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首页> 外文期刊>European Journal of Agronomy >Long-term effect of tillage, crop rotation and N fertilization to wheat on gaseous emissions under rainfed Mediterranean conditions
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Long-term effect of tillage, crop rotation and N fertilization to wheat on gaseous emissions under rainfed Mediterranean conditions

机译:地中海雨养条件下耕作,轮作和氮肥对小麦气体排放的长期影响

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摘要

A field study was conducted to assess the effect of N fertilizer application to wheat (Triticum aestivum L.), tillage system and crop rotation on total denitrification N losses, NO and CO emissions under Mediterranean conditions in a long-term trial started 18 years ago on a Vertisol soil. The tillage system consisted of conventional tillage vs. no-tillage and the crop rotation system consisted of two different 2-years rotations: wheat-sunflower (Helianthus annuus L.) (WS) and wheat-faba bean (Vicia faba L.) (WF). Fertilizer rates were 0 and 100kgNhap# applied to wheat splitted in two amendments of 50kgNhap# each. Two different fertilization systems were studied. In the old fertilized plots system fertilizer had been applied for 18 years since the beginning of the trial, and in the new fertilized plots system fertilizer was applied for the first time when this experiment was started. Measurements were carried out after fertilizer applications. In the long term, continued fertilizer application produced a higher soil total N content. Nevertheless, no increase in denitrification potential, NO+N production by denitrification, NO or CO emissions was observed either by the recent application of N or by the continued application during 18 years. The soil presented a higher potential to denitrify up to N than up to NO. So, denitrification was probably occurring mainly in the form of N, while NO emissions were occurring in a great manner by nitrification, both denitrification and nitrification occurring simultaneously at soil field capacity (60-70%) expressed as water filled pore space (WFPS). Conventional tillage induced an increase in soil total N content and in the potential to denitrify up to N with respect to no-tillage. This higher potential was translated into higher NO+N production by denitrification presumably stimulated in the short time by the higher available carbon provided by decomposing roots and by the subsequent creation of soil anaerobic microsites. Contrarily, no effect of tillage was observed on NO emissions because of being produced in an important manner by nitrification, which does not depend on carbon availability. The wheat-faba bean rotation induced higher soil nitrate contents than the wheat-sunflower, although the effect in the long time was not observed regarding soil total N content. The same as for the fertilizer effect, this increase in nitrate content was not followed by a higher denitrification potential or higher NO+N production by denitrification because of the lack of organic matter, while an increase was observed in NO emissions.
机译:在18年前开始的一项长期试验中,进行了一项田间研究,以评估在地中海条件下施氮对小麦(Triticum aestivum L.),耕作制度和作物轮作对总反硝化氮损失,NO和CO排放的影响。在Vertisol土壤上。耕作制度包括常规耕作与免耕,轮作制度包括两种不同的两年轮作:小麦-向日葵(向日葵)和小麦-蚕豆(野豌豆)( WF)。施肥量为0和100kgNhap#应用于分裂为两个50kgNhap#的两个修正案的小麦。研究了两种不同的施肥系统。自试验开始以来,在旧的施肥地系统中已施肥18年,而在新的施肥地系统中,该实验开始时首次施肥。施肥后进行测量。从长远来看,持续施用肥料会产生更高的土壤总氮含量。然而,无论是最近施用的氮还是18年间的连续施用,都未观察到反硝化潜力,反硝化产生的NO + N,NO或CO排放量的增加。土壤对氮的反硝化作用比对氮的反硝化作用更大。因此,反硝化作用可能主要以N的形式发生,而NO的排放则主要通过硝化作用发生,反硝化作用和硝化作用同时发生在土壤田间持水量(60-70%)处,以充水孔隙空间(WFPS)表示。 。常规耕作导致土壤总氮含量的增加,并且就免耕而言增加了反硝化能力。这种高潜力转化为更高的NO + N产量,这可能是由于在短时间内通过分解根而提供的更高的可用碳以及随后产生的土壤厌氧性微场所而激发的反硝化作用所激发的。相反,未观察到耕作对NO排放的影响,因为硝化以重要方式产生硝化,而硝化不依赖于碳的有效性。尽管没有观察到土壤总氮含量的长期影响,但小麦-蚕豆轮作引起的土壤硝酸盐含量高于小麦-向日葵。与肥料作用相同,由于缺乏有机物,硝酸盐含量的增加不会导致更高的反硝化潜能或更高的反硝化产量,而观察到的是NO排放量的增加。

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