在快速侵蚀的热带山地土壤中微生物氧化岩层有机碳
Jordon D Hemingway1,2, Robert G Hilton3, Niels Hovius4,5
1Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution (WHOI), 266 Woods Hole Road, Woods Hole, MA 02543, USA. jordon_hemingway@fas.harvard.edu.
概括
在台湾的石油有机碳 (OCpetro) 氧化
科学领域:
- 地质化学
- 地形学
- 生物地质化学
背景情况:
- 在山地侵蚀过程中,石化有机碳 (OCpetro) 的氧化会释放二氧化碳.
- 在景观中控制石油氧化率的机制尚不清楚.
研究的目的:
- 量化台湾中部地区的石油氧化和二氧化碳排放.
- 在山地土壤中对OCpetro重矿化的控制进行调查.
主要方法:
- 在土壤中分析大量的OC和脂质生物标志物.
- 测量OCpetro含量和同位素组成
- 基于氧化率的二氧化碳排放流量的估计.
主要成果:
- 平均67%的石油在土壤中被氧化.
- 二氧化碳排放量在6.1至18.6公C/km2/年之间.
- 微生物活动调解OCpetro的重矿化.
结论:
- 山地土壤中的快速氧化是大气二氧化碳的重要来源.
- 二氧化碳排放量随着侵蚀速度的增加而增加,
- 在这些系统中,微生物重矿化是OCpetro氧化的主要驱动因素.
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