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Long-term nitrous oxide fluxes in annual and perennial agricultural and unmanaged ecosystems in the upper Midwest USA

机译:美国中西部上部一年生和多年生农业及未管理生态系统中的一氧化二氮长期通量

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Differences in soil nitrous oxide (N2O) fluxes among ecosystems are often difficult to evaluate and predict due to high spatial and temporal variabilities and few direct experimental comparisons. For 20 years, we measured N2O fluxes in 11 ecosystems in southwest Michigan USA: four annual grain crops (corn-soybean-wheat rotations) managed with conventional, no-till, reduced input, or biologically based/organic inputs; three perennial crops (alfalfa, poplar, and conifers); and four unmanaged ecosystems of different successional age including mature forest. Average N2O emissions were higher from annual grain and N-fixing cropping systems than from nonleguminous perennial cropping systems and were low across unmanaged ecosystems. Among annual cropping systems full-rotation fluxes were indistinguishable from one another but rotation phase mattered. For example, those systems with cover crops and reduced fertilizer N emitted more N2O during the corn and soybean phases, but during the wheat phase fluxes were similar to 40% lower. Likewise, no-till did not differ from conventional tillage over the entire rotation but reduced emissions similar to 20% in the wheat phase and increased emissions 30-80% in the corn and soybean phases. Greenhouse gas intensity for the annual crops (flux per unit yield) was lowest for soybeans produced under conventional management, while for the 11 other crop 9 management combinations intensities were similar to one another. Among the fertilized systems, emissions ranged from 0.30 to 1.33 kg N2O-N ha(-1) yr(-1) and were best predicted by IPCC Tier 1 and Delta EF emission factor approaches. Annual cumulative fluxes from perennial systems were best explained by soil NO3- pools (r(2) = 0.72) but not so for annual crops, where management differences overrode simple correlations. Daily soil N2O emissions were poorly predicted by any measured variables. Overall, long-term measurements reveal lower fluxes in nonlegume perennial vegetation and, for conservatively fertilized annual crops, the overriding influence of rotation phase on annual fluxes.
机译:由于高度的时空变化和很少的直接实验比较,通常难以评估和预测生态系统中土壤一氧化二氮(N2O)通量的差异。在20年的时间里,我们测量了美国密歇根州西南部11个生态系统中的N2O通量:采用常规,免耕,减少输入或基于生物/有机输入的方式管理四种年度谷物作物(玉米-大豆-小麦轮作);三种多年生作物(苜蓿,杨树和针叶树);以及四个不同演替年龄的不受管理的生态系统,包括成熟的森林。一年生谷物和固氮作物系统的平均N2O排放量高于非豆类多年生作物系统的平均N2O排放,并且在不受管理的生态系统中平均排放量较低。在一年生种植系统中,全旋通量彼此之间没有区别,但旋回相位很重要。例如,那些覆盖作物且氮肥减少的系统在玉米和大豆阶段排放的N2O增多,但在小麦阶段,通量减少了40%。同样,免耕与常规耕作在整个轮作中没有什么不同,但是在小麦期减少的排放量接近20%,在玉米和大豆期减少的排放量增加30-80%。在常规管理下生产的大豆,年度作物的温室气体强度(每单位产量通量)最低,而在其他11种作物上,9种管理组合的强度彼此相似。在施肥系统中,排放量从0.30到1.33 kg N2O-N ha(-1)yr(-1)不等,最好通过IPCC Tier 1和Delta EF排放因子方法进行预测。多年生系统的年度累积通量最好用土壤NO3-库来解释(r(2)= 0.72),但对于一年生作物却不是这样,因为一年生作物的管理差异覆盖了简单的相关性。任何测量变量均无法很好地预测每日土壤N2O排放量。总体而言,长期测量显示,非豆科多年生植物的通量较低,而对于保守施肥的一年生作物,轮作期对年通量的影响最为显着。

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