在二氧化碳水平增加的情况下,通过热层臭氧减少土壤碳形成
Wendy M Loya1, Kurt S Pregitzer, Noah J Karberg
1School of Forest Resources and Environmental Science, Michigan Technological University, Houghton, Michigan 49931, USA. wmloya@mtu.edu
Nature
|October 17, 2003
概括
升高的热层臭氧显著减少了土壤碳的形成,即使增加了二氧化碳. 这一发现影响了对森林生产力和碳循环在气候变化中的理解.
科学领域:
- 环境科学 环境科学
- 森林生态 森林生态
- 生物地质化学生物地质化学
背景情况:
- 过去一个世纪以来,北半球的热带臭氧增加了35%,对森林和农业生产率产生了负面影响.
- 升高的臭氧可能会通过影响土壤碳输入量和质量来改变陆地碳循环.
- 增加臭氧对土壤碳的形成和分解的具体影响仍然在很大程度上是未知的.
研究的目的:
- 为了研究升高的臭氧对土壤碳形成速度的影响.
- 评估在高臭氧和二氧化碳下形成的总和耐腐蚀的酸不溶性土壤碳.
主要方法:
- 使用了实验性树 (Populus tremuloides) 和混合树-白树 (Betula papyrifera) 的种群.
- 大气中的臭氧和二氧化碳度增加了50%.
- 在这些条件下测量了土壤碳形成率.
主要成果:
- 升高的臭氧,加上升高的二氧化碳,将土壤总碳形成率降低了50%.
- 在这些条件下,酸不溶土壤碳的形成率也下降了50%.
- 这些减少与仅暴露于二氧化碳升高的森林相对而言.
结论:
- 升高的臭氧会显著降低土壤碳形成率,即使在二氧化碳升高的条件下.
- 这表明,臭氧水平上升将使全球土壤碳封存减少.
- 减少土壤碳形成对陆地碳循环和气候变化缓解具有关键意义.
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