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        Compositional and structural variations of bitumen and its interactions with mineral matters during Huadian oil shale pyrolysis

        Zhibing Chang,Mo Chu,Chao Zhang,Shuxia Bai,Hao Lin,Liangbo Ma 한국화학공학회 2017 Korean Journal of Chemical Engineering Vol.34 No.12

        Thermal bitumen is an important intermediate derived from kerogen decomposition during oil shale pyrolysis. In this study, free bitumen (FB) and bound bitumen (BB) were obtained by extracting oil shale chars (300- 550 oC) before and after demineralization, and then analyzed by liquid chromatography fractionation, Fourier transform infrared spectroscopy, and gas chromatography/mass spectrometry. The FB yield first increased and then decreased with increasing temperature, and the maximum value was 2.10% at 400 oC. The decarboxylation of acids and decomposition of esters at 350-450 oC decreased the content of these compounds. Meanwhile, the intense cracking reactions of aliphatic compounds and alkyl chains at 400-450 oC decreased the carbon chain lengths and molecular weights of these compounds. From the analytical results obtained for the BB fractions, we suggest that some carboxylic acids or carboxyl group-containing compounds may be trapped on carbonate particles by the formation of Ca2+COO− bonds, whereas other oxygenated compounds (e.g., esters and phenols) can be adsorbed preferentially by clay minerals through Lewis acid-base interactions.

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