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Selective chemical degradation of kerogen from Nenjiang Formation of the southern Songliao Basin

机译:松辽盆地南部嫩江组干酪根的选择性化学降解

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A sequential selective chemical degradation has been performed on the kerogen from the Nenjiang Formation of the southern Songliao Basin by using a series of mild chemical degradations (alkaline hydrolysis, cleavage of ether-bonds and sulfur-bonds, and ruthenium tetroxide (RuO_4) oxidation). Subsequently, the GC-MS analyses are carried out on different degradation products. The results show that chemical degradations can release a great number of GC/MS-determinable biomarkers from insoluble kerogen, such as, alkaline hydrolysis products mainly comprise n-alkanes, fatty acids and al-kanols; thiophene compounds are predominantly ether-bound to kerogen matrix; the products from the cleavage of sulfur-sulfur and sulfur-carbon bonds in the kerogen include fatty acids, alkanols and some n-alkanes with high carbon numbers; RuO_4 oxidation products are predominantly monocarboxylic acids and α,ω-dicarboxylic acids. The distributions of main degradation products indicate that organic matter in this kerogen is predominantly derived from algae and bacteria, and that small amounts of high plant-derived organic matter are possibly combined into kerogen matrix at the late stage by sulfur bonds and other means. This study will provide an important approach for further discussing sources of organic matter in source rocks and their depositional paleoenvironments.
机译:通过一系列轻度化学降解(碱性水解,醚键和硫键的裂解以及四氧化钌(RuO_4)氧化)对松辽盆地南部嫩江组干酪根进行了连续的选择性化学降解。 。随后,对不同的降解产物进行了GC-MS分析。结果表明,化学降解可从不溶性干酪根中释放出大量可由GC / MS测定的生物标志物,例如碱性水解产物主要包括正构烷烃,脂肪酸和链烷醇。噻吩化合物主要与醚键合在干酪根基质上;干酪根中硫-硫键和硫-碳键的裂解产物包括脂肪酸,链烷醇和一些碳原子数高的正构烷烃; RuO_4氧化产物主要是一元羧酸和α,ω-二元羧酸。主要降解产物的分布表明,该干酪根中的有机物主要来自藻类和细菌,并且少量的高植物来源有机物可能在后期通过硫键和其他方式结合到干酪根基质中。这项研究将为进一步讨论烃源岩中有机质的来源及其沉积古环境提供重要的方法。

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