多年生黑麦草
土壤水分
磷
农学
黑麦草
化学
氮气
接种
生物量(生态学)
园艺
禾本科
生物
环境科学
土壤科学
有机化学
作者
Yawen Shen,Tianle Xu,Baodong Chen,Biao Zhu
出处
期刊:Rhizosphere
[Elsevier BV]
日期:2021-07-17
卷期号:19: 100414-100414
被引量:13
标识
DOI:10.1016/j.rhisph.2021.100414
摘要
Although phosphorus (P) addition and arbuscular mycorrhizal fungal (AMF) colonization have potential for mitigating soil N2O emission, the effects and mechanisms remain unresolved. We conducted a pot experiment with ryegrass (Lolium perenne) growing in a growth chamber for 80 days with three factors: Plant and AMF presence (unplanted, with plants, with plants colonized by AMF), two nitrogen (N) addition levels (0 and 50 mg N kg−1 soil) and two P addition levels (0 and 20 mg P kg−1 soil). Our results showed that N addition and AMF colonization had insignificant effects on soil N2O emission. However, the presence of plants decreased soil N2O emission by 90%–99% (planted vs. unplanted) under P addition. Moreover, P addition increased (+134%) N2O emission from unplanted soil, but decreased (74%–98%) it from planted soil. Further analysis showed that soil N2O emission was controlled by soil available P, soil NO3−-N, plant biomass P and N across all treatments. The lower N2O emissions from planted soils were mainly due to the lower soil NO3−-N content which might be immobilized by plant biomass, while the higher N2O emissions from unplanted soils under P addition were attributed to the increased soil available P content. Furthermore, we found an antagonistic effect between AMF inoculation and P addition on soil N2O emission because sufficient soil P may inhibit AMF colonization and activity. Taken together, we conclude that plant presence combined with P addition can effectively reduce N2O emission from P-limited soils.
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