不是所有的土壤碳都是平等的:在的输入下,不稳定和稳定的池
Huadong Zang1, Imran Mehmood2,3, Yakov Kuzyakov4,5
1College of Agronomy and Biotechnology, China Agricultural University, Beijing, China.
Global change biology
|July 8, 2024
概括
的输入减少了土壤有机物 (SOM) 的分解,特别是在不稳定的池中. 这一发现对于理解土壤碳捕集潜力在增加沉积下至关重要.
科学领域:
- 土壤科学 土壤科学
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
背景情况:
- 人类活动在全球范围内增加了 (N) 投入,影响了土壤碳 (C) 循环.
- 输入对不同微生物可用性的土壤有机物 (SOM) 池的影响尚未完全理解.
研究的目的:
- 调查N输入对不同周转时间的SOM池的影响.
- 要量化各种SOM池对N的敏感性.
主要方法:
- 利用了SOM中13C自然丰富度和21年的C3C-C4植物转换的组合.
- 采用长期化方法来评估SOM矿化率.
- 随着时间的推移,分析了微生物群落和功能基因的变化.
主要成果:
- 输入抑制了所有SOM池的矿化,对不稳定池的影响更大.
- 非常不稳定的C池对N添加表现出最高的敏感性 (18%-52%抑制).
- 随着时间的推移,细菌群落的变化和降低降解基因表达导致了N诱导的SOM抑制.
结论:
- 不稳定的SOM池对N的可用性更敏感,并且显示出更强的矿化抑制.
- 增加N的可用性可能会提高全球不稳定SOM池中的C封存潜力.
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