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经过9年的夏季试验变暖和增加雪深度后,土壤和植物碳池的变化
Lena Hermesdorf1, Louise H Mortensen1, Sophia B Blitz1
1Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen, Denmark.
The Science of the total environment
|August 21, 2024
概括
气候变暖增加了原土壤的碳,而增加的雪深减少了它. 这些对抗碳池的影响是由植物反应驱动的,特别是Betula nana,在树枝球土壤中最为明显.
科学领域:
- 北极生态学 北极生态学
- 气候变化影响气候变化的影响.
- 土壤科学 土壤科学
背景情况:
- 北极生态系统对气候变化敏感,对土壤和植物碳池的影响不确定.
- 了解这些影响对于预测全球碳预算至关重要.
研究的目的:
- 调查增加的雪深和夏季变暖对原土壤的影响,并在格陵兰西部种植碳池.
- 评估植物物种特异性反应及其对地下碳动态的级联影响.
主要方法:
- 应用了9年的实验性加雪 (雪) 和夏季加热 (开放的顶部室).
- 分析了土壤样本 (包括树根球),植被 (NDVI,覆盖,生物质) 和卫星图像.
主要成果:
- 夏季的变暖显著增加了Betula nana的生长和的生物量,导致土壤有机碳在顶部20厘米的增加,特别是在树叶球土壤中.
- 仅仅雪深增加对Betula nana产生了负面影响,并且没有显示出地下影响.
- 加热和加雪具有相反的效果,在联合治疗中没有观察到相互作用效应.
结论:
- 植物反应,特别是Betula nana,调解气候变化对原碳池的影响.
- 树叶球土壤是处理对土壤碳的影响的关键指标.
- 单独的变暖和增加雪的处理对生态系统的碳产生了截然不同的影响,突出了北极气候变化反应的复杂性.
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