在土壤中的有机物分解和全球变暖的后果
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Updated: Sep 9, 2025

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Simulating Temperature in a Soil Incubation Experiment
Published on: October 28, 2022
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Ekaterina Filimonenko1,2, Yakov Kuzyakov3,4
1National Key Laboratory of Wheat Improvement, College of Agronomy, Shandong Agricultural University, Tai'an, Shandong, China.
Global change biology
|September 4, 2025
概括
激活能量 (Ea) 决定了土壤有机物 (SOM) 的转化速率. 酶显著降低了Ea,加速了分解和营养循环,这对全球变暖对碳和营养循环的影响有影响.
科学领域:
- 土壤科学
- 生物地质化学
- 化学动力学
背景情况:
- 激活能量 (Ea) 对于确定生物化学反应的速率至关重要,包括土壤有机物 (SOM) 的转化.
- 了解Ea对于预测土壤过程如何应对全球变暖等环境变化至关重要.
研究的目的:
- 评估各种土壤有机物 (SOM) 转化过程的激活能量 (Ea).
- 为了比较化学氧化,微生物矿化和酶催化反应的Ea值.
- 评估Ea对全球变暖下的SOM稳定性和营养循环的影响.
主要方法:
- 使用来自氧化和水解酶活动,SOM矿化 (CO2产生) 和热氧化的Ea值数据库.
- 应用Arrhenius方程来计算不同SOM转换路径的Ea.
- 在化学,微生物和酶分解过程中比较Ea值.
主要成果:
- SOM 的化学氧化具有高的 Ea (79 kJ mol-1).
- 微生物矿化 (67 kJ mol-1) 和分解 (40 kJ mol-1) 的Ea值较低.
- 酶催化水解呈现最低的 Ea (33 kJ mol-1),明显比化学氧化更快.
- 矿物离子 (N,P,S) 的酶分裂比聚合物水解快40倍.
- 由于酶催化和保护,土壤中的微生物矿化速度比纯化学氧化快140倍.
结论:
- 与化学氧化相比,酶催化大大降低了SOM分解的激活能量.
- 较高的Ea过程对温度增加更为敏感,这表明在全球变暖下SOM分解加速.
- 全球变暖可能会增加碳循环, 而不是营养循环,
- 可以通过激活能量值来评估SOM的稳定性及其对气候变化的反应.
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