龙口煤田古近系褐煤地球化学特征

    Geochemical Characteristics of Paleogene Lignite in Longkou Coalfield

    • 摘要: 应用现代测试技术手段和实验方法,研究龙口煤田古近系褐煤地球化学特征并分析其生物气生成潜力。研究结果表明,龙口褐煤的Ro值平均为0.41%,处于未成熟阶段,挥发组分含量高,表明可生物降解潜力大;显微组分中腐植组含量占绝对优势,体现良好的生化活性;氯仿沥青“A”抽提率在1.8%~7.5%之间,属于好的烃源岩;族组分组成特征表明龙口褐煤处于有机质演化的早期阶段,有利于生物气生成;饱和烃碳数分布特征表明龙口褐煤形成的沉积环境为弱还原的淡水-微咸水深湖相,其母质来源中有低等水生生物的混入;龙口褐煤腐殖酸成熟度低,其分子结构中芳香环化程度低,其母质来源主要为陆生的含维管束植物。龙口煤田褐煤地球化学特征综合表明其具有良好的生物气生成潜力。

       

      Abstract: By means of the modern testing technology and experimental methods, we study geochemical characteristics of lignite of Paleogene in Longkou Coalfield and analyze generating potential of biogenic gas. The results of the study showed that, average Ro value of Longkou lignite was 0.41%, and it was at the immature stage . High volatile content showed that the biodegradable potential was great . Huminite content was dominant , and it embodied high biochemical activity . Extraction rate of chloroform bitumen "A" was between 1.8% to 7.5%, so it belonged to good source rocks. Characteristics of group composition indicated that lignite was in early stages of the evolution of organic matter, and it was conducive to biogenic gas. The distribution characteristics of saturated hydrocarbon showed that the sedimentary environment was deep fresh and brackish lacustrine deposited in weak reduction and the source material was mixed with the lower aquatic organism. The maturity of humic acids was low, the degree of aromatic ring was low, and the source material was mainly terrestrial plants with vascular bundle. Geochemistry of lignite in Longkou Coalfield suggested that it had good generating potential of biogenic gas.

       

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