中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Generation Potential and Kinetics of Gaseous Hydrocarbons from Upper Paleozoic Carboniferous Benxi Formation Mudstone in Ordos Basin, China

文献类型:期刊论文

作者Liu, Min2,3,4; Kong, Qingfen1; Wang, Huaichang1; Zhang, Hui1; Guo, Huijuan3,4; Wang, Yunpeng3,4; Shi, Shuyong3,4; Wang, Qiang3,4; Liu, Jinzhong3,4; Peng, Ping'an3,4
刊名ACS OMEGA
出版日期2024-09-05
卷号9期号:37页码:39088-39099
ISSN号2470-1343
DOI10.1021/acsomega.4c05874
英文摘要Industrial quantities of tight gas from the Carboniferous Benxi Formation have been found in the southern Ordos Basin. The source and contributions from mudstone and coal in the Benxi Formation to the tight gas are still unclear, and the hydrocarbon generation potential and kinetics of the Benxi Formation mudstone have rarely been reported, which has halted resource evaluation of tight gas. Confined pyrolysis experiments were performed to determine the yields and kinetic parameters for gaseous hydrocarbon formation for a representative sample of a Benxi Formation mudstone from the Ordos Basin, with a hydrogen index (HI) of 137 mg/g TOC and T-max of 434 degrees C. The maximum yield of C-1-C-5 hydrocarbons is 143 mg/g TOC. For samples with similar HI, Upper Paleozoic mudstone samples might have a higher total gas generation potential than Upper Paleozoic coal samples because of the more reducing environment during mudstone deposition, which is beneficial for the preservation of sedimentary lipids. Even though the HI of Upper Paleozoic coals is apparently higher than that of Upper Paleozoic mudstones, they have a similar late gas generation potential. Basin modeling shows that the amount of natural gas generated from Benxi Formation mudstone increases southward. Coaly source rocks from the Ordos Basin with a lower oil generation potential have more negative delta C-13(1) values when the vitrinite reflectance is lower than 1.4-1.7%. This phenomenon might be related to the more negative delta C-13 of wet gas or the small hydrocarbon molecules incorporated into the kerogen compared with the components generating primary cracking gases. This study deepens the understanding of gaseous hydrocarbons generated from mudstone and coal in transitional depositional environments and provides the key parameters for tight gas resources in this area.
WOS研究方向Chemistry
语种英语
WOS记录号WOS:001307774900001
源URL[http://ir.gig.ac.cn/handle/344008/80647]  
专题有机地球化学国家重点实验室
通讯作者Guo, Huijuan
作者单位1.PetroChina Changqing Oilfield, Res Inst Explorat & Dev, Xian 710018, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China
4.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Peoples R China
推荐引用方式
GB/T 7714
Liu, Min,Kong, Qingfen,Wang, Huaichang,et al. Generation Potential and Kinetics of Gaseous Hydrocarbons from Upper Paleozoic Carboniferous Benxi Formation Mudstone in Ordos Basin, China[J]. ACS OMEGA,2024,9(37):39088-39099.
APA Liu, Min.,Kong, Qingfen.,Wang, Huaichang.,Zhang, Hui.,Guo, Huijuan.,...&Peng, Ping'an.(2024).Generation Potential and Kinetics of Gaseous Hydrocarbons from Upper Paleozoic Carboniferous Benxi Formation Mudstone in Ordos Basin, China.ACS OMEGA,9(37),39088-39099.
MLA Liu, Min,et al."Generation Potential and Kinetics of Gaseous Hydrocarbons from Upper Paleozoic Carboniferous Benxi Formation Mudstone in Ordos Basin, China".ACS OMEGA 9.37(2024):39088-39099.

入库方式: OAI收割

来源:广州地球化学研究所

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