添加对土壤碳的稳定性和循环的变量影响
Jason C Neff1, Alan R Townsend, Gerd Gleixner
1Earth Surface Processes Team, Geologic Division, US Geological Survey, MS 980, Denver Federal Center, Denver, Colorado 80225, USA. jneff@usgs.gov
Nature
|November 1, 2002
概括
化肥加快了土壤碳分解的轻微分数,但稳定了较重的分数. 大量土壤碳保持不变,表明当前土壤碳模型的局限性.
科学领域:
- 土壤科学 土壤科学
- 生物地质化学生物地质化学
- 环境科学环境科学
背景情况:
- 土壤储存大量的陆地碳,这对于了解全球碳循环至关重要.
- 已知气候对土壤碳分解的影响,但的作用尚不确定.
- 在全球范围内,反应性的增加来自农业和化石燃料.
研究的目的:
- 研究化肥对土壤碳动态的影响.
- 分析不同土壤碳池对添加的反应.
主要方法:
- 使用了14C,13C和特定化合物的分析.
- 从长期化肥场进行土壤碳检查.
主要成果:
- 添加气加速了土壤轻碳分量的分解 (十年周转).
- 添加稳定了与矿物相关的土壤碳分数 (数十年到一个世纪的寿命).
- 没有观察到土壤散装碳的显著变化.
结论:
- 目前的单池模型不足以评估土壤对环境变化的碳反应.
- 的可用性对土壤碳储存有复杂的影响.
- 需要进一步的研究来比较高肥料添加量与长期大气沉积效应.
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