在中国的森林中延长植被碳循环时间
Rong Ge1, Xiaoli Ren2, Honglin He3
1Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; Institute of Natural Resources and Environmental Audits, School of National Audit, Nanjing Audit University, Nanjing 211815, China.
Science bulletin
|February 3, 2026
概括
在中国的年轻森林中,植物碳循环时间正在增加,与欧洲和北美的老森林不同. 这一趋势是由比分解更快的增长驱动的,影响了碳捕获和气候减缓努力.
科学领域:
- 陆地生态系统科学 地球生态系统科学
- 气候变化研究 气候变化研究
- 森林生态 森林生态
背景情况:
- 植物碳循环时间 (τveg) 是陆地碳循环不确定性的关键因素.
- 欧洲和北美的成熟森林显示,由于气候变化,tveg的减少.
- 在年轻森林中 τveg 的趋势仍然不清楚.
研究的目的:
- 调查中国主要年轻森林中植被碳循环时间 (τveg) 的时间趋势.
- 了解年轻森林生态系统中tveg动态的驱动因素.
- 为土地表面模型和森林管理策略提供信息.
主要方法:
- 使用多源数据模型同化.
- 在中国的森林中采用长期网络观测.
- 分析了森林年龄结构和环境因素,如沉积和二氧化碳水平.
主要成果:
- 揭示了中国森林中 τveg 的总体显著增加 (每年 0.025 ± 0.002 年).
- 观察到,在高沉积的年轻森林中,增加的CO2加快了生长速度,增加了t.
- 证明年轻森林因与生长相比的分解速度较慢而更有效地封存碳.
结论:
- 森林年龄显著影响tveg动态,年轻的森林显示增加的周转时间.
- 对陆地碳循环和气候缓解的准确评估需要将年龄依赖的tveg纳入陆地表面模型.
- 结果为森林管理提供了洞察力,通过优化位动态来增强碳保留和封存.
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