4.7 Article

Investigation on the characteristics and interaction of co-pyrolysis of oil shale and peanut shell

Journal

FUEL
Volume 340, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.fuel.2023.127502

Keywords

Oil shale; Peanut shell; Co-pyrolysis; Kinetic analysis; Interaction mechanism

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In order to address the issues of low oil yield in oil shale and high oxygen content in biomass pyrolysis oil, the co-pyrolysis of oil shale and peanut shell was studied using thermogravimetric analyzer and fixed bed reactor. Through analysis of co-pyrolysis characteristics, kinetics, and oil phase products, a series of co-pyrolysis interaction mechanisms were proposed. The co-pyrolysis led to earlier decomposition of oil shale and higher conversion rate of the blended feedstock. The interaction at different temperatures was dominated by oil shale radicals and minerals catalysis at low temperatures, and by biomass alkali/alkaline earth metals at high temperatures. These interactions promoted the formation of aliphatic and aromatic hydrocarbons in the oil, reducing carbon chain length and increasing light oil content.
Aiming at the low oil yield of oil shale, and the high content of oxygen in biomass pyrolysis oil, the co-pyrolysis of oil shale and peanut shell were studied by thermogravimetric analyzer and fixed bed reactor. Based on the copyrolysis characteristics, kinetic and oil phase products analysis, a series of co-pyrolysis interaction mechanism has been proposed. The co-pyrolysis caused the earlier decomposition of oil shale and higher conversion rate of blended feedstock. The contribution of co-pyrolysis to the total conversion and oil phase products yield was most significant with biomass blending ratio of 50 %, while the contribution to the activation energy and the generation of aliphatic hydrocarbons was most significant when the ratio was 25 %. The co-pyrolysis interaction at low-temperature (160-400 degrees C) is dominated by oil shale radicals promoting biomass bond breaking and the minerals catalysis on biomass decomposition. For high-temperature (400-600 degrees C), it is dominated by biomass alkali/alkaline earth metals which catalyze oil shale decomposition. The interaction promotes the formation of aliphatic and aromatic hydrocarbons in the oil, reduces the average carbon chain length and increases the light oil content.

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