永久土融化导致北方泥炭地大量的碳损失,而泥炭质量的变化有限
Lorna I Harris1,2, David Olefeldt1,3, Nicolas Pelletier4
1Department of Renewable Resources, University of Alberta, Edmonton, Alberta, Canada.
Global change biology
|August 11, 2023
概括
在泥炭地上的永久土融化会导致显著的碳损失,超过13%的土壤碳在600年内释放出来. 虽然较深的泥炭质量基本保持不变,但总体碳库存减少,影响气候反循环.
科学领域:
- 环境科学 环境科学
- 地质科学是地球科学.
- 气候科学 气候科学
背景情况:
- 在泥炭地上的永久土融化会将大量的土壤碳释放到大气中.
- 这种碳排放作为气候变化反机制.
- 了解解后的碳动态对于气候建模至关重要.
研究的目的:
- 研究永久土融化对泥炭储存和质量的影响.
- 随着时间的推移,量化碳损失和新的泥炭积累.
- 评估泥炭解后泥炭分解能力的变化.
主要方法:
- 从代表不同解年龄的时间序列中收集了泥炭芯.
- 分析了泥炭碳储存,分解代理 (FTIR,C/N比率) 和通过实验室化进行潜在的分解性.
- 永久土高原和热土沼泽之间的泥炭特性比较.
主要成果:
- 在不到600年的时间里,泥炭碳总量减少了大约13% (~19.3公斤C m-2).
- 据估计,在融化后,深层泥炭中约有19%的碳丢失.
- 没有发现深层泥炭质量或可变性的显著变化,也没有发现矿化率的增加.
结论:
- 加拿大西部泥炭地上的永久土融化导致了相当大的碳净损失.
- 尽管深层泥炭质量发生了有限的变化,但整体碳库存显著下降.
- 需要进行进一步的研究,以阐明导致融化后碳损失的确切机制.
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