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Nitrogen-15 budget in model ecosystems of white clover and perennial ryegrass exposed for four years at elevated atmospheric pCO(2)

机译:在大气pCO升高下暴露四年的白三叶草和多年生黑麦草模型生态系统中的氮15预算(2)

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Although there are many indications that N cycling in grassland ecosystems changes under elevated atmospheric CO2 partial pressure (pCO(2)), most information has been obtained in short-term studies. Thus, N budgets were established for four years under ambient and 60 Pa pCO(2) at two levels of N fertilization in two contrasting model ecosystems: Trifolium repens L. (white clover) and Lolium perenne L. (perennial ryegrass) were planted in soil in boxes in the Swiss FACE experiment. While T. repens showed an 80% increase in harvested biomass with no change in biomass allocation under elevated atmospheric pCO(2) compared to ambient conditions, L. perenne showed an increase only in the biomass of the roots. During the four years of the experiment, the systems gained N both from N retained in the soil and from stubble/stolon and roots left after the final harvest; in total between 11 and 86 gN m(-2). Nitrogen retention in the soil was between 4 and 64 g m(2). The L. perenne system gained the most N and retained the most N in the soil at high N fertilization and elevated atmospheric pCO(2). The input of new C and N into the soil correlated well in the L. perenne systems but not in the T. repens systems. Elevated atmospheric pCO(2) led neither to an increase in N retention in the soil nor did it reduce the loss of N from the soil. In the L. perenne systems, N fertilization played the main role in both the retention of N and the sequestration of C, while in the T. repens systems symbiotic N-2 fixation may have controlled N retention in the soil.
机译:尽管有许多迹象表明,草地生态系统中的氮循环会在大气CO2分压升高的情况下发生变化(pCO(2)),但大多数信息是通过短期研究获得的。因此,在两个相反的模型生态系统中,在两个不同的模型生态系统中,在两个氮肥水平下,分别在环境和60 Pa pCO(2)下确定了四年的氮预算:三叶草(白叶三叶草)和多年生黑麦草(黑麦草)。瑞士FACE实验中的盒子中的土壤。与环境条件相比,在大气pCO(2)升高的条件下,白三叶显示收获的生物量增加了80%,而生物量分配没有变化,但紫苏只显示了根部的生物量增加。在实验的四年中,系统从土壤中保留的氮以及最后收获后留下的残茬//茎和根中获得了氮。总共介于11到86 gN m(-2)之间。氮在土壤中的保留量为4至64 g m(2)。在高氮施肥和升高的大气pCO(2)的条件下,L。perenne系统获得最多的N,并在土壤中保留最多的N。在Perennes L.系统中,新的C和N在土壤中的输入相关性很好,而在T. repens系统中则没有相关性。升高的大气pCO(2)既不会增加土壤中氮的保留,也不会减少土壤中氮的损失。在L. perenne系统中,N的施肥在N的保留和C的固存中起主要作用,而在T. repens系统中,共生的N-2固定可能控制了土壤中的N保留。

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