Molecular transformations of heteroatomic organic compounds in crude oils caused by biodegradation and subsequent thermal maturation: Insights from ESI FT-ICR MS

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Organic Geochemistry Pub Date : 2024-01-20 DOI:10.1016/j.orggeochem.2024.104741
Bin Jiang , Weimin Liu , Yuhong Liao , Ping'an Peng
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Abstract

The Tarim and Junggar basins are major petroliferous sedimentary deposits in China. Some oil reservoirs in these basins experienced superimposed secondary alterations including early biodegradation followed by thermal maturation/alteration (SSA-B&M). Heteroatomic polar organic compounds in crude oil are significantly influenced by SSA-B&M, which play a vital role in understanding the evolutionary history of oil reservoir. However, research on such alterations is limited. The present study employed negative and positive ion electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry (ESI FT-ICR MS) to investigate the molecular transformations of heteroatomic organic compounds in crude oils resulting from SSA-B&M. The findings indicate that biodegradation leads to an enrichment of naphthenic acids, while subsequent cyclization, aromatization and thermal cracking reactions enhances the aromaticity of the pyrolysis products of all the oil samples with varying degree of biodegradation. Notably, highest aromaticity was observed for the crude oil that has been most severely altered by biodegradation. During early and moderate stages of biodegradation, the abundances of O2 compounds (molecules contain two oxygen atoms) representing carboxylic acids were continuously increasing. However, at severe biodegradation levels, fatty acids with 1 double bond equivalents (DBE) underwent degradation, while the naphthenic acids were further enriched. Subsequently, during maturation, O2 compounds with 1 to 5 DBE experienced a steady decline in abundance. The naphthenic acids mainly experienced aromatization, while the fatty acids were partly decarboxylized and cracked thereby forming new n-alkanes. Biodegradation led to modification in neutral nitrogen compounds with 3 to 4 condensed rings (DBE = 9–12) and long alkyl side chains, while the impact on basic nitrogen compounds was relatively minimal. After subsequent thermal maturation, both neutral and basic nitrogen compounds with long alkyl side chains underwent cracking, while those with shorter alkyl side chains and higher degrees of condensation tended to remain relatively unchanged. Finally, two new indices were defined and tested to correctly evaluate the maturation and biodegradation level for crude oils that have experienced SSA-B&M.

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生物降解和随后的热熟化引起的原油中杂原子有机化合物的分子转化:从 ESI FT-ICR MS 中获得的启示
塔里木盆地和准噶尔盆地是中国主要的含油沉积矿床。这些盆地中的一些油藏经历了叠加的二次变化,包括早期生物降解和随后的热成熟/变化(SSA-B&M)。原油中的异原子极性有机化合物受 SSA-B&M 的影响很大,对了解油藏的演化历史起着至关重要的作用。然而,有关这种变化的研究还很有限。本研究采用负离子和正离子电喷雾傅立叶变换离子回旋共振质谱法(ESI FT-ICR MS)研究了 SSA-B&M 导致的原油中杂原子有机化合物的分子转化。研究结果表明,生物降解会导致环烷酸的富集,而随后的环化、芳香化和热裂解反应则会提高生物降解程度不同的所有油样热解产物的芳香度。值得注意的是,受生物降解影响最严重的原油的芳香度最高。在生物降解的早期和中度阶段,代表羧酸的 O2 化合物(分子中含有两个氧原子)的丰度不断增加。然而,在严重生物降解阶段,含有 1 个双键当量(DBE)的脂肪酸发生降解,而环烷酸则进一步富集。随后,在成熟过程中,双键当量为 1 至 5 的 O2 化合物的丰度持续下降。环烷酸主要发生了芳香化,而脂肪酸则部分发生了脱羧和裂解,从而形成了新的正构烷烃。生物降解导致具有 3 至 4 个缩合环(DBE = 9-12)和长烷基侧链的中性氮化合物发生变化,而对碱性氮化合物的影响相对较小。在随后的热熟化过程中,具有长烷基侧链的中性氮化合物和碱性氮化合物都发生了裂解,而具有较短烷基侧链和较高缩合度的氮化合物则相对保持不变。最后,我们定义并测试了两个新的指数,以正确评估经历过 SSA-B&M 的原油的熟化和生物降解水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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