碱性高锰酸钾对油页岩角质的氧化作用

N. Burdelnaya, Ya. Sennikova, Dmitry Bushnev
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引用次数: 0

摘要

我们在碱性介质中用高锰酸钾对波罗的海地区奥陶纪库克石油页岩、蒂曼-佩乔拉地区多曼尼克油页岩和卡什皮尔矿床上侏罗统油页岩的角质层样本进行了分析氧化。我们用 3.5 % 的高锰酸钾溶液进行了单级氧化,然后用色谱-质谱法分析了羧酸的三甲基硅烷衍生物,用 0.5 % 的高锰酸钾溶液进行了多级氧化,并用红外光谱分析了氧化产物。在多曼尼克页岩和侏罗纪页岩的角质层中,一些正烷基结构与角质基质外围相关,而在库克斯岩角质层的结构中,正烷基结构主要是较大片段的连接纽带。在多阶段过程中,较温和的氧化作用会导致形成大块的角质层碎片,这些碎片通常重复其碳结构,但氧化程度更高。
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Oxidation of oil shale kerogen by alkaline potassium permanganate
We carried out the analytical oxidation of kerogen samples from oil shales of Ordovician kukersite from the Baltic region, Domanik shales from Timan-Pechora and Upper Jurassic oil shales of the Kashpir deposit by potassium permanganate in an alkaline medium. We performed a single-stage oxidation with 3.5 % solution of potassium permanganate, followed by analysis of trimethylsilyl derivatives of carboxylic acids using chromatography-mass spectrometry, and multi-stage oxidation by 0.5 % solution of potassium permanganate and analysis of oxidation products using IR spectroscopy. Some n-alkyl structures are peripherally associated with the kerogen matrix in the kerogen of Domanik and Jurassic shales, while in the structure of kukersite kerogen, n-alkyl structures are mainly connecting links for larger fragments. Milder, in case of a multi-stage process, oxidation results in formation of large fragments of kerogen, generally repeating its carbon structure, but more oxidized.
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