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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >The characteristics of the biomarkers and δ ~(13)C of n-alkanes released from thermally altered solid bitumens at various maturities by catalytic hydropyrolysis
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The characteristics of the biomarkers and δ ~(13)C of n-alkanes released from thermally altered solid bitumens at various maturities by catalytic hydropyrolysis

机译:通过催化加氢热解从不同成熟度的热改变的固体沥青释放的正构烷烃的生物标志物和δ〜(13)C的特征

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Solid bitumen occurs extensively in the paleo-reservoirs of marine sequences in southern China. The fluids in these paleo-reservoirs have usually experienced severe secondary alteration such as biodegradation and/or thermal maturation. The concentrations of extractable organic matter (EOM) in the resulting solid bitumens are too low to satisfy the amount required for instrumental analysis such as GC-MS and GC-IRMS. It is also difficult to get enough biomarkers and n-alkanes by dry pyrolysis or hydrous pyrolysis directly because such solid bitumens are hydrogen poor due to high maturities. Catalytic hydropyrolysis (HyPy) can release much more EOM from solid bitumen at mature to highly over-mature stages than Soxhlet extraction, dry pyrolysis and hydrous pyrolysis. However, whether the biomarkers in hydropyrolysates can be used for bitumen-source or bitumen-bitumen correlations has been questionable. In this study, a soft biodegraded solid bitumen sample of low maturity was thermally altered to various maturities in a closed system. HyPy was then employed to release bound biomarkers and n-alkanes. Our results show that the geochemical parameters for source and maturity based on biomarkers released from these thermally altered bitumen residues by HyPy are insensitive to the degree of thermal alteration. Furthermore, the maturity parameters are indicative of lower maturity than bitumen maturation products at a corresponding temperature. This suggests that biomarker source and maturity parameters, based on the products of HyPy, remain valid for bitumens which have suffered both biodegradation and severe thermal maturation. The distributions of δ ~(13)C of n-alkanes in hydropyrolysates are also insensitive to the temperature used for bitumen artificial maturation. Hence, the δ ~(13)C values of n-alkanes in hydropyrolysates may also provide useful information in bitumen-bitumen correlation for paleo-reservoir solid bitumens.
机译:固体沥青广泛存在于中国南方海洋层系的古水库中。这些古油藏中的流体通常经历了严重的二次变化,例如生物降解和/或热成熟。生成的固体沥青中的可萃取有机物(EOM)浓度太低,无法满足仪器分析(例如GC-MS和GC-IRMS)所需的量。直接通过干法热解或含水热解也很难获得足够的生物标志物和正构烷烃,因为这种固态沥青由于成熟度高而缺乏氢。与索氏提取,干法热解和水合热解相比,催化加氢热解(HyPy)在成熟到高度成熟阶段可以从固体沥青中释放出更多的EOM。然而,是否可以将水解产物中的生物标记物用于沥青源或沥青-沥青相关性。在这项研究中,在封闭系统中将低成熟度的软生物降解固体沥青样品热更改为各种成熟度。然后使用HyPy释放结合的生物标志物和正构烷烃。我们的研究结果表明,基于由HyPy从这些热改变的沥青残渣中释放的生物标记物来确定来源和成熟度的地球化学参数对热改变的程度不敏感。此外,成熟度参数指示在相应温度下比沥青成熟产品低的成熟度。这表明基于HyPy产物的生物标志物来源和成熟度参数对于遭受了生物降解和严重热成熟的沥青仍然有效。氢解产物中正构烷烃的δ〜(13)C分布对沥青人工成熟所用的温度也不敏感。因此,加氢裂解液中正构烷烃的δ〜(13)C值也可为古油藏固体沥青的沥青-沥青相关性提供有用的信息。

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