频繁的干旱减少了有机矿物土壤中的碳稳定
Fabrizio Albanito1, Sabine Reinsch1, Mark Richards2
1UK Centre for Ecology & Hydrology, Bangor, UK.
Global change biology
|January 6, 2026
概括
经常出现的干旱会减少土壤有机碳 (SOC) 池,并降低碳捕集效率 (CSE). 干旱的频率,而不是持续时间,是影响有机矿物土壤土壤碳稳定性的主要因素.
科学领域:
- 土壤科学 土壤科学
- 生物地质化学生物地质化学
- 气候变化影响气候变化的影响.
背景情况:
- 气候变化正在增加干旱的频率,影响土壤的碳汇.
- 经常性干旱对土壤有机物分解和碳排放的长期影响尚不清楚.
研究的目的:
- 为了模拟长期干旱对土壤有机碳 (SOC) 封存和稳定的影响.
- 开发新的指标来评估 SOC 在反复干旱场景下的变化.
- 确定控制土壤碳稳定性的主要因素 (频率与持续时间).
主要方法:
- 使用ECOSSE生物地球化学模型进行模拟.
- 在温带高原生态系统中模拟长期干旱事件.
- 开发和应用新的指标:碳捕获效率 (CSE) 和稳定效率 (SE).
主要成果:
- 经常出现的干旱导致微生物 (BIO) 和软化 (HUM) SOC池的数量减少.
- 干旱改变了不稳定和稳定池的碳利用效率 (CUE).
- 碳捕获效率 (CSE) 下降了高达15%,稳定效率 (SE) 下降到40%.
结论:
- 经常出现的干旱重塑了SOC的动态,减少了CSE并改变了分解稳定平衡.
- 干旱频率是有机矿物土壤中土壤长期碳稳定的主要驱动因素.
- 在干旱后,分解和稳定之间持续的脱发生.
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