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气候变暖减少了温带森林中的土壤气损失
Kai Huang1,2,3, Di Wu1,3, Dongwei Liu1,3,4
1Chinese Academy of Sciences Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China.
概括
全球变暖出乎意料地减少了温带森林中的土壤氧化 (NO) 和氧化 (N2O) 排放量. 暖化引起的土壤干燥,而不是增加的转化,导致了这些较低的温室气体排放.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 土壤科学 土壤科学
背景情况:
- 全球变暖预计将通过气体通道增加生态系统的气损失.
- 目前预测气损失的模型依赖于不确定的实验室实验,局部验证有限.
- 的可用性对于初级生产率和碳捕获至关重要.
研究的目的:
- 调查温暖化对温带森林土壤气态气排放的现场影响.
- 挑战现有的生态系统模型关于变暖和气损失的假设.
- 为了确定在变暖条件下观察到的气排放变化背后的机制.
主要方法:
- 进行了为期6年的实地实验,该实验涉及将温带森林升温2°C.
- 测量了超过20万个土壤氧化 (NO) 和氧化 (N2O) 流量.
- 使用升级方法来估计 (N2) 流量.
主要成果:
- 变暖显著降低了19%的土壤NO和16%的N2O排放量.
- 这些减少归因于由变暖引起的土壤干燥,这限制了微生物活动.
- 观察到的变化并不能通过增加转化为N2,浸或植物吸收来解释.
结论:
- 这些发现挑战了仅仅是变暖加快了生态系统气排放的假设.
- 暖化引起的土壤水分损失和改变的冷解周期可以抵消温度对循环的影响.
- 在现场的土壤湿度动态对于准确预测陆地循环对全球变暖的反应至关重要.
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