永久土的融化加速了旧土壤的碳释放,在13年的原变暖实验中超过了新植物投入
Emma Lathrop1,2, Craig See3, Xanthe Walker1,2,4
1Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, Arizona, USA.
Global change biology
|December 8, 2025
概括
北极地区的变暖导致土壤有机碳大量从古老的永久土中消失. 这种古老的碳易于分解,加速气候变化,但灌木扩张可能会提供一些缓解.
科学领域:
- 地球科学 地球科学 地球科学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 永久土土壤储存了大量的古代土壤有机碳 (SOC).
- 北极的变暖可能会导致这种SOC的分解,加速全球气候变化.
- 测量SOC在永久土解中的损失是具有挑战性的,因为沉降.
研究的目的:
- 直接测量SOC库存和放射性碳在永久土融化期间的变化.
- 在SOC损失估计中考虑沉降.
- 了解全球变暖对深层土壤碳池的影响.
主要方法:
- 在阿拉斯加内陆进行了为期13年的永久土融化实验.
- 直接测量的SOC库存和土壤散装放射性碳 (14C) 变化.
- 在测量过程中考虑了土地沉降.
主要成果:
- 观察到显著的SOC库存下降:14%在环境中和23%在温暖的地块.
- SOC损失主要发生在深层矿物土壤层中.
- 冬季土壤变暖是SOC损失的关键驱动因素,由水分和植被介导.
结论:
- 解永久土释放古老的,深层土壤有机碳进入全球碳循环.
- 更温暖的冬季土壤加快了SOC的损失,突出了这些碳储存的脆弱性.
- 增加灌木生物质可能会减轻深层土壤中的SOC损失.
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