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Moderate precipitation reduction enhances nitrogen cycling and soil nitrous oxide emissions in a semi‐arid grassland

机译:适度降水减少促进了半干旱草地氮循环和土壤一氧化二氮排放

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摘要

Abstract The ongoing climate change is predicted to induce more weather extremes such as frequent drought and high‐intensity precipitation events, causing more severe drying‐rewetting cycles in soil. However, it remains largely unknown how these changes will affect soil nitrogen (N)‐cycling microbes and the emissions of potent greenhouse gas nitrous oxide (N2O). Utilizing a field precipitation manipulation in a semi‐arid grassland on the Loess Plateau, we examined how precipitation reduction (ca. −30) influenced soil N2O and carbon dioxide (CO2) emissions in field, and in a complementary lab‐incubation with simulated drying‐rewetting cycles. Results obtained showed that precipitation reduction stimulated plant root turnover and N‐cycling processes, enhancing soil N2O and CO2 emissions in field, particularly after each rainfall event. Also, high‐resolution isotopic analyses revealed that field soil N2O emissions primarily originated from nitrification process. The incubation experiment further showed that in field soils under precipitation reduction, drying‐rewetting stimulated N mineralization and ammonia‐oxidizing bacteria in favor of genera Nitrosospira and Nitrosovibrio, increasing nitrification and N2O emissions. These findings suggest that moderate precipitation reduction, accompanied with changes in drying‐rewetting cycles under future precipitation scenarios, may enhance N cycling processes and soil N2O emissions in semi‐arid ecosystems, feeding positively back to the ongoing climate change.
机译:摘要 持续的气候变化预计将引发更多的极端天气,如频繁的干旱和高强度降水事件,导致土壤干燥-再润湿循环更加严重。然而,这些变化将如何影响土壤氮(N)循环微生物和强效温室气体一氧化二氮(N2O)的排放,这在很大程度上仍然未知。利用黄土高原半干旱草地的野外降水操纵,我们研究了降水减少(约-30%)如何影响田间土壤N2O和二氧化碳(CO2)排放,以及与模拟干燥-再润湿循环的补充实验室培养。结果表明,降水减少刺激了植物根系周转和氮循环过程,增加了田间土壤N2O和CO2的排放,特别是在每次降雨事件后。此外,高分辨率同位素分析表明,田间土壤N2O排放主要来源于硝化过程。孵育实验进一步表明,在降水减少的田间土壤中,干燥-再润湿刺激了氮矿化和氨氧化细菌,有利于亚硝螺属和亚硝化菌属,增加了硝化作用和N2O排放。这些结果表明,在未来降水情景下,适度的降水减少,伴随着干再润湿循环的变化,可能会增强半干旱生态系统的氮循环过程和土壤N2O排放,从而对持续的气候变化产生积极反馈。

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