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A comparison of different methods for determining the organic and inorganic carbon content of lake sediment from two lakes on the Tibetan Plateau

机译:青藏高原两个湖泊湖泊沉积物中有机碳和无机碳含量测定方法的比较

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摘要

This paper presents three parallel datasets of total organic carbon (TOC) and total inorganic carbon (TIC) as well as carbonate content (CaCO_3) of lake sediment from two lakes on the Tibetan Plateau in order to compare different methods and different machines. The results indicate that two carbon analyzers (a Shimadzu TOC-V_(Cph) with solid sample module SSM-5000A and an Elementar Vario EL II) provide very similar TOC and TIC content despite slightly different performance procedures and temperature controls. A TOC record determined by a wet oxidation method and a carbon analyzer shows consistent down core variation although it seems that the wet oxidation method may overestimate TOC content due to the existence of some reduced compounds or minerals in the sediment TIC content measured by a carbon analyzer and carbonate content determined by a chemical method exhibit similar fluctuation trends in both cores. This suggests that TIC content may be used as an environmental proxy roughly taking the place of carbonate content, especially in sediment with simple carbonate compositions.
机译:本文介绍了三个平行的数据集,分别来自青藏高原两个湖泊的湖泊沉积物的总有机碳(TOC)和总无机碳(TIC)以及碳酸盐含量(CaCO_3),以比较不同方法和不同机制。结果表明,尽管性能程序和温度控制稍有不同,但两个碳分析仪(带有固体样品模块SSM-5000A的Shimadzu TOC-V_(Cph)和Elementar Vario EL II)提供非常相似的TOC和TIC含量。通过湿式氧化法和碳分析仪确定的TOC记录显示出一致的向下岩心变化,尽管由于碳分析仪测得的沉积物中TIC含量存在某些还原性化合物或矿物质,所以湿式氧化法似乎可能高估了TOC含量化学方法确定的碳酸盐含量和碳酸盐含量在两个岩心中都表现出相似的波动趋势。这表明TIC含量可以用作环境指标,大致替代碳酸盐含量,尤其是在具有简单碳酸盐成分的沉积物中。

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  • 来源
    《Quaternary International》 |2012年第10期|p.49-54|共6页
  • 作者单位

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes (TEL), Institute of Tibetan Plateau Research, Chinese Academy of Sciences,P.O. Box 2871 No.18 Shuangqing Rd., Beijing 100085, PR China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes (TEL), Institute of Tibetan Plateau Research, Chinese Academy of Sciences,P.O. Box 2871 No.18 Shuangqing Rd., Beijing 100085, PR China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes (TEL), Institute of Tibetan Plateau Research, Chinese Academy of Sciences,P.O. Box 2871 No.18 Shuangqing Rd., Beijing 100085, PR China;

    Key Laboratory of Tibetan Environment Changes and Land Surface Processes (TEL), Institute of Tibetan Plateau Research, Chinese Academy of Sciences,P.O. Box 2871 No.18 Shuangqing Rd., Beijing 100085, PR China;

    Institut fuer Geographie, Friedrich-Schiller-Universitat, Lbbdergraben 32, 07743 Jena, Germany;

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