全球森林中大气沉积保留的模式和驱动因素
Quanhong Lin1,2, Jianxing Zhu1, Qiufeng Wang1,2
1Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China.
Global change biology
|July 9, 2024
概括
森林保留了超过60%的 (N) 输入量,土壤作为主要的沉. 了解保留对于预测森林碳捕获在增加沉积的情况下至关重要.
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
- 森林科学 森林科学 森林科学
背景情况:
- 森林是关键的陆地碳汇,但它们的容量受到 (N) 沉积的影响.
- 不同森林区的外部N输入的命运和保留模式尚未完全理解.
- 留机制是理解森林碳捕获潜力的关键.
研究的目的:
- 综合全球关于森林中-15 (15N) 标记物实验的数据.
- 揭示森林植物和土壤中15N保留的变化和潜在机制.
- 调查气候和营养动态对保持的影响.
主要方法:
- 从全球森林15N追踪器实验中对408个观测结果的元分析.
- 在整个生态系统,植物和土壤池中的15N保留量的量化.
- 分析区域差异 (亚热带,热带,温带) 和影响因素.
主要成果:
- 全球森林平均保留了15N的63.04%±1.23%,其中土壤是主要的沉积点 (45.76%±1.29%).
- 植物吸收了17.28%±0.83%的15N,主要是叶子和根.
- 与亚热带和热带森林相比,温带森林在有机土壤层中的保留率更高.
结论:
- 森林中的保留受到沉积,气候和营养素供应/需求的显著影响.
- 土壤有机层在保持中起着至关重要的作用,特别是在温带地区.
- 了解这些因素对于预测森林对沉积的反应及其在碳捕获中的作用至关重要.
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