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Evaluation of total organic carbon contents in carbonate source rocks by modified acid treatment method and the geological significance of acid-soluble organic matters

机译:改进的酸处理方法评价碳酸盐岩中总有机碳含量及酸溶性有机质的地质意义

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摘要

Total organic carbon contents are an important parameter in evaluating hydrocarbon source rocks and it shows the hydrocarbon-generating potential of hydrocarbon source rocks. In this study, the total organic carbon of 16 carbonate rocks with different maturity level was determined by a modified acid treatment protocol of the elemental analyzer method. In the modified method, montmorillonite is used to thicken the residue of acid treatment and remaining acid solution. Then, total organic carbon values of "clay-paste" sample were analyzed by the element analysis method. The results of 16 carbonate rocks show that the total organic carbon values with the new method were greater than the conventional total organic carbon test in a majority of the samples. Additionally, the fraction of acid-soluble organic matters was investigated and it shows no clear relationship of the fraction of acid-soluble organic matters with maturity and total organic carbon values in source rocks. Hence, it indicates that the released acid-soluble organic matters are characterized by complex factors that influence their occurrence and compositions.
机译:总有机碳含量是评估烃源岩的重要参数,它显示了烃源岩的生烃潜力。在这项研究中,通过元素分析仪方法的改良酸处理方案确定了16个不同成熟度碳酸盐岩的总有机碳。在改进的方法中,蒙脱石用于增稠酸处理残渣和剩余的酸溶液。然后,通过元素分析法分析“粘土-糊剂”样品的总有机碳值。 16个碳酸盐岩的结果表明,在大多数样品中,用新方法测得的总有机碳值均高于常规总有机碳测试值。此外,对酸溶性有机物的比例进行了研究,结果表明,烃源岩中酸溶性有机物的比例与成熟度和总有机碳值之间没有明确的关系。因此,这表明释放的酸溶性有机物的特征是影响其发生和组成的复杂因素。

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