College of Environment and Resource Science, Zhejiang University, Hangzhou 310029, PR China.
Sci Total Environ. 2021 Nov 20;796:149050. doi: 10.1016/j.scitotenv.2021.149050. Epub 2021 Jul 15.
Fresh biochar application has been recommended as an effective strategy to mitigate methane emissions from paddy soil due to its role in promoting potential methane oxidation (PMO). However, little is known about the effect of biochar on PMO after long-term aging. Here, a laboratory incubation experiment was performed to gain insight into the combined effects of biochar characteristics on soil PMO during the biochar aging process. Biochar samples aged with an HNO/HSO mixture (1:3) were prepared and added at 22.5 and 2.8 t ha to paddy soil. Mixed acid with a dilution of 10- 40% indicated the aging process in paddy field properly. Smaller biochar particles, smoother surface, higher surface area and porosity were observed with the increase of mixed acid ratio. Carboxylic functional groups (COOR) on biochar surface increased accompanied with biochar aging process. Aged biochar application at 22.5 t ha inhibited paddy soil PMO, which mainly caused from the increased COOR groups induced NH-N inhibition for PMO. Increased soil NH-N inhibited PMO by limiting the growth of methanotrophs and nitrifiers due to decreased soil pH. In contrast, 2.8 t aged biochar ha application showed no significant difference on PMO compared with control. Our results indicated that aged biochar exerted in paddy soil have limited effect on mitigating methane emissions from paddy soil in the long term.
新鲜生物炭的应用因其促进潜在甲烷氧化(PMO)的作用而被推荐为减少稻田甲烷排放的有效策略。然而,对于生物炭在长期老化后对 PMO 的影响知之甚少。在这里,进行了一项实验室孵育实验,以深入了解生物炭老化过程中生物炭特性对土壤 PMO 的综合影响。用 HNO3/H2SO4 混合物(1:3)制备并添加到稻田中的老化生物炭样品,其添加量为 22.5 和 2.8 t ha-1。用 10-40%稀释的混合酸可以正确模拟田间老化过程。随着混合酸比例的增加,观察到生物炭颗粒更小、表面更光滑、表面积和孔隙率更高。生物炭表面的羧酸官能团(COOR)随着生物炭老化过程而增加。在 22.5 t ha-1 的条件下,添加老化生物炭会抑制稻田 PMO,这主要是由于 COOR 基团的增加导致 NH4+-N 对 PMO 的抑制作用。由于土壤 pH 值降低,增加的土壤 NH4+-N 通过限制甲烷营养菌和硝化菌的生长来抑制 PMO。相比之下,与对照相比,添加 2.8 t ha-1 的老化生物炭对 PMO 没有显著差异。我们的结果表明,长期来看,在稻田中添加老化生物炭对减少稻田甲烷排放的影响有限。