对两种模型化合物的热化学硫酸盐还原产物的定量分析:对碳氢化合物反应机理和改变过程的启示

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Chemical Geology Pub Date : 2024-05-24 DOI:10.1016/j.chemgeo.2024.122187
Zhenyu Sun , Jian Chen , Qiang Wang , Wanglu Jia , Ping'an Peng
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引用次数: 0

摘要

热化学硫酸盐还原(TSR)是一种重要的氧化还原反应,可显著改变深层储层中的碳氢化合物。虽然近 50 年来在反应机理、过程和地球化学特征等方面取得了重大成就,但包括主要产物在内的 TSR 定量模型尚未建立,这限制了对 TSR 反应机理和碳氢化合物生成过程的了解。本研究对正十八烷(n-C18)和正十二烷基苯(C12B)在密闭金管体系中与 MgSO4 和 H2O 的 TSR 进行了两组热模拟实验,并定量分析了不同相中的所有主要产物,尤其是含氧化合物。结果表明,重质产物中的高分子量含氧化合物以酮类为主,其次是醇类和酸类;水中的低分子量有机酸以乙酸为主,其次是甲酸和丙酸。这两种含氧化合物都促进了 TSR 过程,但方式不同。高分子量含氧化合物在非自动催化阶段的积累对于启动 TSR 催化反应至关重要。此外,碳氢化合物中的含氧化合物可增强极性,使碳氢化合物更容易与 HSO4- 或 [MgSO4] CIP 接触。低分子量有机酸可能通过酸化水而促进 TSR 过程,从而促进 HSO4- 和 [MgSO4] CIP 的形成。TSR 过程中的氧化反应可能将 HMW 含氧化合物转化为 LMW 有机酸和 CO2。对 TSR 中产物的定量分析显示,TSR 对碳氢化合物的破坏速度更快,但破坏方式与热裂解不同,TSR 中碳氢化合物类型的生成过程依次为:重烃、气态烃/轻烃/固体沥青、气态烃/固体沥青。与石油裂解相比,TSR 能促进油藏快速进入更成熟的阶段。碳氢化合物前驱体和反应程度影响了 TSR 的生成过程和所有产物的特性。这些结果有助于加深对 TSR 机理和过程的理解,并有助于评估 TSR 改质油的石油潜力。
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A quantitative analysis on thermochemical sulfate reduction products of two model compounds: Implications for reaction mechanism and alteration process of hydrocarbons

Thermochemical sulfate reduction (TSR) is an important redox reaction that markedly alters hydrocarbons in deep reservoirs. Although the major achievements that involve reaction mechanism, process, and geochemical characteristics were attained in the last 50 years, a quantitative TSR model that includes major products was not built, which restricts the understanding of the reaction mechanism and the generation process of hydrocarbons in TSR. In this study, two series of thermal simulation experiments of the TSR involving n-octadecane (n-C18) and n-dodecylbenzene (C12B) with MgSO4 and H2O in a confined gold-tube system were conducted, and all the major products in different phases, particularly oxygen-containing compounds, were quantitatively analyzed. The results indicated that the high-molecular-weight (HMW) oxygenated compounds in heavy products were predominated by ketones, followed by alcohol and acids, and the low-molecular-weight (LMW) organic acids in water mainly comprised acetic acids, followed by formic acid and propionic acid. Both oxygen-containing compounds prompted the TSR process but in different ways. The accumulation of HMW oxygenated compounds in the non-autocatalytic stages was essential for initiating the catalyzed reaction of TSR. In addition, the oxygenated compounds of hydrocarbons enhance polarity, making hydrocarbons easier to contact with HSO4 or [MgSO4] CIP. The LMW organic acids possibly prompted the TSR process by acidifying the water and thus facilitating the formation of HSO4 and [MgSO4] CIP. The oxidation reaction during TSR possibly converted HMW oxygenated compounds to LMW organic acids and CO2. The quantitative analysis of products in TSR revealed that TSR destroyed the hydrocarbons more rapidly but in a different way from thermal cracking and that the generation process of hydrocarbon types in TSR was in the following order: heavy hydrocarbon, gaseous hydrocarbon/light hydrocarbon/solid bitumen, and gaseous hydrocarbon/solid bitumen. Compared with oil cracking, the TSR promoted the oil reservoir to rapidly progress to more mature stages. The hydrocarbon precursor and reaction extent affected the generation process and the character of all products in the TSR. These results can provide an improved understanding of the TSR mechanism and process and be useful in the evaluation of petroleum potential for TSR-altered oils.

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来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
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