Pyrolysis characteristics of organic-rich shale from the Chang 7 member of Triassic Yanhe Profile in Ordos Basin

被引:3
|
作者
Ge Z. [1 ,2 ]
Sun Q. [2 ,3 ,4 ]
Li D. [1 ,2 ]
Shi Q. [1 ,2 ]
Wei S. [1 ,2 ]
Yang T. [1 ,2 ]
机构
[1] College of Geology and Environment, Xi’an University of Science and Technology, Xi’an, 710054, Shaanxi
[2] Geological Research Institute for Coal Green Mining, Xi’an University of Science and Technology, Xi’an
[3] Shaanxi Provincial Key Laboratory of Geological Support for Coal Green Exploitation, Xi’an
[4] Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Land and Resources, Xi’an
基金
中国国家自然科学基金;
关键词
Activation energy; Chang; 7; Organic-rich shale; Pyrolysis kinetics; TOC;
D O I
10.1007/s12517-021-07382-y
中图分类号
学科分类号
摘要
A set of thick, black organic shale is developed at the bottom of the Chang 7 accumulation, an important oil-producing section of the Triassic Yanchang Formation in Ordos Basin. In this paper, the thermogravimetric (TG) behaviour of different organic-rich shale layers is studied in an argon environment. Changes in activation energy (E) are analysed by the Coats-Redfern kinetic method, and thermodynamic characteristics at different temperature stages are clarified. The TG curve of Chang 7 shale decreases between 400 and 650°C, which is the main temperature range of organic matter pyrolysis. Meanwhile, the pyrolysis rate reaches a maximum at about 500°C. In the low-temperature stage, E is low and increases with the temperature. At a temperature of about 650°C and conversion rate of about 0.8, the E reaches a maximum. The organic carbon content in layers Y4 and Y5 are higher, while the E is relatively low. © 2021, Saudi Society for Geosciences.
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