Donglin Zhang, Meijun Li, Rongzhen Qiao, Hong Xiao
{"title":"超深层油藏高纯度石油中芳烃成熟度参数的适用性和局限性","authors":"Donglin Zhang, Meijun Li, Rongzhen Qiao, Hong Xiao","doi":"10.1021/acs.energyfuels.4c02159","DOIUrl":null,"url":null,"abstract":"A substantial reserve of highly mature light oil has been discovered in the Ordovician reservoir of the Shunbei oilfield, Tarim Basin, Northwest China. This study aims to provide an objective assessment of oil maturity in the Shunbei oilfield and establish a reliable maturity evaluation index for oil in the high thermal evolution stage. Eighteen crude oil samples from the no. 4 fault zone (F4) of the Shunbei oilfield were systematically analyzed. Aromatic hydrocarbon, light hydrocarbon components, and diamondoid compositions were analyzed by gas chromatography–mass spectrometry. The depositional environment and the organic matter input of their related source rocks were determined by the corresponding geochemical indicators. The results indicate that the F4 oils have been derived from the same source kitchen and belong to the same oil population. The oil maturity in the study area was evaluated by the maturity parameters relative to aromatics, light hydrocarbons, and diamondoids. The analysis indicates that the results of aromatic parameters for identifying oil maturity contradict those of light hydrocarbon and diamondoid parameters. The equivalent vitrinite reflectance of the oil samples ranges from 1.43% to 1.54%. It is concluded that light hydrocarbon and diamondoid parameters can reliably be used to evaluate the maturity of oil in the high thermal evolution stage. However, most of the aromatic maturity parameters exhibit significant limitations during the high-temperature evolution stage. The maturity parameters of phenanthrene and dibenzothiophene were “reversed” in the high thermal evolution stage due to demethylation and thermal alteration, respectively. Additionally, most naphthalene maturity parameters are affected by thermally induced condensation, rendering them unsuitable for maturity evaluation of the high-temperature evolution stage. Notably, pentamethylnaphthalene ratio [PMNr, PMNr = 1, 2, 4, 6, 7-/(1, 2, 4, 6, 7 + 1, 2, 3, 5, 6)-pentamethylnaphthalene] exhibits a strong positive correlation with gas–oil ratio, <i>n</i>-heptane/methylcyclohexane (<i>n</i>C<sub>7</sub>/MCH) ratio, and (3 + 4)-methyldiamantane concentrations, indicating their reliability as maturity indicators for highly to overmature oils and source rocks.","PeriodicalId":35,"journal":{"name":"Energy & Fuels","volume":"17 1","pages":""},"PeriodicalIF":5.2000,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Applicability and Limitation of Aromatic Maturity Parameters in High-Maturity Oil from Ultradeep Reservoirs\",\"authors\":\"Donglin Zhang, Meijun Li, Rongzhen Qiao, Hong Xiao\",\"doi\":\"10.1021/acs.energyfuels.4c02159\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A substantial reserve of highly mature light oil has been discovered in the Ordovician reservoir of the Shunbei oilfield, Tarim Basin, Northwest China. This study aims to provide an objective assessment of oil maturity in the Shunbei oilfield and establish a reliable maturity evaluation index for oil in the high thermal evolution stage. Eighteen crude oil samples from the no. 4 fault zone (F4) of the Shunbei oilfield were systematically analyzed. Aromatic hydrocarbon, light hydrocarbon components, and diamondoid compositions were analyzed by gas chromatography–mass spectrometry. The depositional environment and the organic matter input of their related source rocks were determined by the corresponding geochemical indicators. The results indicate that the F4 oils have been derived from the same source kitchen and belong to the same oil population. The oil maturity in the study area was evaluated by the maturity parameters relative to aromatics, light hydrocarbons, and diamondoids. The analysis indicates that the results of aromatic parameters for identifying oil maturity contradict those of light hydrocarbon and diamondoid parameters. The equivalent vitrinite reflectance of the oil samples ranges from 1.43% to 1.54%. It is concluded that light hydrocarbon and diamondoid parameters can reliably be used to evaluate the maturity of oil in the high thermal evolution stage. However, most of the aromatic maturity parameters exhibit significant limitations during the high-temperature evolution stage. The maturity parameters of phenanthrene and dibenzothiophene were “reversed” in the high thermal evolution stage due to demethylation and thermal alteration, respectively. Additionally, most naphthalene maturity parameters are affected by thermally induced condensation, rendering them unsuitable for maturity evaluation of the high-temperature evolution stage. Notably, pentamethylnaphthalene ratio [PMNr, PMNr = 1, 2, 4, 6, 7-/(1, 2, 4, 6, 7 + 1, 2, 3, 5, 6)-pentamethylnaphthalene] exhibits a strong positive correlation with gas–oil ratio, <i>n</i>-heptane/methylcyclohexane (<i>n</i>C<sub>7</sub>/MCH) ratio, and (3 + 4)-methyldiamantane concentrations, indicating their reliability as maturity indicators for highly to overmature oils and source rocks.\",\"PeriodicalId\":35,\"journal\":{\"name\":\"Energy & Fuels\",\"volume\":\"17 1\",\"pages\":\"\"},\"PeriodicalIF\":5.2000,\"publicationDate\":\"2024-09-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Energy & Fuels\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://doi.org/10.1021/acs.energyfuels.4c02159\",\"RegionNum\":3,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENERGY & FUELS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Energy & Fuels","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1021/acs.energyfuels.4c02159","RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
Applicability and Limitation of Aromatic Maturity Parameters in High-Maturity Oil from Ultradeep Reservoirs
A substantial reserve of highly mature light oil has been discovered in the Ordovician reservoir of the Shunbei oilfield, Tarim Basin, Northwest China. This study aims to provide an objective assessment of oil maturity in the Shunbei oilfield and establish a reliable maturity evaluation index for oil in the high thermal evolution stage. Eighteen crude oil samples from the no. 4 fault zone (F4) of the Shunbei oilfield were systematically analyzed. Aromatic hydrocarbon, light hydrocarbon components, and diamondoid compositions were analyzed by gas chromatography–mass spectrometry. The depositional environment and the organic matter input of their related source rocks were determined by the corresponding geochemical indicators. The results indicate that the F4 oils have been derived from the same source kitchen and belong to the same oil population. The oil maturity in the study area was evaluated by the maturity parameters relative to aromatics, light hydrocarbons, and diamondoids. The analysis indicates that the results of aromatic parameters for identifying oil maturity contradict those of light hydrocarbon and diamondoid parameters. The equivalent vitrinite reflectance of the oil samples ranges from 1.43% to 1.54%. It is concluded that light hydrocarbon and diamondoid parameters can reliably be used to evaluate the maturity of oil in the high thermal evolution stage. However, most of the aromatic maturity parameters exhibit significant limitations during the high-temperature evolution stage. The maturity parameters of phenanthrene and dibenzothiophene were “reversed” in the high thermal evolution stage due to demethylation and thermal alteration, respectively. Additionally, most naphthalene maturity parameters are affected by thermally induced condensation, rendering them unsuitable for maturity evaluation of the high-temperature evolution stage. Notably, pentamethylnaphthalene ratio [PMNr, PMNr = 1, 2, 4, 6, 7-/(1, 2, 4, 6, 7 + 1, 2, 3, 5, 6)-pentamethylnaphthalene] exhibits a strong positive correlation with gas–oil ratio, n-heptane/methylcyclohexane (nC7/MCH) ratio, and (3 + 4)-methyldiamantane concentrations, indicating their reliability as maturity indicators for highly to overmature oils and source rocks.
期刊介绍:
Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.