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Processes regulating progressive nitrogen limitation under elevated carbon dioxide: a meta-analysis

机译:在升高的二氧化碳下调节渐进式氮限制的过程:荟萃分析

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The nitrogen (N) cycle has the potential to regulate climate change through its influence on carbon (C) sequestration. Although extensive research has explored whether or not progressive N limitation (PNL) occurs under COsub2/sub enrichment, a comprehensive assessment of the processes that regulate PNL is still lacking. Here, we quantitatively synthesized the responses of all major processes and pools in the terrestrial N cycle with meta-analysis of COsub2/sub experimental data available in the literature. The results showed that COsub2/sub enrichment significantly increased N sequestration in the plant and litter pools but not in the soil pool, partially supporting one of the basic assumptions in the PNL hypothesis that elevated COsub2/sub results in more N sequestered in organic pools. However, COsub2/sub enrichment significantly increased the N influx via biological N fixation and the loss via Nsub2/subO emission, but decreased the N efflux via leaching. In addition, no general diminished COsub2/sub fertilization effect on plant growth was observed over time up to the longest experiment of 13 years. Overall, our analyses suggest that the extra N supply by the increased biological N fixation and decreased leaching may potentially alleviate PNL under elevated COsub2/sub conditions in spite of the increases in plant N sequestration and Nsub2/subO emission. Moreover, our syntheses indicate that COsub2/sub enrichment increases soil ammonium (NHsub4/subsup+/sup) to nitrate (NOsub3/subsup?/sup) ratio. The changed NHsub4/subsup+/sup/NOsub3/subsup?/sup ratio and subsequent biological processes may result in changes in soil microenvironments, above-belowground community structures and associated interactions, which could potentially affect the terrestrial biogeochemical cycles. In addition, our data synthesis suggests that more long-term studies, especially in regions other than temperate ones, are needed for comprehensive assessments of the PNL hypothesis.
机译:氮(N)循环有可能通过影响碳(C)的固存来调节气候变化。尽管广泛的研究探索了在CO 2 富集下是否发生进行性N限制(PNL),但仍缺乏对调节PNL的过程的全面评估。在这里,我们通过文献中对CO 2 实验数据的荟萃分析,定量合成了陆地N循环中所有主要过程和池的响应。结果表明,CO 2 的富集显着增加了植物和凋落物库中的固氮能力,但并未增加土壤池中的固氮能力,部分支持了PNL假设中CO 2 < / sub>导致更多N被隔离在有机池中。然而,CO 2 的富集通过生物固氮作用显着增加了N的流入量,而N 2 O的排放则显着增加了氮的损失,但浸出却降低了N的流出量。另外,直到13年的最长实验,随着时间的推移,未观察到CO 2 对植物生长的普遍影响。总体而言,我们的分析表明,尽管植物固氮和N 2的增加,但生物固氮增加和淋溶减少导致的额外氮供应可能会在CO 2 升高的条件下缓解PNL。 O排放。此外,我们的合成结果表明,CO 2 的富集将土壤铵盐(NH 4 + )增加为硝酸盐(NO 3 )的比率。 NH 4 + / NO 3 比值的变化以及随后的生物过程可能导致土壤微环境的变化,地下地上的群落结构及其相关相互作用,可能会影响陆地生物地球化学循环。此外,我们的数据综合表明,需要进行更长期的研究,尤其是在温带地区以外的地区,才能对PNL假设进行全面评估。

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