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Chemical composition and distribution of the components of valley peat from Amur oblast

机译:阿穆尔州谷泥炭的化学组成和组成分布

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摘要

The chemical composition of sedge peat from the Egor'evskoe deposit as lowland peat from Amur oblast was characterized. The elemental composition of organic matter and mineral macro- and microcomponents was studied, and the distribution of bitumens, their fractions, and humic acids in the depth of occurrence was revealed. It was found that peat genesis processes occur over the entire vertical profile, and the most converted organic matter is formed at a depth of to 90 cm. The individual composition of alkane fractions consists of C-13-C-36 normal structure homologues with a carbon preference index somewhat higher than unity; the presence of pristane, phytane, and farnezane was detected. In the fractions of fatty acids, predominantly even compounds from C-10 to C-30 were identified with special distribution features at the separate stages of peat formation. The analysis of the individual composition of n-alkanes and fatty acids made it possible to supplement botanical characteristics with information on the contribution of macrophytes, algal material, and microorganisms to the formation of the organic matter of peat.
机译:对来自Egor'evskoe矿床的芦苇泥炭的化学成分进行了表征,作为来自阿穆尔州的低地泥炭。研究了有机物和矿物的宏观和微观成分的元素组成,并揭示了沥青,其级分和腐殖酸在发生深度的分布。发现泥炭的形成过程发生在整个垂直剖面上,并且转化最多的有机物形成在90 cm的深度。烷烃馏分的单独组成由C-13-C-36正常结构同系物组成,其碳优先指数略高于1。检测到存在rist烷,植烷和法呢烷。在脂肪酸馏分中,主要鉴定出的甚至是C-10至C-30的化合物在泥炭形成的各个阶段都具有特殊的分布特征。通过对正构烷烃和脂肪酸的单独组成进行分析,可以利用有关大型植物,藻类物质和微生物对泥炭有机物形成的贡献的信息来补充植物学特征。

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  • 来源
    《Solid Fuel Chemistry》 |2016年第6期|339-345|共7页
  • 作者单位

    Russian Acad Sci, Inst Geol & Nat Management, Far East Branch, Blagoveshchensk 675000, Russia;

    Russian Acad Sci, Inst Geol & Nat Management, Far East Branch, Blagoveshchensk 675000, Russia;

    Russian Acad Sci, Inst Geol & Nat Management, Far East Branch, Blagoveshchensk 675000, Russia;

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