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首页> 外文期刊>Global change biology >Global soil nitrous oxide emissions since the preindustrial era estimated by an ensemble of terrestrial biosphere models: Magnitude, attribution, and uncertainty
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Global soil nitrous oxide emissions since the preindustrial era estimated by an ensemble of terrestrial biosphere models: Magnitude, attribution, and uncertainty

机译:全球土壤二氮氧化物排放自陆地生物圈模型的集合估计以来:数值,归因和不确定性

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摘要

Our understanding and quantification of global soil nitrous oxide (N2O) emissions and the underlying processes remain largely uncertain. Here, we assessed the effects of multiple anthropogenic and natural factors, including nitrogen fertilizer (N) application, atmospheric N deposition, manure N application, land cover change, climate change, and rising atmospheric CO2 concentration, on global soil N2O emissions for the period 1861-2016 using a standard simulation protocol with seven process-based terrestrial biosphere models. Results suggest global soil N2O emissions have increased from 6.3 +/- 1.1 Tg N2O-N/year in the preindustrial period (the 1860s) to 10.0 +/- 2.0 Tg N2O-N/year in the recent decade (2007-2016). Cropland soil emissions increased from 0.3 Tg N2O-N/year to 3.3 Tg N2O-N/year over the same period, accounting for 82% of the total increase. Regionally, China, South Asia, and Southeast Asia underwent rapid increases in cropland N2O emissions since the 1970s. However, US cropland N2O emissions had been relatively flat in magnitude since the 1980s, and EU cropland N2O emissions appear to have decreased by 14%. Soil N2O emissions from predominantly natural ecosystems accounted for 67% of the global soil emissions in the recent decade but showed only a relatively small increase of 0.7 +/- 0.5 Tg N2O-N/year (11%) since the 1860s. In the recent decade, N fertilizer application, N deposition, manure N application, and climate change contributed 54%, 26%, 15%, and 24%, respectively, to the total increase. Rising atmospheric CO2 concentration reduced soil N2O emissions by 10% through the enhanced plant N uptake, while land cover change played a minor role. Our estimation here does not account for indirect emissions from soils and the directed emissions from excreta of grazing livestock. To address uncertainties in estimating regional and global soil N2O emissions, this study recommends several critical strategies for improving the process-based simulations.
机译:我们对全球土壤二氮氧化物(N2O)排放和潜在过程的理解和定量仍然很大程度上不确定。在这里,我们评估了多种人类学和自然因素的影响,包括氮肥(N)施用,大气压沉积,粪便N应用,陆地覆盖变化,气候变化和大气二氧化碳浓度上升,在全球土壤N2O排放期间1861-2016使用具有七个基于过程的地面生物圈模型的标准仿真协议。结果表明全球土壤N2O排放量从预工业期的6.3 +/- 1.1 TG N2O-N /年增加到最近十年(2007-2016)中的9.3 +/- 1.1 TG N2O-N /年。农田土壤排放量从0.3 TG N2O-N /年增加到3.3 TG N2O-N /持续时间,占总增加的82%。自20世纪70年代以来,从地区,中国,南亚和东南亚正在迅速增加农田N2O排放量。然而,自20世纪80年代以来,美国农田N2O排放量幅度相对平整,而欧盟农田N2O排放似乎减少了14%。土壤N2O排放量主要是自然生态系统占近十年来全球土壤排放量的67%,而自1860年代以来仅显示了0.7 +/- 0.5 TG N2O-N /年(11%)的相对较小的增加。近十年来,N肥施用,N沉积,粪便N应用和气候变化分别贡献了54%,26%,15%和24%,以总增加。大气CO 2浓度上升10%通过增强的植物注量减少土壤N2O排放量,陆地覆盖变动发挥了次要作用。我们的估计不会考虑来自土壤的间接排放以及放牧牲畜的排泄物的定向排放。为了解决估计区域和全球土壤N2O排放的不确定性,本研究建议改善基于过程的模拟的几种关键策略。

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