陆地植物在有氧条件下的甲排放
Frank Keppler1, John T G Hamilton, Marc Brass
1Max-Planck-Institut für Kernphysik, Saupfercheckweg 1, 69117 Heidelberg, Germany. frank.keppler@mpi-hd.mpg.de
Nature
|January 13, 2006
概括
科学家们发现,即使在富含氧气的环境中,活植物也会产生甲,这是一种强大的温室气体. 这种以前未知的植物性甲来源可能会对全球甲预算和气候变化模型产生重大影响.
科学领域:
- 环境科学 环境科学
- 生物地质化学生物地质化学
- 植物生理学 植物生理学
背景情况:
- 自工业化前以来,大气中的甲度几乎翻了三倍,对气候产生了重大影响.
- 甲是影响大气化学,平流层臭氧和水蒸气的关键温室气体.
- 自然甲来源主要归因于无毒环境中的生物过程.
研究的目的:
- 为了研究陆地植物中新型,未被识别的甲形成过程.
- 在有氧条件下量化活植物和植物垃圾的甲排放量.
- 评估这种新甲来源对全球甲预算的影响.
主要方法:
- 利用稳定的碳同位素分析来确定甲形成途径.
- 进行实验室和田间化实验,使用完整的植物和脱落的叶子.
- 缩小观察到的甲排放量,以估计全球源强度.
主要成果:
- 证明陆地植物在有氧条件下容易在现场形成甲.
- 从完整的植物和脱落的叶子中观察到大量的甲排放.
- 估计全球甲源强度为 62-236 Tg yr ((-1) 来自活植物和 1-7 Tg yr ((-1) 来自植物垃圾.
结论:
- 确定了以前未知的生物甲来源,源自活植物.
- 这种以植物为基础的甲生产对全球甲预算有重大影响.
- 这些发现需要重新考虑天然甲来源及其在过去气候变化中的作用.
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