Biology and Fertility of Soils ( IF 5.1 ) Pub Date : 2024-04-05 , DOI: 10.1007/s00374-024-01814-z Balázs Grosz , Stefan Burkart , Reinhard Well
The absence of N2 flux measurements in liquid manure-amended soils has resulted in a poor understanding of the effect of manure application on gaseous N losses. The aim of this study was to quantify N2, N2O, CO2, N2O reduction to N2, depth distribution of moisture, water-extractable organic C, NO3−, NH4+, pH, and diffusivity in a laboratory incubation experiment with an arable silt-loam soil. To quantify N processes and gaseous fluxes, 15N tracing was applied. An artificial livestock slurry-mixture was added to the soil in various treatments (control, surface or injected application; slurry-application rate: 42.9 kg N ha− 1; soil water content of either 40% or 60% water-filled pore space (WFPS)). The soil was incubated for 10 days. The depth distribution of the control parameters was measured twice during the experiment on days 5 and 10. The average increase in N2 and N2O fluxes from denitrification was about 900% in slurry-amended soils. The highest N2 and N2O fluxes from denitrification were measured in the slurry injection, 60% WFPS treatment (7.83 ± 3.50 and 11.22 ± 7.60 mg N m− 2 d− 1, respectively). The hypothesis that injected slurry at a higher water content enhances denitrification was confirmed. This study provides important insights into the formation, spatial and temporal variation of the manure-soil hotspot and its impact on the denitrification process. The results will form part of a dataset to develop, improve and test manure application submodules of biogeochemical models and will help to understand in detail the effect of hotspots on N-cycling in manure-treated soils.
中文翻译:
液体有机肥及其施用方法对粉壤土耕地 N2、N2O 和 CO2 通量的短期影响
由于缺乏液体肥料改良土壤中的 N 2通量测量,导致人们对肥料施用对气态氮损失的影响了解甚少。本研究的目的是量化 N 2、N 2 O、CO 2、N 2 O 还原为 N 2、水分深度分布、水可萃取有机 C、NO 3 −、NH 4 +、pH 和扩散率用可耕种的粉砂壤土进行实验室孵化实验。为了量化 N 过程和气体通量,应用了15 N 示踪。在各种处理中将人工牲畜泥浆混合物添加到土壤中(对照、表面或注射施用;泥浆施用量:42.9 kg N ha − 1;土壤含水量为 40% 或 60% 充水孔隙空间(世界粮食计划署))。将土壤培养10天。在第 5 天和第 10 天的实验过程中,对控制参数的深度分布进行了两次测量。在泥浆改良土壤中,反硝化过程中N 2和 N 2 O 通量的平均增加量约为 900%。在浆液注入、60% WFPS 处理中测量了反硝化产生的最高 N 2和 N 2 O 通量(分别为 7.83 ± 3.50 和 11.22 ± 7.60 mg N m − 2 d − 1)。证实了注入较高含水量的浆料可增强反硝化作用的假设。这项研究为粪便-土壤热点的形成、时空变化及其对反硝化过程的影响提供了重要的见解。研究结果将构成数据集的一部分,用于开发、改进和测试生物地球化学模型的粪便施用子模块,并将有助于详细了解热点对粪便处理土壤中氮循环的影响。