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Crude-oil biodegradation via methanogenesis in subsurface petroleum reservoirs

机译:地下石油储层中甲烷生成的原油生物降解

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Biodegradation of crude oil in subsurface petroleum reservoirs has adversely affected the majority of the world's oil, making recovery and refining of that oil more costly. The prevalent occurrence of biodegradation in shallow subsurface petroleum reservoirs has been attributed to aerobic bacterial hydrocarbon degradation stimulated by surface recharge of oxygen-bearing meteoric waters2. This hypothesis is empirically supported by the likelihood of encountering biodegraded oils at higher levels of degradation in reservoirs near the surface. More recent findings, however, suggest that anaerobic degradation processes dominate subsurface sedimentary environments, despite slow reaction kinetics and uncertainty as to the actual degradation pathways occurring in oil reservoirs. Here we use laboratory experiments in microcosms monitoring the hydrocarbon composition of degraded oils and generated gases, together with the carbon isotopic compositions of gas and oil samples taken at wellheads and a Rayleigh isotope fractionation box model, to elucidate the probable mechanisms of hydrocarbon degradation in reservoirs. We find that crude-oil hydrocarbon degradation under methanogenic conditions in the laboratory mimics the characteristic sequential removal of compound classes seen in reservoir-degraded petroleum. The initial preferential removal of n-alkanes generates close to stoichiometric amounts of methane, principally by hydrogenotrophic methanogenesis. Our data imply a common methanogenic biodegradation mechanism in subsurface degraded oil reservoirs, resulting in consistent patterns of hydrocarbon alteration, and the common association of dry gas with severely degraded oils observed worldwide. Energy recovery from oilfields in the form of methane, based on accelerating natural methanogenic biodegradation, may offer a route to economic production of difficult-to-recover energy from oilfields.
机译:地下石油储层中原油的生物降解已对世界上大多数石油造成了不利影响,使该石油​​的开采和精炼成本更高。浅层地下石油储层中生物降解的普遍发生,归因于含氧大气水的表面补给刺激了好氧细菌碳氢化合物的降解2。在地面附近的储层中,在较高的降解水平下遇到生物降解油的可能性从经验上支持了这一假设。然而,最近的发现表明,厌氧降解过程在地下沉积环境中起着主导作用,尽管反应动力学缓慢并且对于油藏中发生的实际降解途径尚不确定。在这里,我们在微观环境中使用实验室实验来监测降解的油和生成的气体的碳氢化合物组成,以及在井口和瑞利同位素分馏箱模型中获得的天然气和油样的碳同位素组成,以阐明储层中碳氢化合物降解的可能机理。 。我们发现,在甲烷化条件下,实验室中的原油碳氢化合物降解模仿了在油藏降解的石油中见到的化合物类别的特征性顺序去除。最初优先去除正构烷烃主要是通过氢营养甲烷化作用而产生接近化学计量的甲烷。我们的数据表明,在地下退化的油藏中存在常见的产甲烷生物降解机制,从而导致烃变化的规律性一致,并且在全球范围内观察到干气与严重退化的油之间的常见关联。以加速自然产甲烷生物降解为基础,以甲烷形式从油田回收能源,可能为经济生产难以回收的能源提供了一条途径。

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