老生长森林可以在土壤中积累碳
Guoyi Zhou1, Shuguang Liu, Zhian Li
1South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 510650, China. gyzhou@scib.ac.cn
概括
旧生长的森林是重要的碳汇,在其土壤中积累大气中的碳. 这一发现挑战了传统观点,并提出了森林碳循环的动态,不平衡模型.
科学领域:
- 生态生态学 生态生态学
- 森林科学 森林科学 森林科学
- 土壤科学 土壤科学
- 气候变化研究 气候变化研究
背景情况:
- 旧生长的森林传统上被认为是碳中和的,因为碳吸收和呼吸的平衡.
- 主流的生态系统生态模型没有考虑到旧生长森林土壤中大量的碳封存.
研究的目的:
- 调查老生长森林作为碳汇的作用.
- 挑战这些生态系统中碳预算的既定理解.
- 提出研究土壤碳动态的新框架.
主要方法:
- 在中国南部的老生长森林中分析了土壤碳积累率.
- 从1979年到2003年收集长期数据.
- 在顶部20厘米的土壤层中测量碳封存.
主要成果:
- 旧生长的森林每年以每公0.61兆克的平均速度积累大气中的碳.
- 在上层土壤层中观察到显著的碳封存.
- 有证据表明,改变地下碳循环过程是为了应对环境变化.
结论:
- 旧生长的森林作为大量的碳汇,与之前的假设相反.
- 这项研究支持一种非平衡概念框架,用于理解土壤碳动态.
- 森林碳循环过程,特别是在地下,正在适应环境变化.
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