An EPR Study of the Effect of Thermochemical Processes on the Transformations of the Organic Matter and Mineral Matrix of a Bituminous Rock

IF 1.3 4区 工程技术 Q3 CHEMISTRY, ORGANIC Petroleum Chemistry Pub Date : 2024-08-30 DOI:10.1134/s0965544124040078
G. P. Kayukova, N. M. Khasanova, A. N. Mikhailova, Z. R. Nasyrova, A. V. Vakhin
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Abstract

Thermochemical transformations of the organic matter and mineral matrix of the bituminous oil-containing rock from the productive stratum of Permian heavy crude deposits (Ashal’cha oilfield) at 350 and 600°С in a hydrogen medium were studied by electron paramagnetic resonance (EPR) spectroscopy. A rock sample taken from a depth of 117.5–118.5 m was studied before and after hydrothermal treatment at 300°С in the presence of an aqueous phase. Comparison of the EPR spectra shows that, as compared to the initial rock, an increase in the temperature to the “oil window” level, 350°С, leads to a fourfold increase in the intensity of the signal from free organic radicals (С350), and after hydrothermal treatment its intensity increases by a factor of 5. This fact characterizes the oil-generation potential of the rock with the formation of liquid and gaseous hydrocarbons. On reaching the “oil and gas window” temperature (600°С), organic carbon radicals (С600) were not detected. This fact suggests that the rock from productive deposits of the Permian age virtually completely realizes its oil-generation potential at 350°C. The amount of Mn2+ ions in calcite after the hydrothermal treatment gradually decreases with an increase in the pyrolysis temperature. Iron oxides and hydroxides were detected as concomitant compounds. They can exhibit catalytic properties in hydrothermal and pyrolytic processes. The presence of minerals of iron and manganese in different oxidation states suggests nonequilibrium conditions of the rock alteration. Thus, EPR can serve as a nondestructive method for simultaneous monitoring of the mineral composition and organic matter of rocks.

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热化学过程对沥青岩有机物和矿物基质转化影响的 EPR 研究
摘要 通过电子顺磁共振 (EPR) 光谱法研究了二叠纪重质原油矿床(Ashal'cha 油田)富产地层含沥青油岩石的有机物和矿物基质在 350 和 600°С 氢介质中的热化学变化。在水相存在的情况下,在 300°С 温度下进行热液处理前后,对取自 117.5-118.5 米深处的岩石样本进行了研究。对 EPR 光谱进行比较后发现,与最初的岩石相比,温度升高到 "石油窗口 "水平(350°С)后,自由有机自由基的信号强度(С350)增加了四倍,而经过水热处理后,其强度增加了 5 倍。这一事实说明岩石具有生成液态和气态碳氢化合物的石油潜力。在达到 "油气窗口 "温度(600°С)时,未检测到有机碳基(С600)。这一事实表明,二叠纪高产矿床的岩石在 350°C 时几乎完全实现了其生成石油的潜力。热液处理后方解石中的 Mn2+ 离子含量随着热解温度的升高而逐渐减少。检测到铁氧化物和氢氧化物为伴生化合物。它们在水热和热解过程中可表现出催化特性。不同氧化态的铁和锰矿物的存在表明了岩石改变的非平衡条件。因此,EPR 可以作为一种无损方法,用于同时监测岩石的矿物成分和有机物质。
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来源期刊
Petroleum Chemistry
Petroleum Chemistry 工程技术-工程:化工
CiteScore
2.50
自引率
21.40%
发文量
102
审稿时长
6-12 weeks
期刊介绍: Petroleum Chemistry (Neftekhimiya), founded in 1961, offers original papers on and reviews of theoretical and experimental studies concerned with current problems of petroleum chemistry and processing such as chemical composition of crude oils and natural gas liquids; petroleum refining (cracking, hydrocracking, and catalytic reforming); catalysts for petrochemical processes (hydrogenation, isomerization, oxidation, hydroformylation, etc.); activation and catalytic transformation of hydrocarbons and other components of petroleum, natural gas, and other complex organic mixtures; new petrochemicals including lubricants and additives; environmental problems; and information on scientific meetings relevant to these areas. Petroleum Chemistry publishes articles on these topics from members of the scientific community of the former Soviet Union.
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