脱化有助于在米土壤中产生N2O排放
Hua Xiang1,2,3, Yiguo Hong2, Jiapeng Wu2
1State Key Laboratory of Tropical Oceanography (LTO), South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.
田土壤在脱过程中释放氧化 (N2O),这是由于N2O生产和减少途径的不平衡造成的. 特定的微生物群落有助于这种显著的N2O排放.
科学领域:
- 环境微生物学 环境微生物学
- 生物地质化学生物地质化学
- 土壤科学 土壤科学
背景情况:
- 脱对于循环和温室气体排放至关重要.
- 米土壤是脱的重要贡献者.
- 田土壤脱的氧化 (N2O) 排放机制尚不清楚.
研究的目的:
- 调查田土壤脱的N2O排放潜力.
- 分析与N2O生产和减少相关的酶活性.
- 确定微生物群落的组成和涉及到脱的基因丰度.
主要方法:
- 使用了15N同位素追踪技术.
- 进行了泥化实验.
- 测量了酶活性,定量聚合酶链反应 (qPCR) 和元基因组测序.
主要成果:
- 确定了0.51 ± 0.20 μmol⋅N⋅kg-1的平均潜在N2O排放率 (2.16 ± 0.85%的脱化).
- 观察到较高的N2O生产酶活性 (2.778.94倍) 比减少活性,表明一个不平衡.
- 甲基因组分析揭示了特定的微生物类,如Gammaproteobacteria,有助于N2O排放.
结论:
- 麦田土壤脱化表现出有利于N2O生产的不平衡,导致大量的排放.
- 脱化是一种模块化过程,涉及各种微生物群落.
- 据估计,表面土的N2O年排放量为13.67 ± 5.44 gN2O⋅m-2⋅yr-1.
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