2018
DOI: 10.3176/oil.2018.3.02
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Experimental Research of the Pyrolytic Properties and Mineral Components of Bogda Oil Shale, China

et al.

Abstract: The purpose of this paper was to investigate the pyrolysis properties and mineral structures of Bogda oil shale, Xinjiang, China. To this end, techniques such as Fourier transform infrared spectroscopy (FTIR), X-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive spectrometry (EDS) and thermogravimetry-mass spectrometry (TG-MS) were used. The results showed that oil shale was rich in clay minerals, quartz, calcite, frondelite and pyrite. Aliphatic hydrocarbons were mainly dominant in t… Show more

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Cited by 6 publications
(2 citation statements)
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“…The broad hump appearing at around 2θ = 20° of HD-K indicates that it contains more n -alkanes and naphthenes compared with the three other kerogens . The small sharp diffraction peaks evident in HD-K, FS-K, and DCG-K are attributed to pyrite. , The XRD patterns suggest that mostly minerals, such as quartz, calcite, montmorillonite, and kaolinite, are eliminated by the HCl/HF treatment. , …”
Section: Results and Discussionmentioning
confidence: 99%
“…The broad hump appearing at around 2θ = 20° of HD-K indicates that it contains more n -alkanes and naphthenes compared with the three other kerogens . The small sharp diffraction peaks evident in HD-K, FS-K, and DCG-K are attributed to pyrite. , The XRD patterns suggest that mostly minerals, such as quartz, calcite, montmorillonite, and kaolinite, are eliminated by the HCl/HF treatment. , …”
Section: Results and Discussionmentioning
confidence: 99%
“…The pyrolysis of organic matter in oil shale can be divided into two obvious stages, and the occupation and blockage of intermediate products will affect the measurement of pore structure at the corresponding temperature (Lai et al 2016;Liu et al 2023). After 500 °C, the pyrolysis reaction of organic matter in oil shale is basically completed, and the changes in its pore structure are mainly caused by the thermal effects of temperature on inorganic minerals, such as the removal of crystal water from clay minerals, the decomposition of carbonate minerals, the thermal fracture caused by the expansion of quartz phase change, and the connection and collapse of pore structure at high temperature (Liu et al 2014;Zhang et al 2018); At this stage, the changes of pore structure of Xinjiang oil shale are closely related to its mineral composition.…”
Section: The Results Of Joint Characterizationmentioning
confidence: 99%