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Hydrocarbon speciation studies in ancient sediments by high temperature supercritical carbon dioxide extraction

机译:高温超临界二氧化碳萃取法对古代沉积物中的烃类物种形成研究

摘要

Results on the application of high-temperature supercritical carbon dioxide extraction (HT-SFE) to the study of hydrocarbon (HC) speciation in geological samples are presented. Ancient sediments were treated by stepwise extractions, and by using a fresh sample each time. SFE temperatures ranged between 50 and 350°C. Individual analytes showed to be speciated in different ways throughout the solid matrix because different fractions are extracted under different energy conditions. Aromatic HCs appear to have a stronger association with the matrix than the aliphatics due to their higher polarity and molecular planarity. No evidence of geosynthesis of alkylaromatics during HT-SFE was obtained. Tri- and mono-aromatic steranes were totally extracted at relatively low temperatures while hopanes and steranes show a small fraction strongly interacting with the macromolecular organic structure possibly due to u22trappingu22 processes. The release of u22trappedu22 HCs was confirmed by the u22maturity inversionu22 effect observed for the molecular distribution of hopanes at the highest extraction temperatures. Branched compounds like pristane and phytane showed to have a weaker association with the organic matrix if compared with straight chain analytes. Fresh sample extracted by SFE at different temperatures confirmed the results obtained for the stepwise procedure. Rock-Eva! Pyrolysis and Pyrolysis-Gas Chromatography/Mass Spectrometry (Py-GC/MS) from SFE pre-extracted sediments showed that HCs extracted at the highest temperature levels are not dominated by pyrolysis products and may have been released from trapped conditions, through irreversible thermally induced structural changes of the matrix and/or rearrangements of the macromolecular organic matter possibly via sulfur bond cleavage. No significant changes of the matrix were apparent after HT-SFE as suggested by Rock-Eval Pyrolysis and Py-GC/MS experiments, as well as from Electron Scanning Microscopy (ESM) determinations.
机译:提出了将高温超临界二氧化碳萃取(HT-SFE)应用于地质样品中烃(HC)形态研究的结果。通过逐步提取以及每次使用新鲜样品来处理古代沉积物。 SFE温度范围为50至350°C。由于在不同的能量条件下会提取不同的馏分,因此整个固体基质中的各个分析物都具有不同的规格。芳香族HC与极性化合物相比,由于其较高的极性和分子平面性,与基质的结合性似乎更高。没有证据表明在HT-SFE过程中发生了烷基芳烃的合成。三芳族和单芳族甾烷在相对较低的温度下被完全提取,而hop烷和甾烷则显示出一小部分与高分子有机结构发生强烈相互作用,这可能是由于“捕获”过程所致。通过在最高提取温度下对hop烷的分子分布观察到的 u22成熟度反转 u22效应,证实了 u22捕获的 u22 HCs的释放。与直链分析物相比,支链化合物(例如ane烷和植烷)显示出与有机基质的缔合较弱。通过SFE在不同温度下提取的新鲜样品证实了分步程序获得的结果。摇滚娃!从SFE预提取沉积物中进行的热解和热解气相色谱/质谱(Py-GC / MS)表明,在最高温度水平下提取的HCs不受热解产物的支配,并且可能是由于不可逆的热诱导而从捕获条件中释放出来的基质结构的变化和/或大分子有机物的重排可能是通过硫键断裂。根据Rock-Eval热解和Py-GC / MS实验以及电子扫描显微镜(ESM)的测定,在HT-SFE之后,基质没有明显变化。

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    Diaz Doraida;

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  • 年度 1996
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