酸雨减少了土壤的碳排放,增加了土壤呼吸的温度灵敏度:一个全面的元分析
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Updated: Jul 1, 2025

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Simulating Temperature in a Soil Incubation Experiment
Published on: October 28, 2022
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Weichao Liu1, Jingbo Fang1, Yaoyue Liang1
1College of Agronomy, Northwest A&F University, Yangling 712100, Shaanxi, China; The Research Center of Recycle Agricultural Engineering and Technology of Shaanxi Province, China.
The Science of the total environment
|March 4, 2024
概括
酸雨 (AR) 显著降低了土壤呼吸和微生物生物质,同时增加了土壤呼吸.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
背景情况:
- 土壤呼吸是陆地生态系统中主要的碳流.
- 酸雨 (AR) 对土壤呼吸的影响尚不清楚.
- 了解AR的影响对于预测气候变化下的碳循环至关重要.
研究的目的:
- 进行一项元分析,评估AR对土壤呼吸成分和温度灵敏度 (Q10) 的影响.
- 研究H+输入,AR持续时间,气候和土壤特性等因素如何调节这些反应.
主要方法:
- 来自48项研究的318个土壤呼吸和263个Q10数据点的元分析.
- 统计分析以确定AR对土壤呼吸率 (Rt,Ra,Rh) 和它们的Q10值的影响.
- 检查AR反应与环境变量之间的相关性.
主要成果:
- 通过AR降低了7.41%的总土壤呼吸 (Rt) 和20.75%的自营呼吸 (Ra).
- AR增加了Rt的Q10和异质呼吸 (Rh),但降低了Ra-Q10.
- 土壤酸化,根和微生物生物量减少,微生物群落改变与AR效应有关.
结论:
- AR对土壤呼吸率产生负面影响,并改变其温度灵敏度.
- 这些影响是由土壤酸化,生物质变化,微生物群落转移和环境因素介导的.
- 这项研究提供了AR对土壤呼吸的复杂影响的大规模综合,这对气候变化研究至关重要.
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