Impact of liming and maize residues on N2O and N2 fluxes in agricultural soils: an incubation study

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
Lisa Pfülb, Lars Elsgaard, Peter Dörsch, Roland Fuß, Reinhard Well
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引用次数: 0

Abstract

Since it is known that nitrous oxide (N2O) production and consumption pathways are affected by soil pH, optimising the pH of agricultural soils can be an important approach to reduce N2O emissions. Because liming effects on N2O reduction had not been studied under ambient atmosphere and typical bulk density of arable soils, we conducted mesoscale incubation experiments with soils from two liming trials to investigate the impact of long-term pH management and fresh liming on N transformations and N2O production. Soils differed in texture and covered a range of pH levels (3.8–6.7), consisting of non-limed controls, long-term field-limed calcite and dolomite treatments, and freshly limed soils. Both soils were amended with 15N-labelled potassium nitrate (KNO3) and incubated with and without incorporated maize litter. Packed soil mesocosms were cycled through four phases of alternating temperatures and soil moistures for at least 40 days. Emissions of N2O and dinitrogen (N2) as well as the product ratio of denitrification N2O/(N2O + N2), referred to as N2Oi were measured with the 15N gas flux method in N2-reduced atmosphere. Emissions of N2O increased in response to typical denitrifying conditions (high moisture and presence of litter). Increased temperature and soil moisture stimulated microbial activity and triggered denitrification as judged from 15NO3 pool derived N2O + N2 emissions. Fresh liming increased denitrification in the sandy soil up to 3-fold but reduced denitrification in the loamy soil by 80%. N2Oi decreased throughout the incubation in response to fresh liming from 0.5–0.8 to 0.3–0.4, while field-limed soils had smaller N2Oi (0.1–0.3) than unlimed controls (0.9) irrespective of incubation conditions. Our study shows that the denitrification response (i.e., N2O + N2 production) to liming is soil dependent, whereas liming effects on N2Oi are consistent for both long- and short-term pH management. This extends previous results from anoxic slurry incubation studies by showing that soil pH management by liming has a good mitigation potential for agricultural N2O emissions from denitrification under wet conditions outside of cropping season.

Abstract Image

石灰化和玉米残留物对农业土壤中 N2O 和 N2 通量的影响:一项培育研究
众所周知,一氧化二氮(N2O)的产生和消耗途径受土壤 pH 值的影响,因此优化农业土壤的 pH 值是减少 N2O 排放的重要方法。由于尚未研究过在环境气氛和耕地土壤典型容重条件下施用石灰对减少一氧化二氮的影响,因此我们用两次石灰试验的土壤进行了中尺度培养实验,以研究长期 pH 值管理和新鲜石灰对氮转化和一氧化二氮产生的影响。这些土壤的质地不同,pH 值范围也不同(3.8-6.7),包括非石灰化对照组、长期田间石灰化方解石和白云石处理组以及新石灰化土壤。这两种土壤都用 15N 标记的硝酸钾(KNO3)进行了改良,并与玉米秸秆一起或不与玉米秸秆一起培养。在温度和土壤湿度交替变化的四个阶段中,包装土壤介观模型的循环时间至少为 40 天。采用 15N 气体通量法测量了 N2O 和二氮(N2)的排放量,以及 N2O/(N2O + N2) 的反硝化产物比(简称 N2Oi)。在典型的反硝化条件下(高湿度和存在垃圾),N2O 的排放量增加。温度和土壤湿度的增加刺激了微生物的活动,从 15NO3- 池中衍生的 N2O + N2 排放量判断,这触发了反硝化作用。新施用的石灰可将沙质土壤的反硝化作用提高 3 倍,但将壤土的反硝化作用降低 80%。在整个培养过程中,N2Oi 随新鲜石灰化而从 0.5-0.8 降至 0.3-0.4,而无论培养条件如何,田间石灰化土壤的 N2Oi(0.1-0.3)均小于未石灰化对照(0.9)。我们的研究表明,土壤对石灰化的反硝化反应(即 N2O + N2 生成)与土壤有关,而石灰化对 N2Oi 的影响在长期和短期 pH 值管理中都是一致的。这扩展了之前缺氧泥浆培养研究的结果,表明通过施用石灰进行土壤 pH 值管理具有很好的缓解潜力,可在非耕种季节的潮湿条件下减少农业反硝化产生的 N2O 排放。
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来源期刊
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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