地下深处的生物活动和重油的起源
Ian M Head1, D Martin Jones, Steve R Larter
1NRG petroleum group, School of Civil Engineering and Geosciences, University of Newcastle upon Tyne, Newcastle, NE1 7RU, UK.
Nature
|November 25, 2003
概括
微生物将石油碳化合物降解为高达80°C的重油,这可能标志着地球深层生命的极限. 这个过程经常产生甲,这表明重油回收的新方法.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 石油科学 石油科学 石油科学
背景情况:
- 地下石油储库在高达80°C的温度下受到微生物的生物降解.
- 这种生物过程在地质时间内将碳化合物转化为更密集的重油.
研究的目的:
- 为了研究碳化合物的生物降解在地下环境的温度值.
- 探索这种生物降解极限对深层微生物生命的搜索的影响.
- 考虑重型石油回收的替代策略.
主要方法:
- 在地底储库中分析石油成分.
- 对生物降解过程的地质时间尺度评估.
- 在不同温度和营养条件下的微生物活动研究.
主要成果:
- 碳化合物的生物降解在大约80°C时是显著的.
- 这种温度可能代表了微生物生命在地球深处,营养缺乏的环境中的边界.
- 无氧生物降解通常产生甲作为主要的副产品.
结论:
- 生物降解的80°C值对理解深层生物圈极限有影响.
- 生物降解过程中的甲生产为增强重油回收战略提供了潜力.
- 巨大的重油资源可以通过生物降解过程的替代回收方法获得.
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