储存的驱动因素及其对中国森林碳封存的贡献
Geshere Abdisa Gurmesa1,2,3, Ang Wang1,2,3, Shanlong Li4
1CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang, China.
Global change biology
|January 31, 2026
概括
中国的森林保留约65%的沉积 (N),主要是在土壤中. 这种沉积增强了森林的碳 (C) 捕获,大大增加了中国森林的碳沉积.
科学领域:
- 森林生态 森林生态
- 生物地质化学生物地质化学
- 全球变化生物学
背景情况:
- 人为 (N) 沉积影响森林碳 (C) 循环.
- 了解的保留及其在森林C封存中的作用至关重要,特别是在像中国这样高沉积的地区.
- 之前的研究缺乏系统的区域综合,以澄清沉积对中国森林的影响.
研究的目的:
- 量化中国多样化的森林生态系统中留量及其在植物和土壤池中的分布.
- 确定影响N保留和分区的驱动因素.
- 评估N沉积对森林C捕获的贡献.
主要方法:
- 综合了几十年来在中国北极到热带森林的15N追踪器实验中获得的数据.
- 对保持的分析,在植物生物质和土壤池之间进行分区.
- 立体测量缩放以估计每单位存储的N的C封存.
主要成果:
- 中国的森林平均保留了约65%的沉积N,约2/3储存在土壤中.
- N保留和分割因气候,森林相继阶段和N形式而有所不同.
- 总生态系统保留效率从北极森林下降到热带森林.
- 沉积增加了约0.11 Pg C 的碳封存,1年,为中国的森林碳沉降贡献了20%至30%.
结论:
- 的保留和其对C封存的贡献受到区域环境因素和森林特征的影响.
- 中国的森林在保留沉积的N和隔离C方面发挥着至关重要的作用.
- 研究结果为预测未来全球变化情景下的森林N和C动态提供了关键的见解.
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