大气中二氧化碳的上升减少了根源来源的土壤碳的封存
James Heath1, Edward Ayres, Malcolm Possell
1Department of Biological Sciences, Institute of Environmental and Natural Sciences, Lancaster University, Bailrigg, Lancaster, LA1 4YQ, UK. j.heath@lancaster.ac.uk
概括
森林作为碳吸收器的作用可能会因二氧化碳的丰富而减少. 观察到土壤呼吸的增加和根部碳捕获的减少,可能加速气候变化.
科学领域:
- 森林生态森林生态学
- 气候变化科学 气候变化科学
- 土壤科学 土壤科学
背景情况:
- 森林作为关键的碳汇,在缓解大气二氧化碳水平上升和气候变化方面发挥着至关重要的作用.
- 了解大气中二氧化碳增加对森林碳捕获的影响对于准确的气候建模至关重要.
研究的目的:
- 调查二氧化碳增加对欧洲树种生长和土壤碳动态的影响.
- 评估这些变化对陆地碳汇容量的潜在影响.
主要方法:
- 有控制的实验使欧洲的各种树种暴露在富含二氧化碳的大气中.
- 测量树木生长刺激和土壤微生物呼吸率.
- 在土壤中量化根源衍生的碳封存.
主要成果:
- 在二氧化碳丰富下,在欧洲树种中观察到短期增长刺激.
- 检测到土壤微生物呼吸的显著增加.
- 在土壤中观察到根源衍生碳的封存显著下降.
结论:
- 升高的二氧化碳水平可能会对陆地碳汇的有效性产生负面影响.
- 增加土壤呼吸和减少碳封存可能会导致一个积极的反循环,加速大气二氧化碳的上升.
- 森林生态系统在未来大气条件下,可能对减缓气候变化的能力有所减弱.
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