Lazcano Cristina, Zhu-Barker Xia, Decock Charlotte
Department of Land, Air and Water Resources, University of California Davis, Davis, CA 95616, USA.
Natural Resources Management and Environmental Sciences Department, California Polytechnic State University, San Luis Obispo, CA 93407, USA.
Microorganisms. 2021 May 1;9(5):983. doi: 10.3390/microorganisms9050983.
The use of organic fertilizers constitutes a sustainable strategy to recycle nutrients, increase soil carbon (C) stocks and mitigate climate change. Yet, this depends largely on balance between soil C sequestration and the emissions of the potent greenhouse gas nitrous oxide (NO). Organic fertilizers strongly influence the microbial processes leading to the release of NO. The magnitude and pattern of NO emissions are different from the emissions observed from inorganic fertilizers and difficult to predict, which hinders developing best management practices specific to organic fertilizers. Currently, we lack a comprehensive evaluation of the effects of OFs on the function and structure of the N cycling microbial communities. Focusing on animal manures, here we provide an overview of the effects of these organic fertilizers on the community structure and function of nitrifying and denitrifying microorganisms in upland soils. Unprocessed manure with high moisture, high available nitrogen (N) and C content can shift the structure of the microbial community, increasing the abundance and activity of nitrifying and denitrifying microorganisms. Processed manure, such as digestate, compost, vermicompost and biochar, can also stimulate nitrifying and denitrifying microorganisms, although the effects on the soil microbial community structure are different, and NO emissions are comparatively lower than raw manure. We propose a framework of best management practices to minimize the negative environmental impacts of organic fertilizers and maximize their benefits in improving soil health and sustaining food production systems. Long-term application of composted manure and the buildup of soil C stocks may contribute to N retention as microbial or stabilized organic N in the soil while increasing the abundance of denitrifying microorganisms and thus reduce the emissions of NO by favoring the completion of denitrification to produce dinitrogen gas. Future research using multi-omics approaches can be used to establish key biochemical pathways and microbial taxa responsible for NO production under organic fertilization.
使用有机肥料是一种回收养分、增加土壤碳储量和缓解气候变化的可持续策略。然而,这在很大程度上取决于土壤碳固存与强效温室气体一氧化二氮(N₂O)排放之间的平衡。有机肥料强烈影响导致N₂O释放的微生物过程。N₂O排放的幅度和模式与无机肥料的排放不同且难以预测,这阻碍了制定针对有机肥料的最佳管理措施。目前,我们缺乏对有机肥料对氮循环微生物群落功能和结构影响的全面评估。本文聚焦于动物粪便,概述了这些有机肥料对旱地土壤中硝化和反硝化微生物群落结构和功能的影响。高水分、高有效氮(N)和碳含量的未处理粪便会改变微生物群落结构,增加硝化和反硝化微生物的丰度和活性。经过处理的粪便,如沼渣、堆肥、蚯蚓堆肥和生物炭,也能刺激硝化和反硝化微生物,尽管对土壤微生物群落结构的影响不同,且N₂O排放相对低于生粪。我们提出了一个最佳管理措施框架,以尽量减少有机肥料对环境的负面影响,并最大限度地发挥其在改善土壤健康和维持粮食生产系统方面的益处。长期施用堆肥和积累土壤碳储量可能有助于将氮保留为土壤中的微生物氮或稳定有机氮,同时增加反硝化微生物的丰度,从而通过促进反硝化作用完成以产生氮气来减少N₂O排放。未来使用多组学方法的研究可用于确定在有机施肥条件下负责N₂O产生的关键生化途径和微生物分类群。