增加地下碳分配减少了长期变暖下的土壤碳损失
Andreas Schindlbacher1, Steve Kwatcho Kengdo2,3, Jakob Heinzle1
1Department of Forest Ecology and Soils, Federal Research and Training Centre for Forests, Natural Hazards and Landscape-BFW, Vienna, Austria.
Global change biology
|October 17, 2025
概括
全球变暖增加了森林土壤的二氧化碳 (CO2) 排放量,但根部活动增加可能会补充土壤有机碳 (SOC). 这表明森林碳循环对气温上升的复杂反应.
科学领域:
- 森林生态森林生态学
- 土壤科学 土壤科学
- 气候变化科学 气候变化科学
背景情况:
- 森林土壤储存了大量的土壤有机碳 (SOC).
- 全球变暖可能会加速SOC矿化,释放二氧化碳并产生积极的气候反.
- 阿尔卑斯山森林特别容易受到变暖的影响,原因是温度增加.
研究的目的:
- 研究实验性土壤变暖对森林土壤二氧化碳排放和SOC动态的长期影响.
- 在变暖条件下确定土壤二氧化碳排放变化的主要驱动因素.
主要方法:
- 18年来,北方石灰岩阿尔卑斯山山林中的实验性土壤变暖 (+4°C).
- 测量土壤二氧化碳排放和土壤有机碳 (SOC) 库存.
- 分析SOC的放射性碳年龄和根呼吸/生产.
主要成果:
- 土壤变暖显著和持续地增加了土壤二氧化碳排放 (每1°C约13%).
- SOC库存显示不显著下降,低于建议的排放量.
- 增加根呼吸是二氧化碳排放量增加的主要驱动因素.
- 增加的根产量和营业额可能补充了SOC.
结论:
- 长期的土壤变暖增加了森林土壤的二氧化碳排放量.
- 增加对根系球的碳分配可能部分抵消SOC矿化造成的碳损失.
- 森林对变暖的反应可能比以前认为的要复杂得多.
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