沉积削弱了土壤碳 控制动态在整个邻近的美国
Matthew A Nieland1, Piper Lacy1, Steven D Allison2,3
1Stockbridge School of Agriculture, University of Massachusetts Amherst, Amherst, Massachusetts, USA.
Global change biology
|December 27, 2024
概括
人为沉积破坏了土壤碳和变化之间的联系. 较高的输入削弱了微生物竞争,改变了土壤碳如何预测整个生态系统的化率.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 环境科学 环境科学
背景情况:
- 人为 (N) 沉积在空间和时间上有所变化,受到工业法规和人类活动的影响.
- 土壤中的碳 (C) 含量通常控制矿化N的化分数 (ƒnitrified),影响N的生物可用性.
- 沉积对土壤C和N转化之间的关系的影响仍然不清楚.
研究的目的:
- 调查N沉积是否会改变土壤C和净N转化 (矿化和化) 之间的既定关系.
- 评估沉积率对各种陆地生态系统中化的影响.
主要方法:
- 从14个美国地区的森林,草原和院子收集了土壤,N沉积率各不相同.
- 量化净化,矿化,土壤化学 (C,N,pH),以及微生物生物质和酶活动 (BG,NAG).
主要成果:
- 增加土壤C与降低净化和化度相关,正如预期的那样.
- 较高的N沉积增加了化,降低了土壤C的预测能力,特别是在土壤C高的地点.
- 在COVID-19大流行期间,N沉积对土壤C-ƒ化关系的影响仍然存在,尽管沉积减少.
结论:
- 沉积可以破坏土壤C和净N转换之间的关系,可能是由于微生物N竞争减少.
- 预测陆地生态系统中的N动态需要考虑过去的N输入和土壤C含量.
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