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在深水地平线石油泄漏期间,释放到水柱中的气体和油的组成和命运。

Composition and fate of gas and oil released to the water column during the Deepwater Horizon oil spill.

机构信息

Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.

出版信息

Proc Natl Acad Sci U S A. 2012 Dec 11;109(50):20229-34. doi: 10.1073/pnas.1101242108. Epub 2011 Jul 18.

Abstract

Quantitative information regarding the endmember composition of the gas and oil that flowed from the Macondo well during the Deepwater Horizon oil spill is essential for determining the oil flow rate, total oil volume released, and trajectories and fates of hydrocarbon components in the marine environment. Using isobaric gas-tight samplers, we collected discrete samples directly above the Macondo well on June 21, 2010, and analyzed the gas and oil. We found that the fluids flowing from the Macondo well had a gas-to-oil ratio of 1,600 standard cubic feet per petroleum barrel. Based on the measured endmember gas-to-oil ratio and the Federally estimated net liquid oil release of 4.1 million barrels, the total amount of C(1)-C(5) hydrocarbons released to the water column was 1.7 10(11) g. The endmember gas and oil compositions then enabled us to study the fractionation of petroleum hydrocarbons in discrete water samples collected in June 2010 within a southwest trending hydrocarbon-enriched plume of neutrally buoyant water at a water depth of 1,100 m. The most abundant petroleum hydrocarbons larger than C(1)-C(5) were benzene, toluene, ethylbenzene, and total xylenes at concentrations up to 78 μg L(-1). Comparison of the endmember gas and oil composition with the composition of water column samples showed that the plume was preferentially enriched with water-soluble components, indicating that aqueous dissolution played a major role in plume formation, whereas the fates of relatively insoluble petroleum components were initially controlled by other processes.

摘要

定量的有关天然气和石油组成成分的信息,这些油和气是从深海地平线(Deepwater Horizon)油井泄漏事件中的马孔多(Macondo)油井中流出的,这些信息对于确定石油流速、释放的总油量以及海洋环境中碳氢化合物成分的轨迹和命运是至关重要的。我们使用等压密封采样器,于 2010 年 6 月 21 日直接在马孔多油井上方采集了离散样本,并对天然气和石油进行了分析。我们发现,从马孔多油井中流出的流体的气油比为 1600 标准立方英尺每石油桶。根据测量得到的端元气油比和联邦估计的 410 万桶净液态油释放量,释放到水柱中的 C(1)-C(5)碳氢化合物总量为 1.710(11)g。端元气和油的组成使我们能够研究 2010 年 6 月在水深 1100 米处的中性浮力富含碳氢化合物的西南趋势羽流中采集的离散水样中石油碳氢化合物的分馏作用。丰度最高的大于 C(1)-C(5)的石油碳氢化合物是苯、甲苯、乙苯和总二甲苯,浓度高达 78μg/L。将端元气和油的组成与水柱样品的组成进行比较表明,羽流优先富集水溶性成分,这表明水的溶解在羽流形成中起主要作用,而相对不溶性石油成分的命运最初受其他过程控制。

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