Zhang Kangcheng, Qiu Yunpeng, Zhao Yunfeng, Wang Shuhong, Deng Jun, Chen Mengfei, Xu Xinyu, Wang Hao, Bai Tongshuo, He Tangqing, Zhang Yi, Chen Huaihai, Wang Yi, Hu Shuijin
College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, 210095, China.
Ningxia Yunwu Mountains Grassland Natural Reserve Administration, Guyuan, 756000, China.
Glob Chang Biol. 2023 Jun;29(11):3114-3129. doi: 10.1111/gcb.16672. Epub 2023 Mar 17.
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 (N O). Utilizing a field precipitation manipulation in a semi-arid grassland on the Loess Plateau, we examined how precipitation reduction (ca. -30%) influenced soil N O and carbon dioxide (CO ) 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 N O and CO emissions in field, particularly after each rainfall event. Also, high-resolution isotopic analyses revealed that field soil N O 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 N O 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 N O emissions in semi-arid ecosystems, feeding positively back to the ongoing climate change.
预计持续的气候变化将引发更多极端天气,如频繁干旱和高强度降水事件,导致土壤中干湿循环更为剧烈。然而,这些变化将如何影响土壤氮循环微生物以及强效温室气体一氧化二氮(N₂O)的排放,在很大程度上仍不清楚。利用黄土高原半干旱草原的田间降水控制实验,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,并在补充的实验室模拟干湿循环培养实验中进行了研究。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排放,尤其是在每次降雨事件之后。此外,高分辨率同位素分析表明,田间土壤N₂O排放主要源于硝化过程。培养实验进一步表明,在降水减少条件下的田间土壤中,干湿循环刺激了氮矿化和氨氧化细菌,有利于亚硝化螺菌属和亚硝化弧菌属,增加了硝化作用和N₂O排放。这些发现表明,在未来降水情景下,适度降水减少伴随着干湿循环变化,可能会增强半干旱生态系统中的氮循环过程和土壤N₂O排放,从而对当前的气候变化产生正反馈。