在深层地下油库中无氧碳化合物的生物降解
Carolyn M Aitken1, D M Jones, S R Larter
1School of Civil Engineering and Geosciences, University of Newcastle upon Tyne NE1 7RU, UK.
Nature
|September 17, 2004
概括
无氧碳化合物降解是深层石油储库中常见的过程,挑战了关于石油生物降解需要氧气的先前假设. 这项研究在全球多样化的石油样本中发现了证据.
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:
- 在地下水库中石油的生物降解是一个经济上重要的过程.
- 以前,需要氧气和营养素的有氧降解被认为是主要的机制.
- 由于缺乏直接证据,在深水库中无氧降解的作用一直受到争议.
研究的目的:
- 调查地下石油储库中无氧碳化合物降解的普遍性.
- 提供证据支持或反驳深层油库中无氧生物降解的重要性.
主要方法:
- 在全球范围内分析了77个生物降解的原油样本,这些样本来自各种海洋和湖泊来源.
- 隔离和识别表明无氧碳化合物降解的代谢物.
主要成果:
- 在分析的石油样本中,在很大一部分中发现了暗示无氧碳化合物降解的代谢物.
- 在来自不同地质环境的油中发现了证据,包括加拿大焦油砂.
结论:
- 无氧碳化合物降解是生物降解的地下油库中普遍存在的过程.
- 这一发现对理解石油变化和储备库质量有重大影响.
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