在地球表面环境中广泛分布的岩石源的融合证据
B Z Houlton1, S L Morford2,3, R A Dahlgren2
1Department of Land, Air and Water Resources, University of California, Davis, CA, USA. bzhoulton@ucdavis.edu.
概括
床岩是陆地生态系统的重要,以前未知的源,与大气输入相美. 这种地质极大地影响了地球的预算和地球的碳汇.
科学领域:
- 地质化学
- 生物地质化学
- 生态学
背景情况:
- 的可用性极大地影响了陆地碳捕获和全球气候变化.
- 传统的理解认为大气沉积是陆地生态系统的主要输入.
研究的目的:
- 探讨岩基作为陆地生态系统的潜在源.
- 从岩石中调动的对全球预算的贡献量化.
- 评估对理解陆地碳汇和气候变化的影响.
主要方法:
- 全球平衡的分析.
- 对地化学代理物的检查.
- 空间气候模型的开发和应用.
主要成果:
- 每年从地表附近的岩石中移动大约19到31千克的.
- 这种动员的11到18特拉克在现场经过化学化.
- 这种地质投入将未经管理的陆地余增加8%至26%.
结论:
- 床岩是陆地生态系统的主要源,与大气输入相当.
- 这一发现需要对全球预算进行修订.
- 了解基岩动员对于预测陆地碳汇的营养驱动控制至关重要.
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