Response model of fluid–rock ratio to reservoir space in primary formation of shale oil during hydrous pyrolysis

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Lina Sun, Deliang Fu, Qi Zhang, Yuandong Wu
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Abstract

ABSTRACT Due to the presence of geological fluid under actual geological conditions, water–rock interaction will occur between the fluid and reservoir. Thus, to analyse the influence of the water–rock interaction on storage space during the organic matter evolution stages, this study conducted a series of simulation experiments on shales by using a closed autoclave: four temperatures, 250°C, 300°C, 350°C, 400°C, and five fluid–rock ratios (FRRs), 0:20, 4:20, 10:20, 15:20, and 20:20. Low pressure N2 adsorption measurement was conducted on the solid residues. The experimental results show that the effect of temperature on the yield and pore structure of oil shale was the same as the result when the FRR was = 0:20, 4:20 and = 10:20, 15:20, 20:20, respectively. This result showed that temperature remained the main factor that affected the thermal evolution of hydrocarbon generation. Additionally, temperature was beneficial to the generation and storage of shale oil within a certain range, but only occupied the storage space of shale oils or connected a certain storage space beyond a certain range. The variation trend of shale oil yield with increasing FRR under the same simulated temperatures, 250°C and 400°C, was most affected by the FRR, but little change occurred at 300°C and 350°C. This further proved that the ratio of fluid to rock was an indirect acting factor, which affected the evolution of organic matters and then the development of pore structures. Before the oil window (350°C), the lower evolution degree, the higher water content and the more significant effect. In the higher evolution stage, the higher the water content, and the more complete the kerogen reaction, which was also more conducive to the development of pore structures. Therefore, this study promotes the establishment of linear equations on FRR to the gas adsorption capacity, which further provides a theoretical basis and guidance for the exploration and development of shale oil.
页岩油初生层含水热解流岩比与储层空间响应模型
摘要在实际地质条件下,由于地质流体的存在,流体与储层之间会发生水-岩相互作用。因此,为了分析有机质演化阶段水-岩石相互作用对储存空间的影响,本研究使用封闭高压釜对页岩进行了一系列模拟实验:四个温度,250°C、300°C、350°C、400°C和五个流体-岩石比(FRR),0:20、4:20、10:20、15:20和20:20。对固体残留物进行低压N2吸附测量。实验结果表明,温度对油页岩产量和孔隙结构的影响与FRR分别为0:20、4:20和=10:20、15:20、20:20时的结果相同。这一结果表明,温度仍然是影响生烃热演化的主要因素。此外,温度在一定范围内有利于页岩油的生成和储存,但只占用了页岩油的储存空间或在一定范围外连接了一定的储存空间。在相同的模拟温度(250°C和400°C)下,页岩油产量随FRR的增加而变化的趋势受FRR的影响最大,但在300°C和350°C时变化不大。这进一步证明了流体与岩石的比例是一个间接作用因素,它影响有机质的演化,进而影响孔隙结构的发展。在油窗(350°C)之前,演化程度越低,含水量越高,影响越显著。在较高的演化阶段,含水量越高,干酪根反应越完全,也更有利于孔隙结构的发育。因此,本研究促进了FRR对天然气吸附能力线性方程的建立,进一步为页岩油勘探开发提供了理论依据和指导。
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来源期刊
CiteScore
2.00
自引率
0.00%
发文量
21
期刊介绍: Earth and Environmental Science Transactions (formerly Transactions of the Royal Society of Edinburgh: Earth Sciences) is a general earth sciences journal publishing a comprehensive selection of substantial peer-reviewed research papers, reviews and short communications of international standard across the broad spectrum of the Earth and its surface environments. The journal prides itself on the quality of its graphics and photographic reproduction. The Editors are keen to encourage interdisciplinary papers and Transactions also publishes occasional special symposia and invited volumes of specific interest. We are currently in the process of digitising the archive of RSE Publications, and the archive of the Transactions, dating back to 1788, will be available from the back issues link on this site.
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