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Ten years of free-air CO2 enrichment altered the mobilization of N from soil in Lolium perenne L. swards

机译:十年的自由空气CO2富集改变了黑麦草(Lolium perenne L.)草地中土壤中氮的迁移

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Effects of free-air carbon dioxide enrichment (FACE, 60 Pa pCO(2)) on plant growth as compared with ambient pCO(2) (36 Pa) were studied in swards of Lolium perenne L. (perennial ryegrass) at two levels of N fertilization (14 and 56 g m(-2) a(-1)) from 1993 to 2002. The objectives were to determine how plant growth responded to the availability of C and N in the long term and how the supply of N to the plant from the two sources of N in the soil, soil organic matter (SOM) and mineral fertilizer, varied over time. In three field experiments, N-15-labelled fertilizer was used to distinguish the sources of available N.In 1993, harvestable biomass under elevated pCO(2) was 7% higher than under ambient pCO(2). This relative pCO(2) response increased to 32% in 2002 at high N, but remained low at low N. Between 1993 and 2002, the proportions and amounts of N in harvestable biomass derived from SOM (excluding remobilized fertilizer) were, at high N, increasingly higher at elevated pCO(2) than at ambient pCO(2). Two factorial experiments confirmed that at high N, but not at low N, a higher proportion of N in harvestable biomass was derived from soil (including remobilized fertilizer) following 7 and 9 years of elevated pCO(2), when compared with ambient pCO(2).It is suggested that N availability in the soil initially limited the pCO(2) response of harvestable biomass. At high N, the limitation of plant growth decreased over time as a result of the stimulated mobilization of N from soil, especially from SOM. Consequently, harvestable biomass increasingly responded to elevated pCO(2). The underlying mechanisms which contributed to the increased mobilization of N from SOM under elevated pCO(2) are discussed. This study demonstrated that there are feedback mechanisms in the soil which are only revealed during long-term field experiments. Such investigations are thus, a prerequisite for understanding the responses of ecosystems to elevated pCO(2) and N supply.
机译:在两个水平的多年生黑麦草(Lolium perenne L.)(多年生黑麦草)的草地中研究了空气中二氧化碳富集(FACE,60 Pa pCO(2))对植物生长与环境pCO(2)(36 Pa)的影响。从1993年到2002年施氮(分别为14和56 gm(-2)a(-1))。目标是确定植物生长如何长期响应碳和氮的供应,以及氮如何向作物供不应求。植物从土壤中的氮的两种来源,即土壤有机质(SOM)和矿物肥料中随时间变化。在三个田间试验中,使用N-15标记的肥料来区分可利用的氮源.1993年,pCO(2)升高下的可收获生物量比周围pCO(2)高7%。在高氮水平下,相对pCO(2)的响应在2002年增加到32%,但在低氮水平下仍然较低。从1993年到2002年,源自SOM(不包括固定肥料)的可收获生物量中氮的比例和数量处于N,在升高的pCO(2)处比在环境pCO(2)处越来越高。两项析因实验证实,与环境pCO(7)相比,pCO(2)升高7年和9年后,在高氮而不是低氮下,可收获生物量中较高比例的氮来自土壤(包括固定肥料)。 2)。建议土壤中的N可用性最初限制了可收获生物量的pCO(2)响应。在高氮条件下,由于土壤,特别是SOM促进了N的迁移,植物生长的限制随时间降低。因此,可收获的生物量越来越多地对升高的pCO(2)作出响应。讨论了在升高的pCO(2)下增加SOM中N的动员的潜在机制。这项研究表明,土壤中存在反馈机制,只有在长期的野外实验中才能发现这些反馈机制。因此,此类调查是了解生态系统对pCO(2)和氮供应升高的响应的先决条件。

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