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Warming prevents the elevated CO2-induced reduction in available soil nitrogen in a temperate, perennial grassland

机译:变暖可防止温带多年生草原中二氧化碳升高引起的土壤有效氮减少

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摘要

Rising atmospheric carbon dioxide concentration ([CO2]) has the potential to stimulate ecosystem productivity and sink strength, reducing the effects of carbon (C) emissions on climate. In terrestrial ecosystems, increasing [CO2] can reduce soil nitrogen (N) availability to plants, preventing the stimulation of ecosystem C assimilation; a process known as progressive N limitation. Using ion exchange membranes to assess the availability of dissolved organic N, ammonium and nitrate, we found that CO2 enrichment in an Australian, temperate, perennial grassland did not increase plant productivity, but did reduce soil N availability, mostly by reducing nitrate availability. Importantly, the addition of 2 degrees C warming prevented this effect while warming without CO2 enrichment did not significantly affect N availability. These findings indicate that warming could play an important role in the impact of [CO2] on ecosystem N cycling, potentially overturning CO2-induced effects in some ecosystems.
机译:大气中二氧化碳浓度([CO2])的上升可能会刺激生态系统的生产力和汇聚强度,从而减少碳(C)排放对气候的影响。在陆地生态系统中,增加的[CO2]会减少植物对土壤氮(N)的利用,从而阻止了对生态系统碳同化的刺激。这个过程称为渐进N限制。使用离子交换膜评估溶解性有机氮,铵和硝酸盐的有效性,我们发现在澳大利亚温带多年生草原上富集二氧化碳并没有增加植物的生产力,但确实减少了土壤氮的利用率,主要是通过减少硝酸盐的利用率。重要的是,增加2°C的温度可防止此影响,而没有CO2富集的温度不会显着影响氮的有效性。这些发现表明,变暖可能在[CO2]对生态系统N循环的影响中起重要作用,有可能推翻某些生态系统中由CO2引起的影响。

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