油页岩热解气化过程中硫的迁移机理

    Mechanism of sulfur migration during pyrolysis and gasification of oil shale

    • 摘要: 本文聚焦油页岩热解工业应用中的三大技术瓶颈:含硫化合物导致的热解设备腐蚀加速、尾气排放污染加剧及热解产物品质下降问题,通过建立“气氛-硫形态”的耦合调控体系,系统研究油页岩热解气化过程中硫元素的迁移转化行为与化学转化路径,深入探究多元反应氛围对硫赋存形态演变的协同调控机制,旨在为构建硫定向转化的清洁热解新工艺提供坚实的理论支撑与技术指导。采用程序升温热解试验方法,选取碳元素含量46.47%、硫化铁含量9.74%的油页岩样品,从反应气氛调控和硫形态演化两个维度展开研究。运用傅里叶变换红外光谱(FT-IR)与X射线衍射(XRD)等表征技术,揭示了不同氛围条件下硫的转化路径。试验数据表明:在H2/CO2混合气氛围体系中,硫化铁含量可降至1.10%;引入H2O蒸气形成三元混合气氛围后,硫化铁含量进一步降至0.80%,较原料降幅达91.8%。机理研究发现:惰性氛围主要促进硫铁矿和脂肪族硫的H2S释放;H2氛围加速有机大分子裂解;CO2通过增强有机质气化参与硫转化;而H2O蒸气经水煤气反应产生的活性氢原子对FeS具有显著脱除效果。本研究创新性地揭示了多氛围协同作用下硫形态的定向转化规律,证实混合气氛围可实现深度脱硫,为开发低硫半焦绿色制备工艺奠定了理论基础,对推进油页岩资源高效清洁利用具有重要工程指导意义。

       

      Abstract: This paper addresses three major technical challenges in the industrial application of oil shale pyrolysis: accelerated equipment corrosion induced by sulfur compounds, aggravated exhaust emissions, and quality deterioration of pyrolysis products. A coupled regulatory system integrating “atmosphere-sulfur speciation” is established to systematically investigate the migration behavior and chemical transformation pathways of sulfur during pyrolysis and gasification. The synergistic regulation mechanisms of multi-reaction atmospheres on sulfur speciation evolution are thoroughly explored, aiming to provide theoretical and technical foundations for developing clean pyrolysis processes with targeted sulfur conversion. Programmed temperature pyrolysis experiments are conducted on oil shale samples with a carbon content of 46.47% and an iron sulfide content of 9.74%. The research framework encompasses two dimensions: reactive atmosphere regulation and sulfur speciation evolution. Fourier transform infrared spectroscopy (FT-IR) and X-ray diffraction (XRD) are employed to characterize sulfur transformation pathways under varied atmospheres. Experimental results demonstrate that FeS content decreases to 1.10% in H2/CO2 mixed atmosphere, while further reduction to 0.80% (91.8% decrease from raw material) is achieved in ternary H2/CO2/H2O atmosphere. Mechanistic investigations reveal that inert atmosphere primarily facilitates H2S release from pyrite and aliphatic sulfur; H2 atmosphere promotes cleavage of organic macromolecules; CO2 enhances organic matter gasification; whereas the reactive hydrogen atoms generated by the water-gas reaction of H2O steam remove FeS effectively. This work innovatively elucidates the targeted transformation patterns of sulfur speciation under multi-atmosphere synergy, confirming that mixed atmospheres enable deep desulfurization. It establishes a theoretical foundation for developing green semi-coke preparation processes with low sulfur content, providing crucial engineering guidance for advancing efficient and clean utilization of oil shale resources.

       

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