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Contribution of crop residue, soil, and fertilizer nitrogen to nitrous oxide emissions varies with long-term crop rotation and tillage

机译:作物残余物,土壤和肥料氮对氧化亚氮排放的贡献随着长期作物旋转和耕作而变化

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摘要

Agriculture is an important contributor to N_2O emissions - a potent greenhouse gas - with high peaks occurring when soil mineral nitrogen (N) is high (e.g., after mineralization of organic N and N fertilizer application). Nitrogen dynamics in soil and consequently N_2O emissions are affected by crop and soil management practices (e.g., crop rotation and tillage), an effect mostly assessed in the literature through comparisons of total N_2O emission. Hence, information is scarce on the effect of these management practices on specific N sources affecting N_2O emissions (i.e., N fertilizer, soil, above and belowground crop residues) - a knowledge gap explored in this study with the use of ~(15)N tracers. The isotope approach enabled refinement on global N_2O budget by directly determining the emission factors (EF) of above and belowground crop residues that vary in chemical composition and comparison with default EF values (e.g., IPCC EFs). Our experiment was conducted over the full-cycle of long-term crop rotations to (ⅰ) compare N_2O totals and intensity, under no-tillage and conventional tillage, simple and diverse rotation; (ⅱ) partition total N_2O emissions into soil, N fertilizer, above and belowground crop residue N sources; (ⅲ) compare the 12-month EF of crop residue against the default values proposed by IPCC (2019). For the tillage effect, annual N_2O emissions were from 1.2- to 2.0-times higher on CT than NT soil due to 40% increased soil N derived N_2O emission in CT. The diversified crop rotation emitted 1.3-times higher N_2O than the simple rotation over the full-cycle of the rotations, but the effect was due to differences in N fertilizer rate between the rotations since emissions were equivalent when scaled by N rate. Finally, our results suggested that default IPCC EF are overestimated for crop residues under CT and NT, simple and diverse rotations as measured EFs never surpassed 0.1%.
机译:农业是N_2O排放的重要贡献者 - 一种有效的温室气体 - 当土壤矿物氮(N)高(例如,有机N和N和N肥料矿化后的矿化后)发生高峰。土壤中的氮动力学以及N_2O排放受作物和土壤管理实践的影响(例如,作物旋转和耕作),通过总N_2O排放的比较,在文献中主要评估的效果。因此,信息稀缺了这些管理实践对影响N_2O排放的特定N个来源的效果(即,N肥料,土壤,上述作物残留物) - 本研究中探讨了这项知识差距,使用〜(15)n跟踪器。通过直接确定上述和以下作物残留物的排放因子(EF)在化学成分中的排放因子(EF)和与默认EF值(例如,IPCC EFS)进行比较,使Isotope方法能够通过直接确定上述的排放因子(EF)并进行细化。我们的实验是在长期作物旋转的全周期内进行的(Ⅰ)比较N_2O总数和强度,无耕作和常规耕作,简单多样化; (Ⅱ)将总N_2O排放分配成土壤,氮肥,高于和地下庄稼残留物。 (Ⅲ)将作物残留的12个月EF与IPCC(2019年)提出的违约值进行比较。对于耕作效应,由于CT的N_2O发射量增加了40%,每年N_2O排放量比CT对NT土壤高1.2至2.0倍。多样化的作物旋转比旋转全周期的简单旋转,但效果是由于在缩放时排放的旋转之间的N肥率之间的差异。最后,我们的结果表明,默认的IPCC EF在CT和NT下的裁剪残留量高估,随着测量的EF从未超过0.1%的情况下,简单和多样化的旋转。

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